Oceanographic processes driving low-oxygen conditions inside Patagonian fjords

Oceanographic processes driving low-oxygen conditions inside Patagonian fjords

<p>The dissolved oxygen (DO) levels of coastal ocean waters have decreased over the last few decades in part because of the increase in surface and subsurface water temperature caused by climate change, the reduction in ocean ventilation, and the increase in stratification and eutrophication....

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Bibliographic Details
Main Authors: P. Linford, I. Pérez-Santos, P. Montero, P. A. Díaz, C. Aracena, E. Pinilla, F. Barrera, M. Castillo, A. Alvera-Azcárate, M. Alvarado, G. Soto, C. Pujol, C. Schwerter, S. Arenas-Uribe, P. Navarro, G. Mancilla-Gutiérrez, R. Altamirano, J. San Martín, C. Soto-Riquelme
Format: Article
Language:English
Published: Copernicus Publications 2024-03-01
Series:Biogeosciences
Online Access:https://bg.copernicus.org/articles/21/1433/2024/bg-21-1433-2024.pdf

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https://bg.copernicus.org/articles/21/1433/2024/bg-21-1433-2024.pdf

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