Front. Mar. Sci. Frontiers in Marine Science Front. Mar. Sci. 2296-7745 Frontiers Media S.A. 10.3389/fmars.2024.1522621 Marine Science Correction Corrigendum: Modelling the bottom-up effects of climate change on primary production in the Gulf of St. Lawrence and eastern Scotian Shelf Mei Zhi-Ping 1 Lavoie Diane 2 * Lambert Nicolas 3 4 Starr Michel 2 Chassé Joël 3 Perrie William 1 Long Zhenxia 1 1 Bedford Institute of Oceanography, Fisheries and Oceans Canada, Dartmouth, NS, Canada 2 Maurice-Lamontagne Institute, Fisheries and Oceans Canada, Mont-Joli, QC, Canada 3 Gulf Fisheries Centre, Fisheries and Oceans Canada, Moncton, NB, Canada 4 Canadian Centre for Climate Modelling and Analysis, Environment and Climate Change Canada, Victoria, BC, Canada

Edited and Reviewed by: Shin-ichi Ito, The University of Tokyo, Japan

*Correspondence: Diane Lavoie, Diane.Lavoie@dfo-mpo.gc.ca

23 12 2024 2024 11 1522621 04 11 2024 21 11 2024 Copyright © 2024 His Majesty the King in Right of Canada as represented by Fisheries and Oceans Canada 2024 His Majesty the King in Right of Canada as represented by Fisheries and Oceans Canada

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 A Corrigendum on Modelling the bottom-up effects of climate change on primary production in the Gulf of St. Lawrence and eastern Scotian Shelf By Mei Z-P, Lavoie D, Lambert N, Starr M, Chassé J, Perrie W and Long Z (2024) Front. Mar. Sci. 11:1416744. doi: 10.3389/fmars.2024.1416744 climate change Gulf of St. Lawrence Eastern Scotian Shelf primary production nutrient supply estuarine circulation river runoff Fisheries and Oceans Canada10.13039/501100000041 section-in-acceptance Global Change and the Future Ocean

In the published article, there was an error in panels K-N in Figure 2 as published. The panels are supposed to display the mean temperature and salinity of the upper 50 m water column in historical years (2001-2020) and the change from historical to future years (2071-2090). However, the authors inadvertently used a line of code that calculates the mean of a single layer. This error occurred in the final stage of the manuscript preparation for publication. The corrected Figure 2 and its caption appear below.

Mean annual atmospheric forcing over the 2001-2020 period (the ‘Historical’ period), and the difference between the mean of the 2071-2090 period (Future) and the mean of the 2001-2020 period (Fut. - Hist.) for precipitation (A, B), air temperature at 10 m above sea surface (C, D), surface shortwave radiation (E, F), wind speed (G, H) and sea-ice concentration between January and April (I, J), and similarly, mean 0-50 m water temperature (K, L), mean 0-50 m salinity (M, N), and stratification of the water column in the upper 50 m (O, P). Dots in the figures indicate the cells where future changes are significant from the historical period. The stratification, salinity, and water temperature are not calculated for areas shallower than 50 m, shown as blank.

The authors apologize for this error and state that this does not change the scientific conclusions of the article in any way. The original article has been updated.

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