Sea-air methane flux estimates derived from marine surface observations andinstantaneous atmospheric measurements in the northern Labrador Sea and Baffin Bay

Vast amounts of methane (CH4) stored in submarine sediments are susceptible to release in a warming Arctic, further exacerbating climate change in a positive feedback. It is therefore critical to monitor CH4 over pan-regional scales to detect early signs of CH4 release. However, our ability to monitor CH4 is hampered in remote northern regions by sampling and logistical constraints, and few good baseline data exist in many areas. From high-resolution atmospheric CH4 measurements and discrete surface water samples, we estimated instantaneous sea-air CH4 fluxes at various locations. We also created a baseline study of current background levels of CH4 in North Atlantic waters based on the atmospheric CH4 data over 22 d in summer 2021 on a roughly 5100 km voyage in the northern Labrador Sea and Baffin Bay between 55 and 72 degrees N. In addition, we measured CH4 concentrations across the water column at various stations. Measured atmospheric mixing ratios of CH4 ranged from 1944 to 2012 ppbv, with a mean of 1966 +/- 8 ppbv and a baseline of 1954-1981 ppbv. Dissolved CH4 concentrations in the near-surface water peaked at 5.3 nmol L-1 within 1 km down-current of a known cold seep at Scott Inlet and were consistently oversaturated throughout the water column in Southwind Fjord, which is an area that has been recently affected by submarine landslides. Local sea-air CH4 fluxes ranged from 0.003-0.119 mu molm(-2) d(-1), indicating that the ocean released only small amounts of CH4 to the atmosphere at all stations. Atmospheric CH4 levels were also driven by meteorological, spatial, and temporal variations, and both onshore and ocean-based contributions to atmospheric CH4 mixing ratios are likely. Coupled high-resolution measurements of marine and atmospheric CH4 data have the potential to provide ongoing monitoring in a region susceptible to CH4 releases, as well as critical validation data for globalscale measurements and modelling.

Automated summary

Vast amounts of methane stored in submarine sediments in a warming Arctic are at risk of release, exacerbating climate change. Monitoring methane over large areas is essential, but it is challenging in remote northern regions due to constraints in sampling and logistics. This study provides valuable information on methane fluxes, concentrations, and atmospheric levels in the North Atlantic waters, highlighting the potential for ongoing monitoring and validation of global-scale measurements and modeling.