Increased melt from Greenland’s most active glacier fuels enhanced coastal productivity

Abstract Seasonal phytoplankton blooms in Greenland’s coastal waters form the base of marine food webs and contribute to oceanic carbon uptake. In Qeqertarsuup Tunua, West Greenland, a secondary summertime bloom follows the Arctic spring bloom, enhancing annual primary productivity. Emerging evidenc...

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Main Authors: Michael Wood, Dustin Carroll, Ian Fenty, Clément Bertin, Basil Darby, Stephanie Dutkiewicz, Mark Hopwood, Ala Khazendar, Lorenz Meire, Hilde Oliver, Tara Parker, Josh Willis
Format: Article
Language:English
Published: Nature Portfolio 2025-08-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-025-02599-1
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author Michael Wood
Dustin Carroll
Ian Fenty
Clément Bertin
Basil Darby
Stephanie Dutkiewicz
Mark Hopwood
Ala Khazendar
Lorenz Meire
Hilde Oliver
Tara Parker
Josh Willis
author_facet Michael Wood
Dustin Carroll
Ian Fenty
Clément Bertin
Basil Darby
Stephanie Dutkiewicz
Mark Hopwood
Ala Khazendar
Lorenz Meire
Hilde Oliver
Tara Parker
Josh Willis
author_sort Michael Wood
collection DOAJ
description Abstract Seasonal phytoplankton blooms in Greenland’s coastal waters form the base of marine food webs and contribute to oceanic carbon uptake. In Qeqertarsuup Tunua, West Greenland, a secondary summertime bloom follows the Arctic spring bloom, enhancing annual primary productivity. Emerging evidence links this summer bloom to subglacial discharge from Sermeq Kujalleq, the most active glacier on the Greenland Ice Sheet. This discharge drives localized upwelling that may alleviate nutrient limitation in surface waters, yet this mechanism remains poorly quantified. Here, we employ a high-resolution biogeochemical model nested within a global state estimate to assess how discharge-driven upwelling influences primary productivity and carbon fluxes. We find that upwelling increases summer productivity by 15–40% in Qeqertarsuup Tunua, yet annual carbon dioxide uptake rises by only  ~3% due to reduced solubility in plume-upwelled waters. These findings suggest that intensifying ice sheet melt may alter Greenland’s coastal productivity and carbon cycling under future climate scenarios.
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id doaj-art-1a265b4bfb9b40ec8c8c4f8d5ac4b87c
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issn 2662-4435
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publishDate 2025-08-01
publisher Nature Portfolio
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series Communications Earth & Environment
spelling doaj-art-1a265b4bfb9b40ec8c8c4f8d5ac4b87c2025-08-20T03:06:08ZengNature PortfolioCommunications Earth & Environment2662-44352025-08-016111210.1038/s43247-025-02599-1Increased melt from Greenland’s most active glacier fuels enhanced coastal productivityMichael Wood0Dustin Carroll1Ian Fenty2Clément Bertin3Basil Darby4Stephanie Dutkiewicz5Mark Hopwood6Ala Khazendar7Lorenz Meire8Hilde Oliver9Tara Parker10Josh Willis11Moss Landing Marine Labs, San José State UniversityMoss Landing Marine Labs, San José State UniversityJet Propulsion Laboratory, California Institute of TechnologyJet Propulsion Laboratory, California Institute of TechnologyMoss Landing Marine Labs, San José State UniversityMassachusetts Institute of Technology CambridgeDepartment of Ocean Science and Engineering, Southern University of Science and TechnologyJet Propulsion Laboratory, California Institute of TechnologyGreenland Climate Research Centre, Greenland Institute of Natural ResourcesWoods Hole Oceanographic InstitutionMoss Landing Marine Labs, San José State UniversityJet Propulsion Laboratory, California Institute of TechnologyAbstract Seasonal phytoplankton blooms in Greenland’s coastal waters form the base of marine food webs and contribute to oceanic carbon uptake. In Qeqertarsuup Tunua, West Greenland, a secondary summertime bloom follows the Arctic spring bloom, enhancing annual primary productivity. Emerging evidence links this summer bloom to subglacial discharge from Sermeq Kujalleq, the most active glacier on the Greenland Ice Sheet. This discharge drives localized upwelling that may alleviate nutrient limitation in surface waters, yet this mechanism remains poorly quantified. Here, we employ a high-resolution biogeochemical model nested within a global state estimate to assess how discharge-driven upwelling influences primary productivity and carbon fluxes. We find that upwelling increases summer productivity by 15–40% in Qeqertarsuup Tunua, yet annual carbon dioxide uptake rises by only  ~3% due to reduced solubility in plume-upwelled waters. These findings suggest that intensifying ice sheet melt may alter Greenland’s coastal productivity and carbon cycling under future climate scenarios.https://doi.org/10.1038/s43247-025-02599-1
spellingShingle Michael Wood
Dustin Carroll
Ian Fenty
Clément Bertin
Basil Darby
Stephanie Dutkiewicz
Mark Hopwood
Ala Khazendar
Lorenz Meire
Hilde Oliver
Tara Parker
Josh Willis
Increased melt from Greenland’s most active glacier fuels enhanced coastal productivity
Communications Earth & Environment
title Increased melt from Greenland’s most active glacier fuels enhanced coastal productivity
title_full Increased melt from Greenland’s most active glacier fuels enhanced coastal productivity
title_fullStr Increased melt from Greenland’s most active glacier fuels enhanced coastal productivity
title_full_unstemmed Increased melt from Greenland’s most active glacier fuels enhanced coastal productivity
title_short Increased melt from Greenland’s most active glacier fuels enhanced coastal productivity
title_sort increased melt from greenland s most active glacier fuels enhanced coastal productivity
url https://doi.org/10.1038/s43247-025-02599-1
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