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<front>
<journal-meta>
<journal-id journal-id-type="publisher-id">Front. Mar. Sci.</journal-id>
<journal-title>Frontiers in Marine Science</journal-title>
<abbrev-journal-title abbrev-type="pubmed">Front. Mar. Sci.</abbrev-journal-title>
<issn pub-type="epub">2296-7745</issn>
<publisher>
<publisher-name>Frontiers Media S.A.</publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.3389/fmars.2025.1523585</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Marine Science</subject>
<subj-group>
<subject>Review</subject>
</subj-group>
</subj-group>
</article-categories>
<title-group>
<article-title>Uncrewed surface vehicles in the Global Ocean Observing System: a new frontier for observing and monitoring at the air-sea interface</article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author" corresp="yes">
<name>
<surname>Patterson</surname>
<given-names>Ruth G.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="author-notes" rid="fn001">
<sup>*</sup>
</xref>
<xref ref-type="author-notes" rid="fn003">
<sup>&#x2020;</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/2885040"/>
<role content-type="https://credit.niso.org/contributor-roles/conceptualization/"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/formal-analysis/"/>
<role content-type="https://credit.niso.org/contributor-roles/funding-acquisition/"/>
<role content-type="https://credit.niso.org/contributor-roles/investigation/"/>
<role content-type="https://credit.niso.org/contributor-roles/methodology/"/>
<role content-type="https://credit.niso.org/contributor-roles/project-administration/"/>
<role content-type="https://credit.niso.org/contributor-roles/resources/"/>
<role content-type="https://credit.niso.org/contributor-roles/software/"/>
<role content-type="https://credit.niso.org/contributor-roles/supervision/"/>
<role content-type="https://credit.niso.org/contributor-roles/validation/"/>
<role content-type="https://credit.niso.org/contributor-roles/visualization/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Cronin</surname>
<given-names>Meghan F.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/618553"/>
<role content-type="https://credit.niso.org/contributor-roles/conceptualization/"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/funding-acquisition/"/>
<role content-type="https://credit.niso.org/contributor-roles/investigation/"/>
<role content-type="https://credit.niso.org/contributor-roles/methodology/"/>
<role content-type="https://credit.niso.org/contributor-roles/project-administration/"/>
<role content-type="https://credit.niso.org/contributor-roles/resources/"/>
<role content-type="https://credit.niso.org/contributor-roles/supervision/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Swart</surname>
<given-names>Sebastiaan</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/411409"/>
<role content-type="https://credit.niso.org/contributor-roles/conceptualization/"/>
<role content-type="https://credit.niso.org/contributor-roles/funding-acquisition/"/>
<role content-type="https://credit.niso.org/contributor-roles/investigation/"/>
<role content-type="https://credit.niso.org/contributor-roles/project-administration/"/>
<role content-type="https://credit.niso.org/contributor-roles/resources/"/>
<role content-type="https://credit.niso.org/contributor-roles/supervision/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Beja</surname>
<given-names>Joana</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/640643"/>
<role content-type="https://credit.niso.org/contributor-roles/conceptualization/"/>
<role content-type="https://credit.niso.org/contributor-roles/investigation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Edholm</surname>
<given-names>Johan M.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
<xref ref-type="author-notes" rid="fn004">
<sup>&#x2021;</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/2888896"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/visualization/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>McKenna</surname>
<given-names>Jason</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Palter</surname>
<given-names>Jaime B.</given-names>
</name>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/688779"/>
<role content-type="https://credit.niso.org/contributor-roles/conceptualization/"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/investigation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Parker</surname>
<given-names>Alex</given-names>
</name>
<xref ref-type="aff" rid="aff10">
<sup>10</sup>
</xref>
<xref ref-type="aff" rid="aff11">
<sup>11</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/2992349"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Addey</surname>
<given-names>Charles I.</given-names>
</name>
<xref ref-type="aff" rid="aff12">
<sup>12</sup>
</xref>
<xref ref-type="author-notes" rid="fn004">
<sup>&#x2021;</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/1201600"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Boone</surname>
<given-names>Wieter</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/454882"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Bhuyan</surname>
<given-names>Paban</given-names>
</name>
<xref ref-type="aff" rid="aff13">
<sup>13</sup>
</xref>
<xref ref-type="author-notes" rid="fn004">
<sup>&#x2021;</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/2889079"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Buck</surname>
<given-names>Justin J. H.</given-names>
</name>
<xref ref-type="aff" rid="aff14">
<sup>14</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/632840"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Burger</surname>
<given-names>Eugene F.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/632339"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Burris</surname>
<given-names>James</given-names>
</name>
<xref ref-type="aff" rid="aff14">
<sup>14</sup>
</xref>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Camus</surname>
<given-names>Lionel</given-names>
</name>
<xref ref-type="aff" rid="aff15">
<sup>15</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/1133718"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>de Young</surname>
<given-names>Brad</given-names>
</name>
<xref ref-type="aff" rid="aff16">
<sup>16</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/632020"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>du Plessis</surname>
<given-names>Marcel</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
<xref ref-type="author-notes" rid="fn003">
<sup>&#x2020;</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/2302602"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Flanigan</surname>
<given-names>Mike</given-names>
</name>
<xref ref-type="aff" rid="aff17">
<sup>17</sup>
</xref>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Foltz</surname>
<given-names>Gregory R.</given-names>
</name>
<xref ref-type="aff" rid="aff18">
<sup>18</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/436902"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Gille</surname>
<given-names>Sarah T.</given-names>
</name>
<xref ref-type="aff" rid="aff19">
<sup>19</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/602541"/>
<role content-type="https://credit.niso.org/contributor-roles/investigation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Grare</surname>
<given-names>Laurent</given-names>
</name>
<xref ref-type="aff" rid="aff19">
<sup>19</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/1171886"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Hansen</surname>
<given-names>Jeff E.</given-names>
</name>
<xref ref-type="aff" rid="aff20">
<sup>20</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/951329"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Hole</surname>
<given-names>Lars Robert</given-names>
</name>
<xref ref-type="aff" rid="aff21">
<sup>21</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/680837"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Honda</surname>
<given-names>Makio C.</given-names>
</name>
<xref ref-type="aff" rid="aff22">
<sup>22</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/792472"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Hormann</surname>
<given-names>Verena</given-names>
</name>
<xref ref-type="aff" rid="aff19">
<sup>19</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/596882"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Kohlman</surname>
<given-names>Catherine</given-names>
</name>
<xref ref-type="aff" rid="aff23">
<sup>23</sup>
</xref>
<xref ref-type="author-notes" rid="fn004">
<sup>&#x2021;</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/2009819"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Kosaka</surname>
<given-names>Naoko</given-names>
</name>
<xref ref-type="aff" rid="aff24">
<sup>24</sup>
</xref>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Kuhn</surname>
<given-names>Carey</given-names>
</name>
<xref ref-type="aff" rid="aff25">
<sup>25</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/1083403"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/investigation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Lenain</surname>
<given-names>Luc</given-names>
</name>
<xref ref-type="aff" rid="aff19">
<sup>19</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/1224921"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Looney</surname>
<given-names>Lev</given-names>
</name>
<xref ref-type="aff" rid="aff18">
<sup>18</sup>
</xref>
<xref ref-type="aff" rid="aff26">
<sup>26</sup>
</xref>
<xref ref-type="author-notes" rid="fn004">
<sup>&#x2021;</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/2944107"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Marouchos</surname>
<given-names>Andreas</given-names>
</name>
<xref ref-type="aff" rid="aff27">
<sup>27</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/1048700"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>McGeorge</surname>
<given-names>Elizabeth K.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff28">
<sup>28</sup>
</xref>
<xref ref-type="author-notes" rid="fn003">
<sup>&#x2020;</sup>
</xref>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>McMahon</surname>
<given-names>Clive R.</given-names>
</name>
<xref ref-type="aff" rid="aff29">
<sup>29</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/115171"/>
<role content-type="https://credit.niso.org/contributor-roles/conceptualization/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Mitarai</surname>
<given-names>Satoshi</given-names>
</name>
<xref ref-type="aff" rid="aff30">
<sup>30</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/503133"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Mordy</surname>
<given-names>Calvin</given-names>
</name>
<xref ref-type="aff" rid="aff28">
<sup>28</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/650341"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Nagano</surname>
<given-names>Akira</given-names>
</name>
<xref ref-type="aff" rid="aff31">
<sup>31</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/667573"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Nicholson</surname>
<given-names>Sarah-Anne</given-names>
</name>
<xref ref-type="aff" rid="aff32">
<sup>32</sup>
</xref>
<xref ref-type="author-notes" rid="fn003">
<sup>&#x2020;</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/739534"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Nickford</surname>
<given-names>Sarah</given-names>
</name>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
<xref ref-type="author-notes" rid="fn003">
<sup>&#x2020;</sup>
</xref>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>O&#x2019;Brien</surname>
<given-names>Kevin M.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff28">
<sup>28</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/636734"/>
<role content-type="https://credit.niso.org/contributor-roles/investigation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Peddie</surname>
<given-names>David</given-names>
</name>
<xref ref-type="aff" rid="aff33">
<sup>33</sup>
</xref>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Ponsoni</surname>
<given-names>Leandro</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/1544076"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Ramasco</surname>
<given-names>Virginie</given-names>
</name>
<xref ref-type="aff" rid="aff34">
<sup>34</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/2672395"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Rozenauers</surname>
<given-names>Nick</given-names>
</name>
<xref ref-type="aff" rid="aff35">
<sup>35</sup>
</xref>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Siddle</surname>
<given-names>Elizabeth</given-names>
</name>
<xref ref-type="aff" rid="aff36">
<sup>36</sup>
</xref>
<xref ref-type="author-notes" rid="fn004">
<sup>&#x2021;</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/2915919"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Stienbarger</surname>
<given-names>Cheyenne</given-names>
</name>
<xref ref-type="aff" rid="aff37">
<sup>37</sup>
</xref>
<xref ref-type="author-notes" rid="fn003">
<sup>&#x2020;</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/2994421"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Sutton</surname>
<given-names>Adrienne J.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/353311"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Tada</surname>
<given-names>Noriko</given-names>
</name>
<xref ref-type="aff" rid="aff38">
<sup>38</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/2692794"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Thomson</surname>
<given-names>Jim</given-names>
</name>
<xref ref-type="aff" rid="aff39">
<sup>39</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/632907"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Ueki</surname>
<given-names>Iwao</given-names>
</name>
<xref ref-type="aff" rid="aff21">
<sup>21</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/629879"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Yu</surname>
<given-names>Lisan</given-names>
</name>
<xref ref-type="aff" rid="aff40">
<sup>40</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/633861"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-original-draft/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Zhang</surname>
<given-names>Chidong</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/657645"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname>Zhang</surname>
<given-names>Dongxiao</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff28">
<sup>28</sup>
</xref>
<uri xlink:href="https://loop.frontiersin.org/people/625476"/>
<role content-type="https://credit.niso.org/contributor-roles/data-curation/"/>
<role content-type="https://credit.niso.org/contributor-roles/writing-review-editing/"/>
</contrib>
</contrib-group>
<aff id="aff1">
<sup>1</sup>
<institution>Marine Environmental Services, Elysium EPL</institution>, <addr-line>Darwin, NT</addr-line>, <country>Australia</country>
</aff>
<aff id="aff2">
<sup>2</sup>
<institution>Research Institute of Environment and Livelihoods, Charles Darwin University</institution>, <addr-line>Darwin, NT</addr-line>, <country>Australia</country>
</aff>
<aff id="aff3">
<sup>3</sup>
<institution>Pacific Marine Environment Laboratory, National Oceanic and Atmospheric Administration</institution>, <addr-line>Seattle, WA</addr-line>, <country>United States</country>
</aff>
<aff id="aff4">
<sup>4</sup>
<institution>Department of Marine Sciences, University of Gothenburg</institution>, <addr-line>Gothenburg, West Gothland</addr-line>, <country>Sweden</country>
</aff>
<aff id="aff5">
<sup>5</sup>
<institution>Department of Oceanography, University of Cape Town</institution>, <addr-line>Rondebosch</addr-line>, <country>South Africa</country>
</aff>
<aff id="aff6">
<sup>6</sup>
<institution>Flanders Marine Institute (VLIZ)</institution>, <addr-line>Oostende</addr-line>, <country>Belgium</country>
</aff>
<aff id="aff7">
<sup>7</sup>
<institution>Roger F. Wicker Centre for Ocean Enterprise, The University of Southern Mississippi</institution>, <addr-line>Gulfport, MS</addr-line>, <country>United States</country>
</aff>
<aff id="aff8">
<sup>8</sup>
<institution>Naval Meteorology and Oceanography Command (CNMOC), United States Navy</institution>, <addr-line>Stennis Space Center, MS</addr-line>, <country>United States</country>
</aff>
<aff id="aff9">
<sup>9</sup>
<institution>Graduate School of Oceanography, University of Rhode Island</institution>, <addr-line>Narragansett, RI</addr-line>, <country>United States</country>
</aff>
<aff id="aff10">
<sup>10</sup>
<institution>Astraeus Ocean Systems</institution>, <addr-line>Bellingham, WA</addr-line>, <country>United States</country>
</aff>
<aff id="aff11">
<sup>11</sup>
<institution>Carl Sagan Center, SETI Institute</institution>, <addr-line>Mountain View, CA</addr-line>, <country>United States</country>
</aff>
<aff id="aff12">
<sup>12</sup>
<institution>Department of Oceanography, University of Hawai&#x2019;i at Moana</institution>, <addr-line>Honolulu, HI</addr-line>, <country>United States</country>
</aff>
<aff id="aff13">
<sup>13</sup>
<institution>Department of Marine Sciences, University of Connecticut</institution>, <addr-line>Groton, CT</addr-line>, <country>United States</country>
</aff>
<aff id="aff14">
<sup>14</sup>
<institution>Marine Autonomous Robotic Systems (MARS), National Oceanography Centre</institution>, <addr-line>Southampton</addr-line>, <country>United Kingdom</country>
</aff>
<aff id="aff15">
<sup>15</sup>
<institution>Akvaplan-niva, Digital Solutions</institution>, <addr-line>Oslo</addr-line>, <country>Norway</country>
</aff>
<aff id="aff16">
<sup>16</sup>
<institution>Physics and Physical Oceanography, Memorial University</institution>, <addr-line>St. John&#x2019;s, NL</addr-line>, <country>Canada</country>
</aff>
<aff id="aff17">
<sup>17</sup>
<institution>SeaSatellites (&#x201c;Seasats&#x201d;)</institution>, <addr-line>San Diego, CA</addr-line>, <country>United States</country>
</aff>
<aff id="aff18">
<sup>18</sup>
<institution>Atlantic Oceanographic and Meteorological Laboratory, National Oceanic and Atmospheric Administration</institution>, <addr-line>Miami, FL</addr-line>, <country>United States</country>
</aff>
<aff id="aff19">
<sup>19</sup>
<institution>Scripps Institution of Oceanography, University of California (UC) San Diego</institution>, <addr-line>La Jolla, CA</addr-line>, <country>United States</country>
</aff>
<aff id="aff20">
<sup>20</sup>
<institution>School of Earth and Oceans, University of Western Australia</institution>, <addr-line>Perth, WA</addr-line>, <country>Australia</country>
</aff>
<aff id="aff21">
<sup>21</sup>
<institution>Norwegian Meteorological Institute</institution>, <addr-line>Bergen</addr-line>, <country>Norway</country>
</aff>
<aff id="aff22">
<sup>22</sup>
<institution>Earth Surface System Research Center (ESS), Japan Agency for Marine-Earth Science and Technology (JAMSTEC)</institution>, <addr-line>Yokosuka</addr-line>, <country>Japan</country>
</aff>
<aff id="aff23">
<sup>23</sup>
<institution>School of Oceanography, University of Washington</institution>, <addr-line>Seattle, WA</addr-line>, <country>United States</country>
</aff>
<aff id="aff24">
<sup>24</sup>
<institution>NTT Space Environment and Energy Laboratories</institution>, <addr-line>Musashino, Tokyo</addr-line>, <country>Japan</country>
</aff>
<aff id="aff25">
<sup>25</sup>
<institution>Marine Mammal Laboratory, Alaska Fisheries Science Center, National Oceanic and Atmospheric Administration</institution>, <addr-line>Seattle, WA</addr-line>, <country>United States</country>
</aff>
<aff id="aff26">
<sup>26</sup>
<institution>Rosenstiel School of Marine, Atmospheric and Earth Science, University of Miami</institution>, <addr-line>Miami, FL</addr-line>, <country>United States</country>
</aff>
<aff id="aff27">
<sup>27</sup>
<institution>National Collections and Marine Infrastructure, Commonwealth Scientific and Industrial Research Organization</institution>, <addr-line>Hobart, TAS</addr-line>, <country>Australia</country>
</aff>
<aff id="aff28">
<sup>28</sup>
<institution>Cooperative Institute for Climate, Ocean and Ecosystems Studies, University of Washington</institution>, <addr-line>Seattle, WA</addr-line>, <country>United States</country>
</aff>
<aff id="aff29">
<sup>29</sup>
<institution>Integrated Marine Observing System (IMOS) Animal Tagging, Sydney Institute of Marine Science</institution>, <addr-line>Mosman, NSW</addr-line>, <country>Australia</country>
</aff>
<aff id="aff30">
<sup>30</sup>
<institution>Marine Biophysics Unit, Okinawa Institute of Science and Technology</institution>, <addr-line>Okinawa</addr-line>, <country>Japan</country>
</aff>
<aff id="aff31">
<sup>31</sup>
<institution>Center for Coupled Ocean-Atmosphere Research (CCOAR), Japan Agency for Marine-Earth Science and Technology (JAMSTEC)</institution>, <addr-line>Yokosuka</addr-line>, <country>Japan</country>
</aff>
<aff id="aff32">
<sup>32</sup>
<institution>Southern  Ocean Carbon and Climate Observatory, Council for Scientific and Industrial Research (CSIR), Cape Town</institution>, <addr-line>Western Cape</addr-line>, <country>South Africa</country>
</aff>
<aff id="aff33">
<sup>33</sup>
<institution>Environmental Department, Akvaplan-niva</institution>, <addr-line>Troms&#xf8;</addr-line>, <country>Norway</country>
</aff>
<aff id="aff34">
<sup>34</sup>
<institution>Research Department, Offshore Sensing</institution>, <addr-line>Bergen</addr-line>, <country>Norway</country>
</aff>
<aff id="aff35">
<sup>35</sup>
<institution>Ocius Technology LTD</institution>, <addr-line>Sydney, NSW</addr-line>, <country>Australia</country>
</aff>
<aff id="aff36">
<sup>36</sup>
<institution>Centre for Ocean and Atmospheric Sciences, School of Environmental Sciences, University of East Anglia (UEA)</institution>, <addr-line>Norwich</addr-line>, <country>United Kingdom</country>
</aff>
<aff id="aff37">
<sup>37</sup>
<institution>Global Ocean Monitoring and Observing Program, National Oceanic and Atmospheric Administration</institution>, <addr-line>Silver Spring, MD</addr-line>, <country>United States</country>
</aff>
<aff id="aff38">
<sup>38</sup>
<institution>Research Institute for Marine Geodynamics, Japan Agency for Marine-Earth Science and Technology (JAMSTEC)</institution>, <addr-line>Yokosuka</addr-line>, <country>Japan</country>
</aff>
<aff id="aff39">
<sup>39</sup>
<institution>Applied Physics Laboratory, University of Washington</institution>, <addr-line>Seattle, WA</addr-line>, <country>United States</country>
</aff>
<aff id="aff40">
<sup>40</sup>
<institution>Physical Oceanography, Woods Hole Oceanographic Institution</institution>, <addr-line>Woods Hole, MA</addr-line>, <country>United States</country>
</aff>
<author-notes>
<fn fn-type="edited-by">
<p>Edited by: Gilles Reverdin, Centre National de la Recherche Scientifique (CNRS), France</p>
</fn>
<fn fn-type="edited-by">
<p>Reviewed by: Zhixuan Feng, East China Normal University, China</p>
<p>Laurent Coppola, UMR7093 Laboratoire d&#x2019;Oc&#xe9;anographie de Villefranche (LOV), France</p>
</fn>
<fn fn-type="corresp" id="fn001">
<p>*Correspondence: Ruth G. Patterson, <email xlink:href="mailto:patterson.ruth@gmail.com">patterson.ruth@gmail.com</email>
</p>
</fn>
<fn fn-type="other" id="fn003">
<p>&#x2020;Early Career Research Professional authors (within 10 yrs of completion of PhD)</p>
</fn>
<fn fn-type="other" id="fn004">
<p>&#x2021;Student Authors</p>
</fn>
</author-notes>
<pub-date pub-type="epub">
<day>07</day>
<month>03</month>
<year>2025</year>
</pub-date>
<pub-date pub-type="collection">
<year>2025</year>
</pub-date>
<volume>12</volume>
<elocation-id>1523585</elocation-id>
<history>
<date date-type="received">
<day>06</day>
<month>11</month>
<year>2024</year>
</date>
<date date-type="accepted">
<day>10</day>
<month>02</month>
<year>2025</year>
</date>
</history>
<permissions>
<copyright-statement>Copyright &#xa9; 2025 Patterson, Cronin, Swart, Beja, Edholm, McKenna, Palter, Parker, Addey, Boone, Bhuyan, Buck, Burger, Burris, Camus, de Young, du Plessis, Flanigan, Foltz, Gille, Grare, Hansen, Hole, Honda, Hormann, Kohlman, Kosaka, Kuhn, Lenain, Looney, Marouchos, McGeorge, McMahon, Mitarai, Mordy, Nagano, Nicholson, Nickford, O&#x2019;Brien, Peddie, Ponsoni, Ramasco, Rozenauers, Siddle, Stienbarger, Sutton, Tada, Thomson, Ueki, Yu, Zhang and Zhang</copyright-statement>
<copyright-year>2025</copyright-year>
<copyright-holder>Patterson, Cronin, Swart, Beja, Edholm, McKenna, Palter, Parker, Addey, Boone, Bhuyan, Buck, Burger, Burris, Camus, de Young, du Plessis, Flanigan, Foltz, Gille, Grare, Hansen, Hole, Honda, Hormann, Kohlman, Kosaka, Kuhn, Lenain, Looney, Marouchos, McGeorge, McMahon, Mitarai, Mordy, Nagano, Nicholson, Nickford, O&#x2019;Brien, Peddie, Ponsoni, Ramasco, Rozenauers, Siddle, Stienbarger, Sutton, Tada, Thomson, Ueki, Yu, Zhang and Zhang</copyright-holder>
<license xlink:href="http://creativecommons.org/licenses/by/4.0/">
<p>This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.</p>
</license>
</permissions>
<abstract>
<p>Observing air-sea interactions on a global scale is essential for improving Earth system forecasts. Yet these exchanges are challenging to quantify for a range of reasons, including extreme conditions, vast and remote under-sampled locations, requirements for a multitude of co-located variables, and the high variability of fluxes in space and time. Uncrewed Surface Vehicles (USVs) present a novel solution for measuring these crucial air-sea interactions at a global scale. Powered by renewable energy (e.g., wind and waves for propulsion, solar power for electronics), USVs have provided navigable and persistent observing capabilities over the past decade and a half. In our review of 200 USV datasets and 96 studies, we found USVs have observed a total of 33 variables spanning physical, biogeochemical, biological and ecological processes at the air-sea transition zone. We present a map showing the global proliferation of USV adoption for scientific ocean observing. This review, carried out under the auspices of the &#x2018;Observing Air-Sea Interactions Strategy&#x2019; (OASIS), makes the case for a permanent USV network to complement the mature and emerging networks within the Global Ocean Observing System (GOOS). The Observations Coordination Group (OCG) overseeing GOOS has identified ten attributes of an <italic>in-situ</italic> global network. Here, we discuss and evaluate the maturation of the USV network towards meeting these attributes. Our article forms the basis of a roadmap to formalise and guide the global USV community towards a novel and integrated ocean observing frontier.</p>
</abstract>
<kwd-group>
<kwd>Uncrewed Surface Vehicle (USV)</kwd>
<kwd>Autonomous Surface Vessel (ASV)</kwd>
<kwd>Air-sea interactions</kwd>
<kwd>Global Ocean Observing System (GOOS)</kwd>
<kwd>
<italic>In situ</italic> ocean observing system</kwd>
<kwd>Essential Ocean Variables (EOV)</kwd>
<kwd>Essential Climate Variables (ECV)</kwd>
<kwd>weather observation</kwd>
</kwd-group>
<counts>
<fig-count count="5"/>
<table-count count="2"/>
<equation-count count="0"/>
<ref-count count="148"/>
<page-count count="23"/>
<word-count count="10330"/>
</counts>
<custom-meta-wrap>
<custom-meta>
<meta-name>section-in-acceptance</meta-name>
<meta-value>Ocean Observation</meta-value>
</custom-meta>
</custom-meta-wrap>
</article-meta>
</front>
<body>
<sec id="s1" sec-type="intro">
<label>1</label>
<title>Introduction</title>
<p>The ocean plays a central role in the Earth&#x2019;s cycles of energy, water, gases, and biogeochemistry, influencing weather and climate, biodiversity, and human activities. The ocean surface is an especially important part of the Earth system as it is the interface between the ocean and the atmosphere (<xref ref-type="bibr" rid="B15">Centurioni et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B133">Wanninkhof et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B28">Cronin et&#xa0;al., 2019</xref>). Here, momentum, energy (heat), freshwater, and gases (e.g., climate-critical greenhouse gases) are exchanged between the ocean and atmosphere. These air-sea fluxes act as a force on the ocean, driving ocean circulation and changing the environmental properties and chemistry of the marine biosphere, while at the same time influencing the atmosphere, with impacts on weather and climate. Quantifying these air-sea exchanges is essential to understanding the weather-climate system and the Earth&#x2019;s energy budget, forecasting weather and climate, tracking the role of the ocean in sequestering anthropogenic carbon dioxide (CO<sub>2</sub>), and investigating a range of biological and biogeochemical processes. Despite its importance, the world&#x2019;s air-sea exchanges remain minimally observed.</p>
<p>The surface ocean is prone to harsh sampling conditions from both the atmosphere (e.g., high winds, temperature, rain, snow, and ice) and the surface ocean (e.g., large waves, spray, sea ice, and strong currents) particularly in wintertime. These, plus the remoteness of the majority of the world&#x2019;s oceans, have hindered data collection at the air-sea interface for decades. Air-sea interactions are complex to monitor, requiring measurements of multiple <italic>in-situ</italic> co-located state variables simultaneously by a suite of instrumentation positioned near the surface ocean and lower atmosphere. Air-sea fluxes often have high temporal and spatial variability that are difficult to sufficiently sample by lone ships or moorings; ocean heating of the atmosphere can lead to rapid convective processes, resulting in gustiness, cold-pool downdrafts, and highly-variable surface conditions (<xref ref-type="bibr" rid="B138">Wills et&#xa0;al., 2023</xref>). Likewise, oceanic or atmospheric fronts, and eddies and storms can result in disequilibrium between the ocean and atmosphere (<xref ref-type="bibr" rid="B112">Seo et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B90">Nicholson et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B28">Cronin et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B122">Swart et&#xa0;al., 2019</xref>), making it difficult to infer one from the other.</p>
<p>For over three decades, the Global Ocean Observing System (GOOS) has led a coordinated international effort to build global ocean observing capability (<xref ref-type="bibr" rid="B63">IOC 2018</xref>). This has included growing capacity for observing the air-sea interface. At present, there are only 25 air-sea flux moorings distributed globally as part of the OceanSITES GOOS network (<xref ref-type="bibr" rid="B29">Cronin et&#xa0;al., 2023</xref>). As an acknowledgment of the under-sampled air-sea interface, this is expected to increase as the Tropical Pacific Observing System (TPOS) begins to implement recommendations made by the international community (<xref ref-type="bibr" rid="B26">Cravatte et&#xa0;al., 2016</xref>). With advances in computational power and the applications of artificial intelligence and machine learning, higher spatio-temporal resolutions of the air-sea interface could deliver an ever-expanding list of insights and services than the existing global-scale air-sea flux coverage (<xref ref-type="bibr" rid="B115">Sloyan et&#xa0;al., 2018</xref>). Satellites and numerical models currently have resolutions that are too low to adequately capture or resolve detailed processes, which are required for weather-scale variability and validating assumptions across time and space (<xref ref-type="bibr" rid="B44">Gentemann et&#xa0;al., 2020a</xref>). The inherent challenge of quantifying air-sea fluxes lies in balancing the need for capturing high spatio-temporal resolution in variable conditions, with broad-scale global-mean coverage.</p>
<sec id="s1_1">
<label>1.1</label>
<title>A new era of ocean data collection with USVs</title>
<p>Uncrewed Surface Vehicles (USV; <xref ref-type="fig" rid="f1">
<bold>Figure&#xa0;1</bold>
</xref>) present a transformative solution to improving high-resolution observations in variable conditions, whilst delivering broad-scale coverage of the global ocean surface. Renewable-energy powered USVs can traverse tens of thousands of kilometres unassisted, simultaneously collecting data at high frequencies and thus solving the high-resolution and broad scale juxtaposition required for air-sea interaction observations. USVs enable navigable access to extreme environmental conditions such as tropical cyclones, winter storms and polar ice, which are typically under-sampled due to safety concerns and sparsely located (or absent) fixed moorings. Multiple oceanographic and atmospheric sensors can be remotely operated to simultaneously collect the essential ocean and climate variables necessary to calculate air-sea fluxes. Almost any instrument-based sensor can potentially be integrated, creating a multidisciplinary platform for ocean monitoring (<xref ref-type="bibr" rid="B96">Patterson et&#xa0;al., 2022</xref>), spanning ecology, biology, chemistry, physical oceanography, and atmospheric science. A USV&#x2019;s position at the surface allows constant connectivity, near real-time data relays and access to wind, wave, and solar energy for propulsion and powering sensors. As USVs become more affordable, the implementation of multiple USVs used as force multipliers alongside other crewed or uncrewed vessels will significantly increase spatio-temporal efficiency, reducing the cost and increasing the accuracy of broad-scale surveys.</p>
<fig id="f1" position="float">
<label>Figure&#xa0;1</label>
<caption>
<p>A sample of commercially available USVs, scaled to USV length, illustrating a wide-ranging ecosystem of high technology readiness level. These USVs are renewable powered, persistent, variable in cost and complexity that individually are suited to specific tasks and collectively to a range of different environments and variable conditions.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-12-1523585-g001.tif"/>
</fig>
<p>USVs have recently become a reliable way to access extreme and remote environments including tropical cyclones (<xref ref-type="bibr" rid="B73">Lenain and Melville, 2014</xref>; <xref ref-type="bibr" rid="B81">Mitarai and McWilliams, 2016</xref>; <xref ref-type="bibr" rid="B62">Ino et&#xa0;al., 2021</xref>), major hurricanes (<xref ref-type="bibr" rid="B42">Foltz et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B145">Zhang et&#xa0;al., 2023a</xref>, <xref ref-type="bibr" rid="B143">b</xref>; <xref ref-type="bibr" rid="B141">Yu et&#xa0;al., 2023</xref>), atmospheric cold pools (<xref ref-type="bibr" rid="B137">Wills et&#xa0;al., 2021</xref>, <xref ref-type="bibr" rid="B138">2023</xref>), volcanically active areas where crewed ship operations are restricted (<xref ref-type="bibr" rid="B124">Tada et&#xa0;al., 2024</xref>), and in seasonally sea-ice covered polar seas (<xref ref-type="bibr" rid="B139">Wood et&#xa0;al., 2013</xref>; <xref ref-type="bibr" rid="B121">Swart et&#xa0;al., 2020</xref>; <xref ref-type="bibr" rid="B19">Chiodi et&#xa0;al., 2021</xref>; <xref ref-type="bibr" rid="B38">Du Plessis et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B36">Drushka et&#xa0;al., 2024</xref>; <xref ref-type="bibr" rid="B114">Sivam et&#xa0;al., 2024</xref>). USVs have also collected wave measurements in winter storms and hurricanes (<xref ref-type="bibr" rid="B60">Hole et&#xa0;al., 2016</xref>; <xref ref-type="bibr" rid="B91">Nickford et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B145">Zhang et&#xa0;al., 2023a</xref>), current profiles in the North Sea and Chukchi Sea (<xref ref-type="bibr" rid="B140">Wullenweber et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B17">Chi et&#xa0;al., 2023</xref>), wintertime storm-front interactions (<xref ref-type="bibr" rid="B91">Nickford et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B129">Toolsee et&#xa0;al., 2024</xref>), and have crossed entire ocean basins (<xref ref-type="bibr" rid="B132">Villareal and Wilson, 2014</xref>; <xref ref-type="bibr" rid="B48">Goebel et&#xa0;al., 2014</xref>) as well as circumnavigated Antarctica (<xref ref-type="bibr" rid="B90">Nicholson et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B119">Sutton et&#xa0;al., 2021</xref>). Even a single USV can be used to survey fronts and eddies, if air-sea flux measurements are combined to extrapolate sea surface temperature (SST) to a &#x2018;foundational SST&#x2019; below the daytime stratification that occurs on sunny days with low winds (<xref ref-type="bibr" rid="B30">Cronin et&#xa0;al., 2024</xref>). USV adoption has also forged new disciplinary capabilities by providing reduced-noise platforms for multiple types of acoustic monitoring (<xref ref-type="bibr" rid="B58">Hildebrand et&#xa0;al., 2013</xref>, <xref ref-type="bibr" rid="B57">2014</xref>; <xref ref-type="bibr" rid="B94">Pagniello et&#xa0;al., 2019</xref>), which is also complementary to fisheries research and operations (<xref ref-type="bibr" rid="B85">Mordy et&#xa0;al., 2017</xref>; <xref ref-type="bibr" rid="B53">Handegard et&#xa0;al., 2024</xref>), and have been used and designed for cost-effective maritime domain awareness (<xref ref-type="bibr" rid="B93">Nothacker, 2024</xref>), including for surveillance of remote marine protected areas (<xref ref-type="bibr" rid="B2">Angus et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B82">Molina-Molina et&#xa0;al., 2021</xref>). USVs have allowed an expanded footprint for ocean observing into extreme environments that challenge crewed vessels.</p>
<p>USV manufacturers, universities, and research institutions worldwide have pioneered groundbreaking USV capabilities, yielding valuable data and insights into this technology&#x2019;s capabilities (<xref ref-type="table" rid="T1">
<bold>Table&#xa0;1</bold>
</xref>). However, progress has been siloed within individual projects, reducing the potential for collective knowledge-building. The absence of standardised data collection, processing, disseminating and storage practices further hinders adoption and advancement of the USV industry for the benefit of society. Such complexities are not unique in ocean data collection, and previously, capacity development has been effectively progressed by taking a globally coordinated approach to data collection, management, and distribution. Such is the case with the 15 <italic>in-situ</italic> ocean observing networks within GOOS, including OceanSITES, Argo, drifters, OceanGliders, and Surface Ocean CO<sub>2</sub> Observing Network (SOCONET), which approach global ocean observing under ten Observations Coordination Group (OCG) attributes to meet the needs of the global ocean observing community (<xref ref-type="bibr" rid="B49">GOOS, 2018</xref>).</p>
<table-wrap id="T1" position="float">
<label>Table&#xa0;1</label>
<caption>
<p>Scientific publications since 2010 that utilise USV datasets within nine generalised fields of study.</p>
</caption>
<table frame="hsides">
<thead>
<tr>
<th valign="top" align="center">Discipline</th>
<th valign="top" align="center">Field of Study</th>
<th valign="top" align="center">Peer reviewed publications using USV datasets</th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" rowspan="7" align="center">Physical Ocean and Atmosphere<break/>*Includes air- sea CO2 flux calculations</td>
<td valign="top" align="left">Fluxes and air-sea interactions</td>
<td valign="top" align="left">*<xref ref-type="bibr" rid="B129">Toolsee et&#xa0;al., 2024</xref>; *<xref ref-type="bibr" rid="B92">Nickford et&#xa0;al., 2024</xref>; <xref ref-type="bibr" rid="B114">Sivam et&#xa0;al., 2024</xref>; <xref ref-type="bibr" rid="B102">Reeves Eyre et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B64">Iyer et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B88">Nagano et&#xa0;al., 2022a</xref>; *<xref ref-type="bibr" rid="B90">Nicholson et&#xa0;al., 2022</xref>; *<xref ref-type="bibr" rid="B91">Nickford et&#xa0;al., 2022</xref>; *<xref ref-type="bibr" rid="B146">Zhang et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B51">Grare et&#xa0;al., 2021</xref>; <xref ref-type="bibr" rid="B113">Siddle et&#xa0;al., 2021</xref>; *<xref ref-type="bibr" rid="B119">Sutton et&#xa0;al., 2021</xref>; <xref ref-type="bibr" rid="B144">Zhang et&#xa0;al., 2019a</xref>; *<xref ref-type="bibr" rid="B83">Monteiro et&#xa0;al., 2015</xref>; <xref ref-type="bibr" rid="B39">Edholm et&#xa0;al., 2022</xref> in prep.</td>
</tr>
<tr>
<td valign="top" align="left">Tropical cyclone and extreme winds, including air-sea interactions</td>
<td valign="top" align="left">
<xref ref-type="bibr" rid="B18">Chiodi et&#xa0;al., 2024</xref>; <xref ref-type="bibr" rid="B69">Kosaka et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B141">Yu et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B145">Zhang et&#xa0;al., 2023a</xref>, <xref ref-type="bibr" rid="B143">b</xref>; <xref ref-type="bibr" rid="B42">Foltz et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B80">Miles et&#xa0;al., 2021</xref>; <xref ref-type="bibr" rid="B81">Mitarai and McWilliams, 2016</xref>; <xref ref-type="bibr" rid="B73">Lenain and Melville, 2014</xref>
</td>
</tr>
<tr>
<td valign="top" align="left">Meso and submeso- scale processes</td>
<td valign="top" align="left">
<sup>1</sup>Bhuyan et al.; <xref ref-type="bibr" rid="B30">Cronin et&#xa0;al., 2024</xref>; <xref ref-type="bibr" rid="B17">Chi et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B59">Hodges et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B120">Swart et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B138">Wills et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B38">Du Plessis et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B89">Nagano et&#xa0;al., 2022b</xref>; <xref ref-type="bibr" rid="B140">Wullenweber et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B137">Wills et&#xa0;al., 2021</xref>; <xref ref-type="bibr" rid="B45">Gentemann et&#xa0;al., 2020b</xref>; <xref ref-type="bibr" rid="B87">Nagano and Ando, 2020</xref>; <xref ref-type="bibr" rid="B121">Swart et&#xa0;al., 2020</xref>; <xref ref-type="bibr" rid="B131">Vazquez-Cuervo et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B147">Zhang et&#xa0;al., 2019b</xref>; <xref ref-type="bibr" rid="B71">Krug et&#xa0;al., 2017</xref>
</td>
</tr>
<tr>
<td valign="top" align="left">Marginal sea ice</td>
<td valign="top" align="left">
<xref ref-type="bibr" rid="B36">Drushka et&#xa0;al., 2024</xref>; <xref ref-type="bibr" rid="B27">Crews et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B19">Chiodi et&#xa0;al., 2021</xref>; <xref ref-type="bibr" rid="B148">Zhou et&#xa0;al., 2021</xref>; <xref ref-type="bibr" rid="B79">Meinig et&#xa0;al., 2015</xref>; <xref ref-type="bibr" rid="B22">Cokelet et&#xa0;al., 2015</xref>; <xref ref-type="bibr" rid="B139">Wood et&#xa0;al., 2013</xref>
</td>
</tr>
<tr>
<td valign="top" align="left">Waves</td>
<td valign="top" align="left">
<xref ref-type="bibr" rid="B1">Amador et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B24">Colosi et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B127">Thomson et&#xa0;al., 2018</xref>; <xref ref-type="bibr" rid="B60">Hole et&#xa0;al., 2016</xref>; <xref ref-type="bibr" rid="B117">Smith and Thomson, 2016</xref>
</td>
</tr>
<tr>
<td valign="top" align="left">Oceanic boundary layer</td>
<td valign="top" align="left">
<xref ref-type="bibr" rid="B65">Jia and Minnett, 2023</xref>; <xref ref-type="bibr" rid="B66">Jia et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B142">Zeiden et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B39">Edholm et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B110">Scott et&#xa0;al., 2020</xref>; <xref ref-type="bibr" rid="B109">Schmidt et&#xa0;al., 2017</xref>; <xref ref-type="bibr" rid="B46">Ghani et&#xa0;al., 2014</xref>; <xref ref-type="bibr" rid="B132">Villareal and Wilson, 2014</xref>; <xref ref-type="bibr" rid="B32">Daniel et&#xa0;al., 2011</xref>; <xref ref-type="bibr" rid="B86">Mullsion et&#xa0;al., 2011</xref>
</td>
</tr>
<tr>
<td valign="top" align="left">Geodesy</td>
<td valign="top" align="left">
<xref ref-type="bibr" rid="B61">Iinuma et&#xa0;al., 2021</xref>; <xref ref-type="bibr" rid="B62">Ino et&#xa0;al., 2021</xref>; <xref ref-type="bibr" rid="B108">Sakic et&#xa0;al., 2021</xref>; <xref ref-type="bibr" rid="B43">Foster et&#xa0;al., 2020</xref>; <xref ref-type="bibr" rid="B98">Penna et&#xa0;al., 2018</xref>; <xref ref-type="bibr" rid="B8">Berger et&#xa0;al., 2016</xref>
</td>
</tr>
<tr>
<td valign="top" align="center" rowspan="2">Biology and ecology</td>
<td valign="top" align="left">Passive acoustics</td>
<td valign="top" align="left">
<xref ref-type="bibr" rid="B12">Camus et&#xa0;al., 2021</xref>; <xref ref-type="bibr" rid="B34">de Robertis et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B94">Pagniello et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B25">Crance et&#xa0;al., 2016</xref>; <xref ref-type="bibr" rid="B33">Davis et&#xa0;al., 2016</xref>; <xref ref-type="bibr" rid="B57">Hildebrand et&#xa0;al., 2014</xref>, <xref ref-type="bibr" rid="B58">2013</xref>; <xref ref-type="bibr" rid="B9">Bingham et&#xa0;al., 2012</xref>; <xref ref-type="bibr" rid="B135">Wiggins, 2009</xref>; <xref ref-type="bibr" rid="B84">Moore et&#xa0;al., 2007</xref>
</td>
</tr>
<tr>
<td valign="top" align="left">Biomass/ecology</td>
<td valign="top" align="left">
<xref ref-type="bibr" rid="B53">Handegard et&#xa0;al., 2024</xref>; <xref ref-type="bibr" rid="B101">Preston et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B4">Bandara et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B35">de Robertis et&#xa0;al., 2021</xref>; <xref ref-type="bibr" rid="B37">Dunn et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B100">Premus et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B74">Levine et&#xa0;al., 2021</xref>; <xref ref-type="bibr" rid="B20">Chu et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B97">Pedersen et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B85">Mordy et&#xa0;al., 2017</xref>; <xref ref-type="bibr" rid="B123">Swart et&#xa0;al., 2016</xref>; <xref ref-type="bibr" rid="B48">Goebel et&#xa0;al., 2014</xref>; <xref ref-type="bibr" rid="B52">Guihen et&#xa0;al., 2014</xref>
</td>
</tr>
</tbody>
</table>
<table-wrap-foot>
<fn>
<p>We have listed each publication under the main field of study to reduce replication, however some publications discuss multiple fields of study.</p>
<p>
<sup>1</sup>Bhuyan, P., Rocha, C. B., Romero, L., and Farrar, J. T. Acoustic Doppler Current Profiler measurements from Saildrones, with applications to submesoscale studies. Earth ArXiv. doi: 10.31223/X5SX30</p>
<p>*Includes air-sea CO2 flux calculations.</p>
</fn>
</table-wrap-foot>
</table-wrap>
</sec>
<sec id="s1_2">
<label>1.2</label>
<title>Towards a permanent, global USV network</title>
<p>The scientific and USV industry communities have appealed for a globally coordinated approach to USV-based ocean monitoring (<xref ref-type="bibr" rid="B21">Clayson et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B29">Cronin et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B134">Whitt et&#xa0;al., 2020</xref>; <xref ref-type="bibr" rid="B28">Cronin et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B133">Wanninkhof et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B15">Centurioni et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B78">Meinig et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B47">Gille et&#xa0;al., 2016</xref>). Adopting a global network approach will transform the patchwork of independent USV projects into an established and trusted capability. As such, a &#x2018;USV Network for GOOS&#x2019; has been established as an endorsed UN Ocean Decade project linked to the Observing Air-Sea Interaction Strategy (OASIS) UN Ocean Decade programme, to serve as a starting point for a permanent global USV network. This initiative aims to evolve the existing USV scientific data collection community into a coordinated entity with clear objectives and priorities, to be endorsed by the GOOS OCG as an emerging network. To achieve this, the USV Network for GOOS will demonstrate the network&#x2019;s progress towards meeting the ten OCG attributes (<xref ref-type="fig" rid="f2">
<bold>Figure&#xa0;2</bold>
</xref>). Below, we discuss each attribute in detail in the context of the existing GOOS OCG networks.</p>
<fig id="f2" position="float">
<label>Figure&#xa0;2</label>
<caption>
<p>Progress on the Observations Coordination Group Attributes of the Global Ocean Observing System networks. Attributes are listed in order of most progressed (green), progressing (yellow), and least progressed (red).</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-12-1523585-g002.tif"/>
</fig>
</sec>
</sec>
<sec id="s2">
<label>2</label>
<title>Network purpose and scope</title>
<p>The primary purpose of the global USV network is to expand and complement the existing GOOS observing capability by improving ocean surface monitoring at small spatio-temporal scales unable to be captured by satellites and mooring arrays, whilst monitoring broadly scales of up to tens of thousands of kilometres. This will improve multidisciplinary observations within GOOS that are currently absent or cost prohibitive. The scope of the USV network will include prioritising core oceanographic and atmospheric observations associated with the energy, water, carbon, and life cycles needed to make transformational advances in weather and climate forecasting.</p>
<p>The network will complement the existing GOOS OCG networks through: (1) Increased observations of multiple co-located air-sea interaction and biogeochemical variables, including many under-sampled Essential Ocean Variables (EOVs) and Essential Climate Variables (ECVs); (2) Expanded sampling in dangerous weather and extreme events, including during high winds and variable sea states; (3) Targeted locational sampling to reach under-sampled areas such as high latitudes, remote tropics,continental shelf, and other areas that are cost-prohibitive to access; (4) Technological Advancement: Fostering a cooperative community to advance USV technology, sharing lessons on sensor integration and interoperability.</p>
</sec>
<sec id="s3">
<label>3</label>
<title>Progress on the OCG attributes</title>
<p>In this section we evaluate the ten attributes of a GOOS network as outlined by the OCG, highlighting current capabilities of the USV community network and where progress is needed.</p>
<sec id="s3_1">
<label>3.1</label>
<title>Attribute 1: Global in scale</title>
<p>Comprehensive global coverage of the open ocean using a range of USV archetypes is already making significant contributions to scientific ocean observations. To highlight this proliferation, we produced global USV coverage maps (<xref ref-type="fig" rid="f3">
<bold>Figure&#xa0;3</bold>
</xref>) using metadata (longitude, latitude, date, time) contributions from USV manufacturers, authors of published USV papers, and this paper&#x2019;s co-authors&#x2019; professional networks. This has resulted in 200 USV datasets collected between 2011 and 2024 (<xref ref-type="fig" rid="f3">
<bold>Figure&#xa0;3</bold>
</xref>), although USV manufacturers indicated that significantly more data exist with commercial clients.</p>
<fig id="f3" position="float">
<label>Figure&#xa0;3</label>
<caption>
<p>USV global ocean coverage maps from 2011 to 2024 as tracks <bold>(A)</bold> and density <bold>(B)</bold>. Latitude-time heat map of count of daily USV observations in 5&#xb0; latitude bins <bold>(C)</bold>. <bold>(D)</bold> Cumulated count of USV observations as a function of latitude. Relative (left vertical axis) and cumulative (right vertical axis) counts of daily observations per month per 5&#xb0; latitude <bold>(E)</bold>.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-12-1523585-g003.tif"/>
</fig>
<p>The global coverage maps indicate tremendous potential to fill observational gaps in remote regions of the ocean, such as the Pacific Ocean and higher latitudes (<xref ref-type="fig" rid="f3">
<bold>Figures&#xa0;3A, B</bold>
</xref>). They also illustrate locations where USVs have not yet been used, such as in the Indian Ocean and South Atlantic. The steady increase in USV adoption over time (<xref ref-type="fig" rid="f3">
<bold>Figures&#xa0;3C, E</bold>
</xref>) is contrasted by large interannual variability of higher and lower sampling years (<xref ref-type="fig" rid="f3">
<bold>Figure&#xa0;3E</bold>
</xref>), indicating that USV observations are not yet sustained globally. Currently, about 80% of USV observations are located in the Northern Hemisphere (<xref ref-type="fig" rid="f3">
<bold>Figure&#xa0;3C</bold>
</xref>). This bias may be attributed to the relatively higher acquisition of funding in the Northern Hemisphere compared to the south, and large, dedicated process studies, such as the Tropical Pacific Observing System (TPOS; <xref ref-type="bibr" rid="B116">Smith et&#xa0;al., 2019</xref>), tropical Atlantic hurricane observations, the Salinity Processes in the Upper Ocean Regional Study (SPURS-2; <xref ref-type="bibr" rid="B118">SPURS project, 2015</xref>; <xref ref-type="bibr" rid="B76">Lindstrom et&#xa0;al., 2015</xref>) and the Sub-Mesoscale Ocean Dynamics Experiment (S-MODE; <xref ref-type="bibr" rid="B40">Farrar et&#xa0;al., 2020</xref>).</p>
</sec>
<sec id="s3_2">
<label>3.2</label>
<title>Attribute 2: Observes one or more Essential Ocean Variables and Essential Climate Variables</title>
<p>A unique aspect of USV technology is the ability to simultaneously monitor a significant range of EOVs and ECVs within the air-sea transition zone. Unlike many OCG networks that focus on measuring a small number of EOVs extensively, the USV network will complement the existing GOOS networks by collecting unprecedented co-located variables. This will effectively expand coverage of multidisciplinary studies, physical ocean-atmospheric observations, and physical ocean-ecological and biological observations.</p>
<p>Our review of USV literature found that of the 40 unique EOVs (<ext-link ext-link-type="uri" xlink:href="https://goosocean.org/what-we-do/framework/essential-ocean-variables/">https://goosocean.org/what-we-do/framework/essential-ocean-variables/</ext-link>) and ECVs (<ext-link ext-link-type="uri" xlink:href="https://gcos.wmo.int/en/essential-climate-variables/table">https://gcos.wmo.int/en/essential-climate-variables/table</ext-link>) 26 have been measured using USVs, plus a further five variables not listed as EOVs or ECVs (<xref ref-type="table" rid="T2"><bold>Table 2</bold></xref>). The maximum number of variables monitored during a single USV deployment was 18, comprising wave height and period (sea state), skin temperature, subsurface temperature, salinity, currents, dissolved oxygen, biomass, ocean sound, atmospheric pressure, longwave and shortwave radiation, air temperature, humidity, wind velocity, seawater and air <italic>p</italic>CO<sub>2</sub>, coloured dissolved organic matter, and chlorophyll-a fluorometry (<xref ref-type="bibr" rid="B144">Zhang et&#xa0;al., 2019a</xref>). Sustained high-resolution data collection is possible due to USVs&#x2019; large payloads, large power capacity aided by renewable energy (e.g. wind and solar), sustained ample computing power, large data storage capacity for high-resolution data, and near real-time data relay typically packaged into 1-minute to 10-minute averages (<xref ref-type="bibr" rid="B59">Hodges et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B42">Foltz et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B102">Reeves Eyre et&#xa0;al., 2023</xref>).</p>
<sec id="s3_2_1">
<label>3.2.1</label>
<title>Air-sea interactions</title>
<p>The majority of USV studies in the literature aimed to quantify air-sea exchange of heat, momentum, freshwater, and CO<sub>2</sub> (<xref ref-type="table" rid="T1">
<bold>Table&#xa0;1</bold>
</xref>). These studies typically measure &gt;8 covariables (<xref ref-type="bibr" rid="B23">Colbo and Weller, 2009</xref>) of the physical EOVs and ocean ECVs. High-resolution (&gt;10 Hz) observations were collected in the majority of cases, which allowed for calculating turbulent fluxes via direct covariances, which are critical for air-sea interactions. Reducing the influence of the ship microclimate on air-sea boundary layer observations has been an important benefit of collecting EOVs and ECVs with USVs as opposed to ship-based observations. Crewed ships use variable air and sea intakes at 0.5 - 8 m above and below the ocean surface, whereas USV intakes can be varied more easily and are consistently closer to 0.5 - 5 m above and 0.1 - 7 m below the ocean surface, closer to the interface microlayer that governs fluxes (<xref ref-type="bibr" rid="B36">Drushka et&#xa0;al., 2024</xref>; <xref ref-type="bibr" rid="B144">Zhang et&#xa0;al., 2019a</xref>). The integration of an electronic precipitation gauge to a USV (<xref ref-type="bibr" rid="B51">Grare et&#xa0;al., 2021</xref>) is a promising step towards comprehensive measurements of air-sea interactions, though there are notable limitations to these approaches during high sea states due to interference from sea spray. The advantages of USVs for reaching high-resolution, fine-scale spatio-temporal physical processes and broadscale coverage is well documented (see <xref ref-type="table" rid="T1">
<bold>Table&#xa0;1</bold>
</xref>).</p>
</sec>
<sec id="s3_2_2">
<label>3.2.2</label>
<title>Biological and ecological</title>
<p>A promising opportunity lies in the USV uptake for observing instrument-based ecological and biological variables such as eDNA (<xref ref-type="bibr" rid="B101">Preston et&#xa0;al., 2023</xref>), primary productivity (<xref ref-type="bibr" rid="B55">Hemsley et&#xa0;al., 2015</xref>), zooplankton (<xref ref-type="bibr" rid="B97">Pedersen et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B52">Guihen et&#xa0;al., 2014</xref>), phytoplankton biomass (<xref ref-type="bibr" rid="B110">Scott et&#xa0;al., 2020</xref>), phytoplankton abundance, community structure, and harmful algal blooms (<xref ref-type="bibr" rid="B111">Seegers et&#xa0;al., 2015</xref>). These are important and under-sampled components of GOOS (<xref ref-type="bibr" rid="B70">Koslow and Couture, 2015</xref>). The emerging instrument-based, underway net primary productivity measurements, enabled by gas tension devices (<xref ref-type="bibr" rid="B31">Cynar et&#xa0;al., 2022</xref>), also offers a promising pathway to expand USV ecological data collection.</p>
<p>USVs have been equipped with hydrophones to monitor and track seasonal changes in the distributions of sound producing marine mammals (<xref ref-type="bibr" rid="B84">Moore et&#xa0;al., 2007</xref>; <xref ref-type="bibr" rid="B33">Davis et&#xa0;al., 2016</xref>; <xref ref-type="bibr" rid="B100">Premus et&#xa0;al., 2022</xref>), occasionally other ocean life (<xref ref-type="bibr" rid="B94">Pagniello et&#xa0;al., 2019</xref>) and anthropogenic sound (<xref ref-type="bibr" rid="B12">Camus et&#xa0;al., 2021</xref>). Early studies using autonomous vehicles focused on documenting detections of marine animals, while more recent work has shifted toward examining how co-located oceanographic variables relate to observed patterns in presence, absence, or distribution (<xref ref-type="bibr" rid="B5">Baumgartner et&#xa0;al., 2014</xref>; <xref ref-type="bibr" rid="B3">Aniceto et&#xa0;al., 2020</xref>). These case-studies demonstrate USV capability to monitor co-located physical variables with: biogeochemical, biological and ecological variables. This co-located sampling has the potential to grow interdisciplinary marine studies and may help solve key scientific questions, such as determining the role of physical processes in marine movement behaviour (<xref ref-type="bibr" rid="B54">Hays et&#xa0;al., 2016</xref>).</p>
</sec>
<sec id="s3_2_3">
<label>3.2.3</label>
<title>Opportunistic monitoring</title>
<p>The inherent ability of USVs to collect and store multidisciplinary data makes them highly versatile and ideal for opportunistic data collection, which is a major opportunity for the USV network. For example, a 2011 expedition that used four wave gliders yielded data for three different disciplines: surface ocean (<xref ref-type="bibr" rid="B132">Villareal and Wilson, 2014</xref>), acoustics (biomass; <xref ref-type="bibr" rid="B48">Goebel et&#xa0;al., 2014</xref>), and air-sea interactions (tropical cyclone; <xref ref-type="bibr" rid="B73">Lenain and Melville, 2014</xref>). During a study that was focused on assessing the presence of sea ice using camera footage (<xref ref-type="bibr" rid="B79">Meinig et&#xa0;al., 2015</xref>; <xref ref-type="bibr" rid="B19">Chiodi et&#xa0;al., 2021</xref>) and another of marine mammal and fish studies (<xref ref-type="bibr" rid="B72">Kuhn et&#xa0;al., 2020</xref>; <xref ref-type="bibr" rid="B85">Mordy et&#xa0;al., 2017</xref>), high-resolution (&gt;10 Hz) 3-D wind velocity measurements were collected.</p>
<table-wrap id="T2" position="float">
<label>Table&#xa0;2</label>
<caption>
<p>Essential Ocean and Climate Variables (EOVs/ECVs) observed using USVs since 2010, for nine generalised fields of study, derived from a review of scientific literature describing the adoption of USVs for open-ocean observing (see <xref ref-type="table" rid="T1">
<bold>Table&#xa0;1</bold>
</xref>).</p>
</caption>
<table frame="hsides">
<thead>
<tr>
<th valign="top" align="left"/>
<th valign="top" align="center"/>
<th valign="top" colspan="10" align="center">Fields of Study</th>
</tr>
<tr>
<th valign="top" align="left">&#xa0;</th>
<th valign="top" align="center">&#xa0;</th>
<th valign="top" align="center">Essential Ocean and Climate Variables&#xa0;</th>
<th valign="top" align="center">Air-sea interaction</th>
<th valign="top" align="center">Air-sea interaction (tropical cyclone)</th>
<th valign="top" align="center">Mesoscale, sub-mesoscale processes</th>
<th valign="top" align="center">Sea ice</th>
<th valign="top" align="center">Waves</th>
<th valign="top" align="center">Surface ocean</th>
<th valign="top" align="center">Passive acoustics</th>
<th valign="top" align="center">Geodesy</th>
<th valign="top" align="center">Biomass/ecology</th>
</tr>
</thead>
<tbody>
<tr>
<td valign="top" rowspan="30" align="left" style="background-color:#404040">
<bold>ESSENTIAL OCEAN VARIABLES</bold>
</td>
<td valign="top" rowspan="11" align="center" style="background-color:#404040">
<bold>Physics</bold>
</td>
<td valign="top" align="left">Sea state</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
</tr>
<tr>
<td valign="top" align="left">Ocean surface stress</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Sea ice</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Sea surface height</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Sea surface temperature</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
</tr>
<tr>
<td valign="top" align="left">Subsurface temperature</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
</tr>
<tr>
<td valign="top" align="left">Surface currents</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Subsurface currents</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Sea surface salinity</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
</tr>
<tr>
<td valign="top" align="left">Ocean surface heat flux</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Ocean bottom pressure</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" rowspan="7" align="center" style="background-color:#404040">
<bold>Biogeo-chemistry</bold>
</td>
<td valign="top" align="left">Oxygen</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
</tr>
<tr>
<td valign="top" align="left">Nutrients</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Inorganic carbon</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Transient tracers</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Particulate matter</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
</tr>
<tr>
<td valign="top" align="left">Nitrous oxide</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Stable carbon isotopes</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" rowspan="9" align="center" style="background-color:#404040">
<bold>Biology and Ecosystems</bold>
</td>
<td valign="top" align="left">Phytoplankton biomass and diversity</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
</tr>
<tr>
<td valign="top" align="left">Zooplankton biomass and diversity</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
</tr>
<tr>
<td valign="top" align="left">Fish abundance and distribution</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
</tr>
<tr>
<td valign="top" align="left">Seabird abundance and distribution</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Marine mammal abundance and Distribution</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Hard coral cover and composition</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Seagrass cover and composition</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Macroalgal canopy cover and composition</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Mangrove cover and composition</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" rowspan="3" align="center" style="background-color:#404040">
<bold>Cross-disciplinary</bold>
</td>
<td valign="top" align="left">Ocean colour</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
</tr>
<tr>
<td valign="top" align="left">Marine Debris (emerging)</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Ocean Sound</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
</tr>
<tr>
<td valign="top" rowspan="10" align="left" style="background-color:#404040">
<bold>ESSENTIAL CLIMATE VARIABLES</bold>
</td>
<td valign="top" rowspan="6" align="center" style="background-color:#404040">
<bold>Surface Atmosphere</bold>
</td>
<td valign="top" align="left">Precipitation</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Pressure</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
</tr>
<tr>
<td valign="top" align="left">Radiation budget</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#xa0;</td>
<td valign="top" align="center">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Temperature (temporal resolution and height above surface if known)</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
</tr>
<tr>
<td valign="top" align="left">Water Vapour</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
</tr>
<tr>
<td valign="top" align="left">Wind speed and direction</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
</tr>
<tr>
<td valign="top" rowspan="4" align="center" style="background-color:#404040">
<bold>Atmospheric composition</bold>
</td>
<td valign="top" align="left">Aerosols</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Carbon dioxide, methane and other greenhouse gases</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
</tr>
<tr>
<td valign="top" align="left">Ozone</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Precursors for aerosols and ozone</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" rowspan="5" align="left" style="background-color:#404040">
<bold>OTHER</bold>
</td>
<td valign="top" rowspan="5" align="center" style="background-color:#404040">
<bold>Other variables</bold>
</td>
<td valign="top" align="left">Imagery (surface and subsurface)</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Photosynthetically Active Radiation</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
</tr>
<tr>
<td valign="top" align="left">Magnetic field</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">Bathymetry</td>
<td valign="top" align="center">&#x2713;</td>
<td valign="top" align="center">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
</tr>
<tr>
<td valign="top" align="left">eDNA</td>
<td valign="top" align="center">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="left">&#xa0;</td>
<td valign="top" align="center">&#x2713;</td>
</tr>
</tbody>
</table>
<table-wrap-foot>
<fn>
<p>Grey text represents existing essential ocean and climate variables that have not been collected using USVs as per the existing literature.</p>
</fn>
</table-wrap-foot>
</table-wrap>
</sec>
</sec>
<sec id="s3_3">
<label>3.3</label>
<title>Attribute 3: Environmental stewardship awareness</title>
<p>USVs powered by renewable energy have entered the market in recent years due, in part, to the availability of low-cost and innovative battery technology and solar panels. Scientists have largely adopted these USVs, which are a subset of USVs that are inherently sustainable, leveraging a combination of renewable energy sources for propulsion, such as wind and wave power, or battery-electric motors charged by solar energy. Instrumentation and electronics are typically powered by solar-charged batteries, enabling USVs to operate in the open ocean for extended periods in the range of multiple months. USVs are typically integrated with large numbers of non-expendable oceanographic and meteorological instrumentation rendering these platforms high-value and therefore non-disposable. Moreover, high frequency &#x2018;delayed data&#x2019; are usually stored onboard, greatly enhancing the value of a safe return to shore. Even after sustaining damage, USVs can be navigated to port for repair (<xref ref-type="bibr" rid="B91">Nickford et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B119">Sutton et&#xa0;al., 2021</xref>).</p>
<p>While the emergence of USVs powered by renewable energy is exciting for a range of sectors, this full reliance on renewable energy sources presents limitations, particularly regarding power availability and speed of propulsion. Studies have highlighted instances where the reliance on solar power alone for propulsion and instrument operation has led to gaps in data collection (<xref ref-type="bibr" rid="B92">Nickford et&#xa0;al., 2024</xref>; <xref ref-type="bibr" rid="B19">Chiodi et&#xa0;al., 2021</xref>; <xref ref-type="bibr" rid="B74">Levine et&#xa0;al., 2021</xref>). For example, an operational project using 20 wave gliders to monitor tide levels in Japanese waters, encountered consistent difficulties due to insufficient power (<xref ref-type="bibr" rid="B62">Ino et&#xa0;al., 2021</xref>). Other projects have reported USVs with a combination of wind and electric motor propulsion unable to fight strong currents (<xref ref-type="bibr" rid="B20">Chu et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B124">Tada et&#xa0;al., 2024</xref>), limiting their use in these environments. Power limitations can also lead to ambiguity regarding data transmission frequencies, affecting the quality of the data collected and reducing the efficacy of USV adoption. <xref ref-type="bibr" rid="B81">Mitarai and McWilliams (2016)</xref> expected real-time high frequency (20 Hz) data return, however, received data at 10-minute intervals in real-time and the high-frequency data once the platform had returned to port. A marginal sea ice study in the higher latitudes required cameras to be turned off during periods of low power (<xref ref-type="bibr" rid="B19">Chiodi et&#xa0;al., 2021</xref>), or reduced power duty cycles of a mini echosounder survey to as low as 25% as day time grew shorter with the changing season (<xref ref-type="bibr" rid="B34">de Robertis et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B74">Levine et&#xa0;al., 2021</xref>). The latter would also apply when cloudiness is persistent and there are larger solar angles. While relying solely on renewable energy sources in some environments introduces limitations, USV manufacturers are integrating hybrid fuel capabilities to extend operational capability and improve reliability for wintertime, high latitudes, during periods of high cloud cover, and in locations where there are strong currents. These integrations will be critical to allow the USV network to maintain environmental stewardship whilst also meeting network targets to operate in these challenging operational environments.</p>
<p>As with any <italic>in situ</italic> surface ocean data collection, biofouling is one of the limiting factors for USV deployment durations - a universal issue also affecting other platforms such as surface buoys and drifters. While adding anti-fouling to the instruments, sensors and the hull is one obvious solution, these typically contain copper. This can affect inductive salinity measurements if too close to the sensor (<xref ref-type="bibr" rid="B67">Johnson and Fassbender, 2023</xref>), so care must be taken to ensure an adequate sensor placement distance from the antifouling during the instrument integration process. Other anti-fouling options such as wipers and UV lights are theoretically more practical on a USV than on, say, a surface buoy or drifter because of the USVs larger power payloads (<xref ref-type="bibr" rid="B106">Ryan et&#xa0;al., 2020</xref>). One significant advantage of USVs is that they are recovered after missions, so all their sensors can be post-calibrated, unlike some of the expendable observing platforms. Comparing USV data with other platforms such as moored surface data at varying degrees of biofouling also provides an opportunity for better understanding the impact of biofouling on sensor data in general, following examples comparing fouled with un-fouled wave buoys (<xref ref-type="bibr" rid="B128">Thomson et&#xa0;al., 2015</xref>). Depending on where the USV is operating (e.g. warm, tropical environments versus higher latitudes), biofouling can present significant limitations on the duration of the platform deployment. Major benefits of the USV technology is that the data can be monitored in real-time, underwater cameras, if available, can be placed to monitor biofouling, and USVs can self-retrieve, or be swapped out with a recently serviced USV when biofouling (or indeed power or calibration limitations) becomes an issue.</p>
</sec>
<sec id="s3_4">
<label>3.4</label>
<title>Attribute 4: Community of practice</title>
<p>A governance framework will set the network&#x2019;s community of practice to drive implementation, development and long-term sustainment. A core steering committee comprising three leadership committees will lead the network. Each leadership committee will be made up of stakeholders across what we consider are the three crucial aspects to delivering ocean data using USVs: science, data management, and public-private partnerships. This multidisciplinary stakeholder-led governance structure will ensure that the network&#x2019;s potential is fully realised and remains aligned with contemporary needs, including the recruitment and support of Early Career Ocean Professionals (ECOP) and ensuring the barriers to Justice, Inequality, Diversity, and Inclusion (JEDI) are broken (<xref ref-type="bibr" rid="B68">Johri et&#xa0;al., 2021</xref>). As such, open calls for participation, also following CARE principles (Collective benefit, Authority to control, Responsibility and Ethics; <xref ref-type="bibr" rid="B13">Carroll et&#xa0;al., 2020</xref>), will aid inclusive participation by individuals in under-represented regions and developing nations. A governance structure will be adopted that aligns with these principles and allows for equitable representation of the diverse stakeholders. If endorsed by GOOS OCG as an official emerging network, the USV network will benefit from OCG-facilitated discussions and opportunities aligned with these principles, and opportunity-sharing between the other OCG networks. USV network leadership committees will be required to provide transparency in decision-making and communications, and be required to declare conflicts of interest, especially when working with private companies. Guidance in implementing measures to maintain these standards will be drawn from other OCG networks.</p>
<p>To date, the network committee comprises the co-authors of this paper, and meets intermittently to share news, updates, ideas, and work on collaborative funding proposals. These meetings comprise a combination of recorded webinars (available at <ext-link ext-link-type="uri" xlink:href="https://airseaobs.org/resources/usv-for-goos-webinar">https://airseaobs.org/resources/usv-for-goos-webinar</ext-link>) and meetings to work on network activities and discuss funding opportunities to propel the network. A core committee will be formed within 12 months of this paper being published, and the steering committee will organise regular committee meetings to undertake tasks such as setting priorities for the network goals and activities, and developing funding pitches to work towards meeting the ten OCG attributes. Inter-sessional activities will be workshopped on relevant aspects of the network related to the ten attributes. The core steering committee will report annually to the GOOS OCG committee and provide input into GOOS OCG activities, and liaise with other relevant communities, such as OceanOPS (<ext-link ext-link-type="uri" xlink:href="https://www.ocean-ops.org/">https://www.ocean-ops.org/</ext-link>), the Ocean Best Practices System (OBPS; <ext-link ext-link-type="uri" xlink:href="https://www.oceanbestpractices.org/">https://www.oceanbestpractices.org/</ext-link>) and other OCG networks.</p>
</sec>
<sec id="s3_5">
<label>3.5</label>
<title>Attribute 5: Delivers data that are free, open, and available in a timely manner</title>
<p>Data distribution is a major challenge for the USV network due to nuances that are unique to the USV network, including the multiple and diverse platform types, manufacturers, and the multitude of USV data delivery mechanisms and options; USV data delivery needs to be considered differently from other networks. One aspect of data delivery stems from USVs&#x2019; unique capability to persistently relay Near Real-Time (NRT) data (e.g. roughly every 10 minutes) as well as very high-resolution Delayed Mode (DM) data (<xref ref-type="fig" rid="f4">
<bold>Figure&#xa0;4</bold>
</xref>). NRT data transmission configuration depends on the USV satellite communication subscription (e.g., bandwidth and data) which currently varies with USV make, model, and operators. Alongside this, the complexity of the Global Telecommunication System (GTS) and the transmission procedures for different data types (e.g., biological and ecological data) constrain data uploads to the GTS. It is possible for the USV network to borrow and adapt standards of existing networks to make it easier for USV end-users to make their data publicly available. For example, the Ships Observations Team (SOT) has recently formed a task team for Enhancement of Independent Class Observations (TT-EICO). This task team is designed to support the development and maintenance of new pilot projects to include gathering of data and metadata, and their quality control, from vessels where the information is not yet made available on the GTS (pers comm. Shawn Smith and Darin Figurskey). USV data handling and transmission will need to be considered independently of OceanGliders, drifters, and Argo platforms because of the large data storage payloads and their constant connection to satellites at the surface. For NRT transmission, the World Meteorological Organisation (WMO) GTS uses the BUFR (Binary Universal Form for the Representation of meteorological and oceanographic data) format and an existing template was developed to specifically support USV NRT data exchange. This template has been used over the last several years to exchange USV data on the GTS and is a strong starting point for implementation across the USV network. In this context, the GTS is currently evolving the WMO Information System (WIS; <ext-link ext-link-type="uri" xlink:href="https://community.wmo.int/en/activity-areas/wis">https://community.wmo.int/en/activity-areas/wis</ext-link>) so USV data infrastructure will be planned to meet the requirements of the WIS 2.0 as it replaces the GTS. The USV network is in an ideal position to lead the development of appropriate data and metadata formats, which will be made available online in the form of templates to the scientific community, USV manufacturers, and private USV users should they wish to make their data publicly available. The network will offer expertise and guidance to ensure data is disseminated according to the GOOS OCG attributes.</p>
<fig id="f4" position="float">
<label>Figure&#xa0;4</label>
<caption>
<p>A proposed data flow diagram for ensuring quality and timely delivery of data to the global community.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-12-1523585-g004.tif"/>
</fig>
<p>The USV network is committed to promoting FAIR, CARE and TRUST principles, defined here: FAIR principles (Findable, Accessible, Interoperable, Reusable; <xref ref-type="bibr" rid="B136">Wilkinson et&#xa0;al., 2016</xref>; <xref ref-type="bibr" rid="B125">Tanhua et&#xa0;al., 2019</xref>) list the characteristics that facilitate data exchange; the TRUST principles (Transparency, Responsibility, User focus, Sustainability and Technology; <xref ref-type="bibr" rid="B75">Lin et&#xa0;al., 2020</xref>) focus on defining the criteria for best practices in digital preservation by repositories, and the CARE principles are people and purpose oriented, ensuring that Indigenous innovations and self-determination are not ignored, thus decreasing the power differentials and historical contexts. Communicating these data-norms and expectations is an important aspect of developing the community of practice. These principles will be communicated to the public and network as part of the USV community of practice (on a USV network website, which is currently being developed) so that data contributors are aware of the principles under which the network and associated data distribution operates.</p>
<p>The USV network will develop data processing strategies and best practices by harnessing community-agreed protocols and taking advantage of existing efforts and data distribution models from other GOOS networks and data delivery quality standards. As USVs are new technology, the network has a collective responsibility to ensure that appropriate quality controls on data processing and delivery are met. While these processes are not yet fully formed, we will draw from the learnings of other OCG networks introducing new technologies. For example, open source code will be encouraged in a similar fashion to that of the OceanGlider community (<ext-link ext-link-type="uri" xlink:href="https://github.com/OceanGlidersCommunity">https://github.com/OceanGlidersCommunity</ext-link>) to promote open source code development at the community level. This coordinated approach will ensure methodologies and standard operating procedures will be developed amongst the USV community to avoid duplicitous efforts, siloed practices, and provide products that will benefit scientists and USV manufacturers alike. Key QARTOD (Quality Assurance/Quality Control of Real-Time Oceanographic Data) principles, such as quality descriptors and detailed quality flags will be developed following industry-standard codes and manuals (<xref ref-type="bibr" rid="B11">Bushnell, 2017</xref>; <ext-link ext-link-type="uri" xlink:href="https://github.com/ioos/ioos_qc">https://github.com/ioos/ioos_qc</ext-link>). A centralised system to curate and distribute data for stakeholders is essential for managing and disseminating data. For example, CUBEnet (<ext-link ext-link-type="uri" xlink:href="http://oceancube.usm.edu/">http://oceancube.usm.edu/</ext-link>) has been able to streamline data access for stakeholders and enhance the utility of oceanographic data and address science-based questions in the Gulf of Mexico. By integrating these best practices and leveraging the experiences from the established systems and best practices discussed above, the USV network will develop a cohesive and efficient data management solution for the USV user community.</p>
</sec>
<sec id="s3_6">
<label>3.6</label>
<title>Attribute 6: Maintains network mission and targets</title>
<p>Each OCG network has a role in GOOS, and its progress towards its specific mission and targets must be tracked. The USV network defines its unique contribution to GOOS as its ability to observe multiple EOVs and ECVs at fine spatio-temporal scales, whilst monitoring broadly at scales of up to tens of thousands of kilometres from seconds to months. The USV network targets remote and difficult to access locational and disciplinary environments.</p>
<p>Recognising that air-sea fluxes are concentrated near fronts, <xref ref-type="bibr" rid="B28">Cronin et&#xa0;al. (2019)</xref> proposed that a global network of approximately 1000 platforms deployed as pairs or clusters within 10&#xb0; by 10&#xb0; boxes may be a reasonable target (368 boxes would cover the global ocean), playing a similar role to the Argo network target of one float profile per 3&#xb0; by 3&#xb0; box every 10 days (<xref ref-type="bibr" rid="B105">Roemmich et&#xa0;al., 2019</xref>) or the drifter network target of one drifter per 5&#xb0; by 5&#xb0; box (<xref ref-type="bibr" rid="B14">Centurioni, 2018</xref>). Alternatively, the USV network may want a target of having repeat transects that can capture the annual mean air-sea fluxes, enabling national and international stocktakes, such as called for by the 2015 Paris Accord (<xref ref-type="bibr" rid="B133">Wanninkhof et&#xa0;al., 2019</xref>). Such repeat transects could be referred to as GO-USV transects, as their targets are similar to those of the GO-SHIP network, albeit with a focus on air-sea interaction at more rapid timescales than the GO-SHIP focus on full water column variability over decadal timescales. If these transects were made as a USV cluster, the transect could act like a &#x2018;mobile meso-net&#x2019;, capturing the multi-scale variability of convective systems that drive much of the air-sea interactions. An example of this type of sampling is being tested in TPOS, where near-annual missions with 2-4 USVs sampling cold pools and convective mesoscale systems as USVs transect through the Inter-tropical convergence zone, and then sample submesoscale SST fronts as they travel into or out of the cold tongue of surface water on the equator (<xref ref-type="bibr" rid="B30">Cronin et&#xa0;al., 2024</xref>, <xref ref-type="bibr" rid="B29">2023</xref>; <xref ref-type="bibr" rid="B138">Wills et&#xa0;al., 2023</xref>). Once demonstrated, the &#x2018;mobile cluster&#x2019; or &#x2018;force-multiplier&#x2019; approach to ocean data collection could be transformative to climate and weather science.</p>
<p>At minimum, the USV targets should track the attributes discussed in this section, including metrics related to coverage, number of EOVs and ECVs, applications addressed, and data sets. Defining targets and gaps for future goals requires active community discussion and in some part is likely to be regionally dependent, and progress over time.</p>
</sec>
<sec id="s3_7">
<label>3.7</label>
<title>Attribute 7: Ensures metadata quality and delivery</title>
<p>Delivery of quality NRT or DM metadata is an essential aspect of a coordinated, global USV network. To date, the existing USV community has been independently managing data and metadata associated with individual projects; some data being stored privately, and other data being made freely available in online catalogues, such as the National Centers for Environmental Information (NCEI; <ext-link ext-link-type="uri" xlink:href="https://www.ncei.noaa.gov/">https://www.ncei.noaa.gov/</ext-link>), Zenodo (<ext-link ext-link-type="uri" xlink:href="https://zenodo.org/">https://zenodo.org/</ext-link>), European Marine Observation and Data Network (EMODnet; <ext-link ext-link-type="uri" xlink:href="https://emodnet.ec.europa.eu/en">https://emodnet.ec.europa.eu/en</ext-link>), and USV manufacturers websites (<ext-link ext-link-type="uri" xlink:href="https://www.saildrone.com/technology/data-sets">https://www.saildrone.com/technology/data-sets</ext-link>).</p>
<p>The USV community recognises two key opportunities for delivering quality data and metadata in a frictionless way to global end users as outlined by the GOOS OCG (<ext-link ext-link-type="uri" xlink:href="https://goosocean.org/who-we-are/observations-coordination-group/data-management/">https://goosocean.org/who-we-are/observations-coordination-group/data-management/</ext-link>). These opportunities are to develop: (1) A central repository for global USV data that follows FAIR, TRUST, and CARE principles, and can be accessed from anywhere in the world (discussed further in Section 7); and (2) Standardisation of USV data and metadata, including various formats for NRT and DM, and for data storage and distribution, discussed below.</p>
<p>A major requirement for metadata quality and delivery is the development and adherence to standards. While there are currently no formal standards for USV metadata collection, the National Oceanic and Atmospheric Administration (NOAA) is working towards developing a data and metadata template for USVs (<ext-link ext-link-type="uri" xlink:href="https://www.ncei.noaa.gov/products/uncrewed-system-metadata-templates">https://www.ncei.noaa.gov/products/uncrewed-system-metadata-templates</ext-link>) that, alongside parallel efforts in other nations and agencies, and across different manufacturers, could be harmonised to form standard templates for the network. The USV network will play a major role in establishing open communication lines between industry and scientists to help with the co-development of proposed standards. While reviewing literature for this paper, we found that USV data streams regularly omit important metadata, such as the distance from a sensor to the water level. Changes in the location of the sensor in relation to the water line or USV centre of gravity can alter the way the data should be interpreted. There are opportunities for the network to focus on standard metadata content and data formats for use across the community.</p>
</sec>
<sec id="s3_8">
<label>3.8</label>
<title>Attribute 8: Develops and follows standards and best practices</title>
<p>Best practices extend from standardising metadata collection (discussed in Attribute 7) to data collection methodologies from an ecosystem of USV archetypes, and approaches to industry data collection. Adopting standards across a USV network that encompasses industry- and science-operated vehicles and sensors is particularly important for building trust with future scientific and industry end users, including GOOS regional alliances, OCG networks, and industry (<xref ref-type="bibr" rid="B95">Parks et&#xa0;al., 2024</xref>). A significant aspect that is continually identified within the scientific USV end-user community has been the lack of certainty around data collected from a non-spherical, propelled platform. An important, and typically overlooked practice is to perform intercomparison studies to describe and account for uncertainties in the powered motion of the USV and the hydrodynamic responses of the hull, which differ compared to a moored spherical buoy, and may be specific to certain variables. This is particularly important for the measurement of wave spectra, which is an under-sampled ocean variable but a key variable for calculating air-sea fluxes (<xref ref-type="bibr" rid="B126">Thomson and Girton, 2017</xref>; <xref ref-type="bibr" rid="B1">Amador et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B24">Colosi et&#xa0;al., 2023</xref>).</p>
<p>Intercomparisons between USVs and established monitoring platforms of known precision and uncertainty, under a range of different conditions are a fundamental process for the trusted adoption of USVs by the scientific community. However, there are challenges associated with these intercomparisons, especially in remote locations, extreme conditions, and/or regions of high natural variability (<xref ref-type="bibr" rid="B107">Sabine et&#xa0;al., 2020</xref>; <xref ref-type="bibr" rid="B144">Zhang et&#xa0;al., 2019a</xref>). Moored buoys are likely the most useful for this purpose, as they remain in fixed locations and provide standard near-surface ocean and atmospheric measurements.</p>
<p>The USV community would benefit from a standardised USV intercomparisons methodology, and a common database of data intercomparisons across a wide range of ocean-atmosphere conditions and USV platform archetypes to determine strengths and weaknesses of different USV platforms and gain confidence in the use of the data for scientific analysis and data assimilation. The USV network will, in collaboration with manufacturers, develop standards for data processing and data quality control (QC) of the platforms and instruments, with the aim of ensuring that data published according to these guidance and standards are of the highest quality and can be used for multiple applications. An assessment of existing standards and recommended practices will be done and where applicable expanded. In order to ensure knowledge sharing and community uptake, the outcomes of this work will be published in OBPS (<ext-link ext-link-type="uri" xlink:href="https://www.oceanbestpractices.org/">https://www.oceanbestpractices.org/</ext-link>) and maintained by the network. Developing standards and best practices will be an opportunity to work with USV manufacturers to ensure that the scientific needs of USVs for certain applications and environments are made available.</p>
</sec>
<sec id="s3_9">
<label>3.9</label>
<title>Attribute 9: Undertakes capacity development and technology transfer</title>
<p>An important aspect of the USV network is its relative advantage in reaching remote and under-sampled locations, which aligns with the GOOS mission to promote feasible, high-impact observing programs. These regions often lack the resources to deploy traditional observatories, and USVs present a compelling option for extending coverage to the archipelagos of southeast Asia, central America, and the tropical Pacific and Indian Oceans. The existing data (<xref ref-type="fig" rid="f3">
<bold>Figure&#xa0;3</bold>
</xref>) show notable coverage in very remote locations, including prolific adoption in the tropical Pacific, and we can see that isolated USV deployments occur in other remote and under-sampled locations, such as Australia&#x2019;s northern regions (the Timor and Arafura Seas), central America&#x2019;s archipelagos, northern parts of South America, and the western African coastline, associated with voyages out of the Canary Islands. Notably, no USV tracks are available in the Indian Ocean, which may present an opportunity to extend multidisciplinary and interdisciplinary co-located observations for the Indian Ocean Observing System (IndOOS), as strongly noted in the 2019 IndOOS roadmap (<xref ref-type="bibr" rid="B6">Beal et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B56">Hermes et&#xa0;al., 2019</xref>; <xref ref-type="bibr" rid="B7">Beal et&#xa0;al., 2020</xref>).</p>
<p>There are substantial opportunities for USV capacity development via comprehensive training and capacity-building programs aimed at developing the technical skills in oceanographic data collection and management (<xref ref-type="bibr" rid="B77">McKenna et&#xa0;al., 2023</xref>). These programs are designed to cover various aspects of USV operation, data acquisition, data processing, and interpretation using advanced analytical tools to better position a changing workforce as well as specifically target a young audience in pursuit of ocean science education and employment. USV technological adoption empowers maritime professionals in enhancing operational capabilities and data handling proficiency as well as provides an on-ramp for educational, and vocational programs.</p>
</sec>
<sec id="s3_10">
<label>3.10</label>
<title>Attribute 10: Observations are sustained</title>
<p>A sustained USV network will potentially be one of the greatest challenges, and a key component to sustainment will be a steady finance stream. Historically and in the near future, the existing missions have and will be individually funded through 2-5 year research grants. However, there is often synergy between intensive process studies (discussed in Attribute 1) and long-term monitoring that can provide seasonal-to-interannual cost recovery, which could help support a sustained USV network. Another strategy to obtain sustained observations might be to take advantage of transits from future USV service stations, particularly ones located in the global south. Ultimately through economies of scale, we can expect that a threshold will be reached where it is more economical to plan as a sustained observing network rather than as one-off missions. For example, USVs could be recovered and redeployed by refurbishing the platform and integrating fresh sensors, similar to how moorings are turned around in sustained long-term mooring networks.</p>
<p>In the context of meeting this attribute, the network is more likely to be sustained if the other attributes are met: data management, a community of practice, data and metadata standards and best practices, governance structure and the setting and delivery of network targets and metrics will all drive and ensure a sustained and burgeoning network.</p>
</sec>
</sec>
<sec id="s4">
<label>4</label>
<title>USVs&#x2019; complementary role in GOOS</title>
<p>As a network focused on air-sea interactions, the USV network will provide a critical and currently unmet capability within GOOS, complementing existing networks by providing high-resolution surface ocean and lower atmosphere observations over broad regions (<xref ref-type="fig" rid="f5">
<bold>Figure&#xa0;5</bold>
</xref>). Essentially, scientific USVs play a major role in measuring air-sea interactions during extreme conditions and capturing submesoscale processes dynamically, contributing multiple variables to valuable process-scale information for enhancing weather and climate research at previously unmet spatial and temporal scales.</p>
<fig id="f5" position="float">
<label>Figure&#xa0;5</label>
<caption>
<p>Uncrewed Surface Vehicles&#x2019; complementary role in the GOOS networks, covering small-scale processes for up to 12 months and spanning oceans, adapted from <ext-link ext-link-type="uri" xlink:href="https://goosocean.org/document/17466">https://goosocean.org/document/17466</ext-link>. Asterisked networks represent those which sample the interior ocean.</p>
</caption>
<graphic mimetype="image" mime-subtype="tiff" xlink:href="fmars-12-1523585-g005.tif"/>
</fig>
<p>USVs have already provided complementary coverage and enhanced both the extent and variety of data collected as an integrated capability within existing GOOS OCG networks. For example, USVs have been paired with OceanGlider deployments, providing simultaneous surface ocean and lower atmospheric observations, adding critical surface observations to the collection of interior ocean observations (<xref ref-type="bibr" rid="B90">Nicholson et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B69">Kosaka et&#xa0;al., 2023</xref>; <xref ref-type="bibr" rid="B145">Zhang et&#xa0;al., 2023a</xref>). In some instances, USVs have been especially augmented to function as motherships for transport and release of OceanGliders (<xref ref-type="bibr" rid="B113">Siddle et&#xa0;al., 2021</xref>). Like the OceanGlider network, USVs can complement OceanSITES network time series by providing spatial gradient information needed for evaluating advective processes, and in this way enable closure of budget analyses governing variability at the time series stations (e.g. <xref ref-type="bibr" rid="B41">Fassbender et&#xa0;al., 2017</xref>). USVs have been deployed as GO-USV repeat transects that could complement the GO-SHIP transects, as discussed in Attribute 6. USV-observed CO<sub>2</sub> fluxes will undoubtedly be an important component of the emerging SOCONET, supporting SOCONET&#x2019;s mission to provide global ocean CO<sub>2</sub> uptake information for annual national assessments and 5-year global stocktakes (<xref ref-type="bibr" rid="B133">Wanninkhof et&#xa0;al., 2019</xref>). Any network, such as SOCONET, that is defined by an EOV, will be reliant upon platform networks like the USV network, to make these measurements. A USV network will invariably make overlapping measurements with other platform networks, however these will likely have different spatial and temporal scales and provide an opportunity for understanding differences in data outputs between different platforms.</p>
<p>USVs offer a valuable complementary service to enhance satellite observations due to their high temporal resolution. For example, most wind-measuring satellites use sun synchronous orbits, meaning that they obtain measurements at best every 12 hours, along a swath with a width typically between 500 and 1500 km, depending on satellite specifications. USVs can provide valuable high-resolution data of satellite-inferred variables such as wind speed and direction, sea surface temperature, and salinity measurements. Satellites interpreted in concert with USV measurements offer a means to evaluate variability over spatio-temporal scales that would be inaccessible from satellites or USVs alone. USV data are already being used for satellite data validation (<xref ref-type="bibr" rid="B103">Ricciardulli et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B141">Yu et&#xa0;al., 2023</xref>). As the USV network grows and the data are more widely trusted and available in appropriate formats, we expect that USV data will be used more extensively to support satellite validation and calibration, consistent with the current usage of surface drifting and moored buoy data. Through webinars and workshops, OASIS sustains communication within the satellite air-sea flux community and supports links with the USV network. Continued interactions between the satellite and USV communities are necessary and will benefit both groups. For example, wind observations from a NOAA-Saildrone USV are being used to validate Synthetic Aperture Radar (SAR) winds in Atlantic hurricanes, while SAR data also provide a consistency check for USVs. Future satellite concepts offer the possibility of obtaining targeted measurements of air-sea fluxes. For example, air-sea turbulent heat fluxes could be inferred using bulk parameterisations by measuring near surface temperature and humidity as well as wind speed and sea surface temperature (<xref ref-type="bibr" rid="B45">Gentemann et&#xa0;al., 2020b</xref>). Air-sea momentum exchange could be inferred using a Doppler scatterometer to measure winds and surface currents simultaneously (<xref ref-type="bibr" rid="B104">Rodr&#xed;guez et&#xa0;al., 2019</xref>), as has been done from aircraft during S-MODE (<xref ref-type="bibr" rid="B40">Farrar et&#xa0;al., 2020</xref>). All of these concepts will rely on <italic>in-situ</italic> surface measurements (e.g. from USVs) to support calibration and validation.</p>
<p>Building on their proven capabilities, the USV network has the potential to drive further complementary services and facilitate unrealised integrations within other GOOS OCG networks. As numerical weather prediction models begin to incorporate true coupled ocean-atmosphere assimilation schemes, USV and other platforms that measure coincident ocean and atmosphere variables will become ever more critical (<xref ref-type="bibr" rid="B99">Penny et&#xa0;al., 2019</xref>). Opportunistic data collection for non-scientific USV missions has the potential to become a realised component of the Volunteer Observing Ships (VOS) and Ships of Opportunity Programme (SOOP), and would require these volunteers to use the network data and metadata standards, and agree to the data principles outlined in Attribute 5.</p>
<p>GOOS regional alliances have also recognised the value and growing USV adoption. The GROOM II project focuses on fostering USV operations, providing 11 European countries and 20 member organisations with information and community resources in operationalising USVs. The USV network will work collaboratively with these and other existing regional networks to foster and build the global USV network. Other under-sampled regional alliances, such as the Southern Ocean, stand to benefit significantly from the USV network, which may be supported under the regional, community-driven Southern Ocean Observing System (SOOS), to address the environmental constraints of ocean observing in such a difficult environment.</p>
</sec>
<sec id="s5">
<label>5</label>
<title>Proposed USV network terms of reference</title>
<p>This paper is a first step in gathering a community of interested individuals which can help set the foundations for a coordinated and collaborative global network. The following terms of reference, which may be adapted after establishing the steering committee, are proposed.</p>
<list list-type="bullet">
<list-item>
<p>Develop and implement a global network for air-sea interaction observations through focusing on sampling the following core EOVs/ECVs: air temperature, air pressure, humidity, skin temperature, sea surface temperature and salinity, current profiles, wind speed and direction, radiation (long-wave/short-wave), atmospheric pressure, seawater and air pCO<sub>2</sub>, dissolved oxygen, and chlorophyll. Focus on stand-alone USV missions in the network, and the integration of USVs within other OCG networks such as GO-USVs, USV VOS/SOOP, USV-OceanGlider pairings, and USVs in SOCONET.</p>
</list-item>
<list-item>
<p>Develop an implementation plan for the coordinated collection of biological and ecological data using USVs.</p>
</list-item>
<list-item>
<p>Coordinate delivery of NRT data to the GTS and quality-controlled data to a network of global data centres.</p>
</list-item>
<list-item>
<p>Develop and systematically review data collection best practices, working with the OBPS and tools to reduce duplication of effort by learning from other networks.</p>
</list-item>
<list-item>
<p>Work with the wider scientific community to develop standardised methods for performing intercomparisons and calculating derived variables, such as surface wave height spectra.</p>
</list-item>
<list-item>
<p>Coordinate and exchange information with GOOS OCG on scientific and technical issues and to optimise the overall capability of GOOS.</p>
</list-item>
<list-item>
<p>Collaborate with the USV manufacturing industry in a two-way dialogue to develop appropriate practices for sampling and data QC.</p>
</list-item>
<list-item>
<p>Ensure FAIR, TRUST, CARE data practices, and JEDI principles across network governance structure.</p>
</list-item>
<list-item>
<p>Promote coordination and partnerships with other ocean observing networks.</p>
</list-item>
</list>
</sec>
<sec id="s6">
<label>6</label>
<title>Network challenges and practicalities</title>
<p>The wide range of unique USV platforms offers both advantages and challenges for global coverage and providing reliable and quality data. Diverse USV platform types will build resilience in sustaining GOOS observations, as was demonstrated by autonomous platforms during the COVID pandemic (<xref ref-type="bibr" rid="B10">Boyer et&#xa0;al., 2023</xref>), however the non-uniform platform shapes, sizes, and movement characteristics introduce complexity and challenges for developing standards and best practices.</p>
<p>Diversity in USV size and shape format will help improve the challenges that arise from the reliance on solar power alone for power generation (discussed in Attribute 3). This reliance is a recognised challenge across manufacturers and end-users. Technology accelerators and philanthropic organisations promoting sustainable marine technology solutions are funding opportunities for novel power generation alternatives to solar, such as wave- and hydro- generators or repackaged wind generators which would be considered for polar-adapted USVs. Although these solutions are in development, there is promising collective global momentum towards problem-solving. In the meantime, USV operators will require the tools, training and experience to work within the limitations of the technology and the environment. Given USVs are highly mobile and manoeuvrable, USV schedules (much like ship schedules) can be coordinated to ensure that operational failures due to low energy do not occur.</p>
<p>Widespread adoption of USVs for ocean science will be shaped by several practical considerations. Public-private partnerships will play a crucial role in this landscape, and the USV network will facilitate collaboration between scientific institutions and USV manufacturers. These partnerships can bridge gaps between scientific needs and commercial capabilities, potentially through dedicated science-business liaisons who understand both USV platforms and scientific methodologies. However, the diversity in USV platforms and the business models of their manufacturers presents challenges, with primary business models, owner-operator, product-as-a-service, and leases, each presenting unique challenges and benefits, influencing operational decision-making, data flow, and cost structures.</p>
<p>Regulatory compliance remains a complex issue due to the absence of standardised international regulations for USVs, which tend to come under the banner of &#x2018;uncrewed maritime vehicles&#x2019;, and include underwater uncrewed vehicles. The 1982 United Nations Convention on the Law of the Sea (<xref ref-type="bibr" rid="B130">UNCLOS</xref>) did not anticipate modern uncrewed technologies and this has led to a fragmented regulatory landscape. The classification of USVs as &#x2018;ships&#x2019; or &#x2018;not-ships&#x2019; significantly impacts their operational freedoms and restrictions. On the high seas, USVs classified as &#x2018;ships&#x2019; enjoy the freedom of navigation as would any other ship. The definition of a USV as a &#x2018;ship&#x2019; or &#x2018;non-ship&#x2019; is governed by each individual nation (<xref ref-type="bibr" rid="B130">UNCLOS</xref>, Art. 91); there is currently no unified global approach for legal status of uncrewed vehicles.</p>
<p>In the context of sustained, long-term marine scientific research at a global scale (i.e. a focus of the GOOS), UNCLOS provides Part XIII Marine Scientific Research (MSR). Part XIII establishes rules to grant consent for MSR to be undertaken and to promote altruistic values such as: the obligations of international states and organisations to promote cooperation; favourable conditions for integrating the efforts of scientists conducting MSR; and data and knowledge needing to be shared and disseminated for the collective good of mankind. However, for the existing GOOS networks, which includes autonomous platforms such as OceanGliders and Argo floats, there are notable concerns and challenges about the practicalities of coordinating the observation networks and attaining MSR clearances, such as in disputed territorial waters, and within practical timelines for planning voyages and deployments (<xref ref-type="bibr" rid="B50">GOOS, 2021</xref>). Sovereign security is a major area of concern for coastal states and can substantially delay or prevent MSR clearances. A global USV network endorsed by GOOS will operate under UNCLOS Part XIII, like other GOOS networks (<xref ref-type="bibr" rid="B50">GOOS, 2021</xref>). While UNCLOS convention allows &#x2018;the right of innocent passage&#x2019; through areas of national jurisdiction (<xref ref-type="bibr" rid="B130">UNCLOS</xref>, Art. 17), in reality the presence of an uncrewed system in foreign waters typically results in disputes (<xref ref-type="bibr" rid="B16">Chang et&#xa0;al., 2024</xref>), since many USVs are associated (or suspected to be) with military operations due to their dual use capabilities. Ultimately, the navigation of USVs undertaking MSR in areas of national jurisdiction falls under the jurisdiction of the coastal state, and USV users must obtain prior approval to operate within the jurisdiction of the coastal state (<xref ref-type="bibr" rid="B130">UNCLOS</xref>). This means that globally-roaming scientific USVs operating inside EEZs will be best operated in partnership with local collaborators who can navigate local governance structures and appeal to sovereign legal maritime authorities.</p>
</sec>
<sec id="s7">
<label>7</label>
<title>Towards an open USV community; immediate needs and conclusion</title>
<p>Growing observing capability using USVs, through new sensor integrations, prolonged endurance, improved manoeuvrability, unprecedented co-variable data collection capability, developing appropriate standards, and fine-scale and real-time data delivery will endure as a result of a coordinated and inclusive community. New developments in profiling capability such as towed and winched instruments, and the emergence of instruments designed specifically for USVs, is already resulting in enhanced environmental measurements. These include rapidly evolving structures connected to the physical and biogeochemical air-sea fluxes such as fronts, mixing, biomass patchiness, and lower marine boundary layer from winds bursts to weather. USVs are also beginning to make direct eddy covariance flux measurements (<xref ref-type="bibr" rid="B102">Reeves Eyre et&#xa0;al., 2023</xref>), which will result in better constraints of bulk formula methods and greatly expand direct observations spatially and temporally. Perhaps the most promising and regularly promoted aspect of USVs that have yet to be implemented at scale in science is the concept of force multipliers to measure a &#x2018;pseudo-synoptic&#x2019; view of rapidly developing phenomena (<xref ref-type="bibr" rid="B91">Nickford et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B90">Nicholson et&#xa0;al., 2022</xref>; <xref ref-type="bibr" rid="B129">Toolsee et&#xa0;al., 2024</xref>), such as ocean fronts, tropical cyclones, marine heatwaves, or phytoplankton blooms. In other words, a few USVs working together can provide unprecedented 3-D or even 4-D perspectives of the ocean or atmosphere during an experiment.</p>
<p>New data science techniques are allowing us to integrate USV observations with various types of model simulations, such as weather forecast operational models, to high-resolution coupled model simulations, in order to understand and upscale the impact that fine-scale processes have on our weather, climate, and ecosystems (<xref ref-type="bibr" rid="B120">Swart et&#xa0;al., 2023</xref>). In general, there are several ways USV data can be applied to numerical modelling. First, USV data provide a ground truth to validate numerical products (reanalysis, simulations, and forecasts). Second, knowledge gained from USV data would help improve numerical model parameterisations (e.g., improved drag coefficient parameterisation under hurricane wind conditions). Third, when USV data are available to operational forecast centres in real time via GTS, their data assimilation systems can inject USV data into their forecast initialisation procedures. To enable this capability, the USV network and its nascent community has an important role to play in the development of agreed standards and best practices, guided and facilitated by OBPS, and digital infrastructure to globally disseminate USV data according to FAIR, CARE, and TRUST principles, and promote JEDI principles across the governance structure. Meeting these needs will facilitate data integration into ocean models and broader adoption by the research community and other users. This community-driven approach that supports scientists and manufacturers in sharing experiences, challenges, and solutions is much-needed across the USV end-user community. Every individual that was approached to join the network in writing this manuscript willingly provided data (published and unpublished) and intellectual contributions, demonstrating the collective drive and need for the network globally. These cohesive and altruistic characteristics of the network community aligns well with the prescribed UNESCO-oriented OCG attributes.</p>
<p>In the short-term, some administrative USV network costs have been provided in-kind by OASIS as an affiliated UN Decade of Ocean Science project. The network is actively pursuing government grants to support operational activities such as website development, data management services and administrative support. A formal endorsement as an emerging GOOS OCG network will increase network visibility and facilitate participation in international collaborations, research programs and regional alliances that pool resources and funding for ocean observing programs involving USVs. The network is pursuing international collaborative research grants to work on key and immediate needs, such as much-needed intercomparisons and the development of standards and best practices guidelines. These efforts are coordinated amongst the network participants, and updates are provided and knowledge shared in regular network meetings. In the medium to long term the network will require more sustained funding streams. Given the novelty of this technology, the USV network will pursue engagement with non-profit organisations, technology organisations (such as the Marine Technology Society) and pursue philanthropic funding. This may require the network to adapt to an organisational structure that is formally &#x2018;not for profit&#x2019;, which may also open doors to other end-users. The USV network has the potential to promote the value of data, technology and the private sector in ocean observing with shared interests in both the altruistic and commercial benefits of a global USV network.</p>
</sec>
</body>
<back>
<sec id="s8" sec-type="author-contributions">
<title>Author contributions</title>
<p>RP: Conceptualization, Data curation, Formal analysis, Funding acquisition, Investigation, Methodology, Project administration, Resources, Software, Supervision, Validation, Visualization, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. JoB: Conceptualization, Investigation, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. MC: Conceptualization, Data curation, Funding acquisition, Investigation, Methodology, Project administration, Resources, Supervision, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. JE: Data curation, Visualization, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. JM: Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. JP: Conceptualization, Data curation, Investigation, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. AP: Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. SS: Conceptualization, Funding acquisition, Investigation, Project administration, Resources, Supervision, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. CA: Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. WB: Data curation, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. PB: Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. JuB: Writing &#x2013; review &amp; editing, Writing &#x2013; original draft. EB: Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. JaB: Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. LC: Data curation, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. BD: Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. MD: Data curation, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. MF: Data curation, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. GF: Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. SG: Investigation, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. LG: Data curation, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. JH: Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. LH: Data curation, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. MH: Data curation, Writing &#x2013; review &amp; editing. VH: Writing &#x2013; review &amp; editing. CKo: Writing &#x2013; review &amp; editing. NK: Data curation, Writing &#x2013; review &amp; editing. CKu: Data curation, Investigation, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. LLe: Data curation, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. LLo: Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. AM: Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. EM: Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. CRM: Conceptualization, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. SM: Data curation, Writing &#x2013; review &amp; editing. CM: Data curation, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. AN: Data curation, Writing &#x2013; review &amp; editing. SAN: Data curation, Writing &#x2013; review &amp; editing. S-AN: Data curation, Writing &#x2013; review &amp; editing. KO: Investigation, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. DP: Data curation, Writing &#x2013; review &amp; editing. LP: Data curation, Writing &#x2013; review &amp; editing. VR: Data curation, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. NR: Data curation, Writing &#x2013; review &amp; editing. ES: Data curation, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. CS: Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. AS: Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. NT: Data curation, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. JT: Writing &#x2013; original draft, Writing &#x2013; review &amp; editing, Data curation. IU: Data curation, Writing &#x2013; original draft, Writing &#x2013; review &amp; editing. LY: Writing &#x2013; review &amp; editing, Writing &#x2013; original draft. CZ: Data curation, Writing &#x2013; review &amp; editing. DZ: Data curation, Writing &#x2013; review &amp; editing.</p>
</sec>
<sec id="s9" sec-type="funding-information">
<title>Funding</title>
<p>The author(s) declare financial support was received for the research, authorship, and/or publication of this article. This work occurred as an activity of the Observing Air-Sea Interactions Strategy (OASIS). We acknowledge funding provided by Elysium EPL and national committees of the Scientific Committee on Oceanic Research (SCOR) and from a grant to SCOR from the U.S. National Science Foundation (OCE-2140395) to support SCOR Working Group #162 (OASIS) activities. Working Group #162 (OASIS) activities. Elysium EPL were not involved in study design, data collection and analysis, decision to publish or preparation of the manuscript. SG acknowledges support from NASA (80NSSC24M0010). SS and MD have received funding from the European Union&#x2019;s Horizon Europe ERC Synergy Grant programme under grant agreement No. 101118693 (WHIRLS). S-AN, SS, and MD have received funding from the European Union&#x2019;s Horizon 2020 Research and Innovation Program under grant agreement No. 821001 (SO-CHIC). S-AN acknowledges support from the Department of Science and Innovation (DSI/CON C3184/2023) and from NRF SA National Antarctic Programme (SANAP230503101416). ES acknowledges support from the Natural Environment Research Council and the ARIES Doctoral Training Partnership [grant number NE/S007334/1].</p>
</sec>
<ack>
<title>Acknowledgments</title>
<p>We thank all those providing USV metadata in order to provide the global USV coverage maps and information. We thank Matt Donnelly for providing critical feedback on the manuscript. SG acknowledges support from NASA (80NSSC24M0010). This is PMEL publication #5684.</p>
</ack>
<sec id="s10" sec-type="COI-statement">
<title>Conflict of interest</title>
<p>Author RP was employed by the company Elysium EPL. Author AP was employed by company Astraeus Ocean Systems. Authors LC and VR were employed by Akvaplan-niva. Author MF was employed by the company Seasats. Author DP was employed by company Offshore Sensing. Author NR was employed by the company Ocius Technology LTD. Author ES has a NERC CASE PhD studentship which receives financial support from AutoNaut Ltd.</p>
<p>The remaining authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.</p>
</sec>
<sec id="s11" sec-type="ai-statement">
<title>Generative AI statement</title>
<p>The author(s) declare that no Generative AI was used in the creation of this manuscript.</p>
</sec>
<sec id="s12" sec-type="disclaimer">
<title>Publisher&#x2019;s note</title>
<p>All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.</p>
</sec>
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