You are here

Greenland freshwater pathways in the sub-Arctic Seas from model experiments with passive tracers

Title: Greenland freshwater pathways in the sub-Arctic Seas from model experiments with passive tracers.
Name(s): Dukhovskoy, Dmitry S., author
Myers, Paul G., author
Platov, Gennady, author
Timmermans, Mary-Louise, author
Curry, Beth, author
Proshutinsky, Andrey, author
Bamber, Jonathan L., author
Chassignet, Eric, author
Hu, Xianmin, author
Lee, Craig M., author
Somavilla, Raquel, author
Type of Resource: text
Genre: Text
Date Issued: 2016-01
Physical Form: computer
online resource
Extent: 1 online resource
Language(s): English
Abstract/Description: Accelerating since the early 1990s, the Greenland Ice Sheet mass loss exerts a significant impact on thermohaline processes in the sub-Arctic seas. Surplus freshwater discharge from Greenland since the 1990s, comparable in volume to the amount of freshwater present during the Great Salinity Anomaly events, could spread and accumulate in the sub-Arctic seas, influencing convective processes there. However, hydrographic observations in the Labrador Sea and the Nordic Seas, where the Greenland freshening signal might be expected to propagate, do not show a persistent freshening in the upper ocean during last two decades. This raises the question of where the surplus Greenland freshwater has propagated. In order to investigate the fate, pathways, and propagation rate of Greenland meltwater in the sub-Arctic seas, several numerical experiments using a passive tracer to track the spreading of Greenland freshwater have been conducted as a part of the Forum for Arctic Ocean Modeling and Observational Synthesis effort. The models show that Greenland freshwater propagates and accumulates in the sub-Arctic seas, although the models disagree on the amount of tracer propagation into the convective regions. Results highlight the differences in simulated physical mechanisms at play in different models and underscore the continued importance of intercomparison studies. It is estimated that surplus Greenland freshwater flux should have caused a salinity decrease by 0.06-0.08 in the sub-Arctic seas in contradiction with the recently observed salinification (by 0.15-0.2) in the region. It is surmised that the increasing salinity of Atlantic Water has obscured the freshening signal.
Identifier: FSU_libsubv1_wos_000371432200050 (IID), 10.1002/2015JC011290 (DOI)
Keywords: abrupt climate-change, Baffin Bay, decadal oscillations, deep convection, general-circulation models, global ocean, Greenland freshwater, Greenland Ice Sheet melting, ice-sheet, Labrador Sea, Nordic Seas, north-atlantic ocean, overturning circulation, sub-Arctic seas, thermohaline circulation, thermohaline circulation
Publication Note: The publisher’s version of record is available at
Persistent Link to This Record:
Owner Institution: FSU
Is Part Of: Journal of Geophysical Research-Oceans.
Issue: iss. 1, vol. 121

Choose the citation style.
Dukhovskoy, D. S., Myers, P. G., Platov, G., Timmermans, M. -L., Curry, B., Proshutinsky, A., … Somavilla, R. (2016). Greenland freshwater pathways in the sub-Arctic Seas from model experiments with passive tracers. Journal Of Geophysical Research-Oceans. Retrieved from