OOS2025-1035, updated on 26 Mar 2025
https://doi.org/10.5194/oos2025-1035
One Ocean Science Congress 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Summer greenhouse gases spatial variability from Svalbard and Norway fjords
Coraline Leseurre1, Bruno Delille2, Hannelore Theetaert1, Michiel T’Jampens1, and Thanos Gkritzalis1
Coraline Leseurre et al.
  • 1Flanders Marine Institute, VLIZ, Oostende, Belgium
  • 2Chemical Oceanography Unit, ULiège, Liège, Belgium

Since the beginning of the industrial era, the atmospheric greenhouse gases (GHG) have increased continuously (around +50% for carbon dioxide (CO2) and +150% for methane (CH4), for the two most important), causing the current climate change. In November 2023, the World Meteorological Organization (WMO) highlighted once again there are still significant uncertainties about the carbon cycle, its fluxes, and they stressed the importance to follow the non-CO2 GHG with greater global warming potential.

The ocean plays a crucial role in climate regulation as a sink of anthropogenic CO2, while surface seawater is naturally supersaturated in CH4, and shallow coastal waters are a source of CH4 to the atmosphere. However, the air-sea CO2 and CH4 fluxes are driven by different key processes depending on the region of the open or coastal ocean.

To improve the understanding of the processes driving the air-sea exchange of GHG, we investigate the CO2 and CH4 concentrations in open ocean and coastal areas affected by sea ice, glacier runoff and riverine inputs within the context of the European project GreenFeedBack. To do so, we measured CO2 and CH4 concentrations in surface water during a summer cruise (August 2024) conducted on board the RV Skagerak between Sweden, Norway and the Storfjorden in Svalbard. The data were obtained using a custom-made air-seawater equilibration system, that was connected to the vessel’s non-toxic seawater supply (equilibrator and Cavity Ring Down Spectrometer) and discrete sampling. We also investigated the depth distribution of CH4 and carbonate system parameters.

Our first results show very high CH4 concentration in surface seawater near marine-terminated glaciers in the Storfjorden, correlated with salinity gradient (but not the lowest salinity observed in Svalbard). In West-Svalbard, we found minimal CO2 concentration correlated with low salinity, indicating a potential impact of freshwater discharge from the glaciers systems.

How to cite: Leseurre, C., Delille, B., Theetaert, H., T’Jampens, M., and Gkritzalis, T.: Summer greenhouse gases spatial variability from Svalbard and Norway fjords, One Ocean Science Congress 2025, Nice, France, 3–6 Jun 2025, OOS2025-1035, https://doi.org/10.5194/oos2025-1035, 2025.