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.
Authors
- Lee-Gray Boze
- Camille Akhoudas (ORCID: https://orcid.org/0000-0003-4685-9948)
- Christian Stranne (ORCID: https://orcid.org/0000-0003-1004-5213)
- Martin Jakobsson (ORCID: https://orcid.org/0000-0002-9033-3559)
- J. Pohlman (ORCID: https://orcid.org/0000-0002-3563-4586)
- Brett F. Thornton (ORCID: https://orcid.org/0000-0002-5640-6419)
- Adam Ulfsbo (ORCID: https://orcid.org/0000-0001-7550-7381)
Institutions
- 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)
Publication Details
- 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
Funders
- Polarforskningssekretariatet
- Svenska Forskningsrådet Formas
- Vetenskapsrådet
- Stockholms Universitet