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Abstract
This study uses 25 years of satellite data (1998–2022) to show that phytoplankton biomass and bloom phenology in the West Antarctic Peninsula are significantly changing due to anthropogenic climate change. Enhanced phytoplankton biomass, particularly in early austral autumn, results in longer blooms. Sea ice decline and intensification of the Southern Annular Mode (SAM) since 2010 are identified as key drivers. These ecological changes have potential far-reaching consequences for global carbon sequestration and Antarctic food webs.
Publisher
Nature Communications
Published On
Aug 02, 2024
Authors
Afonso Ferreira, Carlos R. B. Mendes, Raul R. Costa, Vanda Brotas, Virginia M. Tavano, Catarina V. Guerreiro, Eduardo R. Secchi, Ana C. Brito
Tags
phytoplankton
climate change
Antarctic Peninsula
sea ice decline
Southern Annular Mode
carbon sequestration
bloom phenology

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