Emerging Influence of Enhanced Greenland Melting on Boundary Currents and Deep Convection Regimes in the Labrador and Irminger Seas

• Published in: Geophysical Research Letters
• Main Authors: Schiller-Weiss, Ilana, Martin, Torge, Schwarzkopf, Franziska U.
• Format: Article in Journal/Newspaper
• Language: English
• Published: AGU (American Geophysical Union) 2024
• Subjects: Greenland; Ice Sheet; Labrador Sea; North Atlantic
• Online Access: https://oceanrep.geomar.de/id/eprint/60100/; https://oceanrep.geomar.de/id/eprint/60100/1/Geophysical%20Research%20Letters%20-%202024%20-%20Schiller%E2%80%90Weiss%20-%20Emerging%20Influence%20of%20Enhanced%20Greenland%20Melting%20on%20Boundary.pdf; https://oceanrep.geomar.de/id/eprint/60100/2/2024gl109022-sup-0001-supporting%20information%20si-s01.pdf; https://doi.org/10.1029/2024GL109022

Freshwater input from Greenland ice sheet melt has been increasing in the past decades from warming temperatures. To identify the impacts from enhanced meltwater input into the subpolar North Atlantic from 1997 to 2021, we use output from two nearly identical simulations in the eddy-rich model VIKING20X (1/20°) only differing in the freshwater input from Greenland: one with realistic interannually varying runoff increasing in the early 2000s and the other with climatologically (1961–2000) continued runoff. The majority of the additional freshwater remains within the boundary current enhancing the density gradient toward the warm and salty interior waters yielding increased current velocities. The accelerated boundary current shows a tendency to enhanced, upstream shifted eddy shedding into the Labrador Sea interior. Further, the experiments allow to attribute higher stratification and shallower mixed layers southwest of Greenland and deeper mixed layers in the Irminger Sea, particularly in 2015–2018, to the runoff increase in the early 2000s. Key Points The West Greenland Current (WGC) freshens and cools with the observed recent increase in meltwater runoff from Greenland The density gradient across the boundary current intensifies, strengthening the WGC and increasing local eddy formation Enhanced meltwater runoff contributed to an eastward shift in deep convection towards the Irminger Sea (2015–2018) Plain Language Summary Global warming has accelerated the melting of the Greenland ice sheet over the past few decades resulting in enhanced freshwater input into the North Atlantic. The additional freshwater can potentially inhibit deep water formation and have future implications on ocean circulation. To determine the influence from Greenland melt, we compare two high-resolution model experiments all with the same forcing but differing input of Greenland freshwater fluxes from 1997 to 2021. We find that in the experiment with realistically increasing Greenland meltwater, the water becomes fresher and cooler ...