Articles | Volume 15, issue 15
https://doi.org/10.5194/bg-15-4781-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-15-4781-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Imprint of Southern Ocean mesoscale eddies on chlorophyll
GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, 24105, Germany
ETH Zurich, Environmental Physics, Institute of Biogeochemistry and Pollutant Dynamics, Zurich, 8092, Switzerland
Princeton University, Program in Atmospheric and Oceanic Sciences, Princeton, 08544, USA
Matthias Münnich
ETH Zurich, Environmental Physics, Institute of Biogeochemistry and Pollutant Dynamics, Zurich, 8092, Switzerland
Nicolas Gruber
ETH Zurich, Environmental Physics, Institute of Biogeochemistry and Pollutant Dynamics, Zurich, 8092, Switzerland
ETH Zurich, Center for Climate Systems Modeling, Zurich, 8092, Switzerland
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- Oceanic eddy-induced modifications to air–sea heat and CO2 fluxes in the Brazil-Malvinas Confluence L. Pezzi et al. 10.1038/s41598-021-89985-9
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Latest update: 14 Dec 2024
Short summary
Although mesoscale ocean eddies are ubiquitous in the Southern Ocean (SO), their regional and seasonal association with phytoplankton has not been quantified. We identify over 100 000 eddies and determine the associated phytoplankton biomass anomalies using satellite-based chlorophyll (Chl) as a proxy. The emerging Chl anomalies can be explained largely by lateral advection of Chl by eddies. This impact of eddies on phytoplankton may implicate downstream effects on SO biogeochemical properties.
Although mesoscale ocean eddies are ubiquitous in the Southern Ocean (SO), their regional and...
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