Unraveling ocean $$\hbox {pCO}_{2}$$ dynamics in Northwest Greenland Fjords

We investigated the relative contributions of various factors that influence seasonal changes in sea surface partial pressure of <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mtext>CO</mml:mtext> <mml:mn>2</mml:mn></mml:msub> </mml:math> ( <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mtext>pCO</mml:mtext> <mml:mn>2</mml:mn></mml:msub> </mml:math> , calculated from the measured pH and total alkalinity) in four regions of northwestern Greenland: Nares Strait, Lincoln Sea, Sherard Osborn and Petermann fjords. Using the temperature minimum layer as a proxy for winter conditions, we examined <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mtext>pCO</mml:mtext> <mml:mn>2</mml:mn></mml:msub> </mml:math> dynamics from the onset of sea-ice melt to summer. Our findings revealed significant spatial variability in <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mtext>pCO</mml:mtext> <mml:mn>2</mml:mn></mml:msub> </mml:math> , driven by differences in temperature, freshwater inputs, and biological activity. In particular, in Sherard Osborn Fjord substantial freshwater inputs and strong stratification were found to enhance <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mtext>pCO</mml:mtext> <mml:mn>2</mml:mn></mml:msub> </mml:math> accumulation, while in Petermann Fjord biological <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mtext>CO</mml:mtext> <mml:mn>2</mml:mn></mml:msub> </mml:math> uptake was the main driver. This study, conducted in summer 2019, underscores the critical role of northwest Greenland's coastal waters as a summer <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mtext>CO</mml:mtext> <mml:mn>2</mml:mn></mml:msub> </mml:math> sink. It highlights the complex interplay of physical and biogeochemical processes in modulating <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mtext>pCO</mml:mtext> <mml:mn>2</mml:mn></mml:msub> </mml:math> , suggesting significant regional differences in <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mtext>CO</mml:mtext> <mml:mn>2</mml:mn></mml:msub> </mml:math> dynamics between two neighboring fjords.

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Journal
Scientific Reports
Published
2025-08-11
DOI
https://doi.org/10.1038/s41598-025-12720-1
Primary Topic
Arctic and Antarctic ice dynamics
Type
article
Field-Weighted Citation Impact
0.00

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article

Unraveling ocean $$\hbox {pCO}_{2}$$ dynamics in Northwest Greenland Fjords

Lee-Gray Boze, Camille Akhoudas, Christian Stranne, Martin Jakobsson et al.
Scientific Reports
Arctic and Antarctic ice dynamics
article

Unraveling ocean $$\hbox {pCO}_{2}$$ dynamics in Northwest Greenland Fjords

Lee-Gray Boze, Camille Akhoudas, Christian Stranne, Martin Jakobsson, J. Pohlman, Brett F. Thornton, Adam Ulfsbo
article en

Abstract

We investigated the relative contributions of various factors that influence seasonal changes in sea surface partial pressure of <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mtext>CO</mml:mtext> <mml:mn>2</mml:mn></mml:msub> </mml:math> ( <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mtext>pCO</mml:mtext> <mml:mn>2</mml:mn></mml:msub> </mml:math> , calculated from the measured pH and total alkalinity) in four regions of northwestern Greenland: Nares Strait, Lincoln Sea, Sherard Osborn and Petermann fjords. Using the temperature minimum layer as a proxy for winter conditions, we examined <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mtext>pCO</mml:mtext> <mml:mn>2</mml:mn></mml:msub> </mml:math> dynamics from the onset of sea-ice melt to summer. Our findings revealed significant spatial variability in <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mtext>pCO</mml:mtext> <mml:mn>2</mml:mn></mml:msub> </mml:math> , driven by differences in temperature, freshwater inputs, and biological activity. In particular, in Sherard Osborn Fjord substantial freshwater inputs and strong stratification were found to enhance <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mtext>pCO</mml:mtext> <mml:mn>2</mml:mn></mml:msub> </mml:math> accumulation, while in Petermann Fjord biological <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mtext>CO</mml:mtext> <mml:mn>2</mml:mn></mml:msub> </mml:math> uptake was the main driver. This study, conducted in summer 2019, underscores the critical role of northwest Greenland's coastal waters as a summer <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mtext>CO</mml:mtext> <mml:mn>2</mml:mn></mml:msub> </mml:math> sink. It highlights the complex interplay of physical and biogeochemical processes in modulating <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mtext>pCO</mml:mtext> <mml:mn>2</mml:mn></mml:msub> </mml:math> , suggesting significant regional differences in <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mtext>CO</mml:mtext> <mml:mn>2</mml:mn></mml:msub> </mml:math> dynamics between two neighboring fjords.

Scientific ReportsVol. 15(1)
United States Geological Survey (US), Stockholm University (SE), Geological Survey of Sweden (SE), Bolin Centre for Climate Research (SE), Woods Hole Coastal and Marine Science Center, Woods Hole Oceanographic Institution (US), University of Gothenburg (SE)
Polarforskningssekretariatet, Svenska Forskningsrådet Formas, Vetenskapsrådet, Stockholms Universitet
Life below water
Openalex Percentile: Top 75%
Arctic and Antarctic ice dynamics
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