Sea-ice retreat suggests re-organization of water mass transformation in the Nordic and Barents Seas

Water mass transformation in the Nordic and Barents Seas, triggered by air-sea heat fluxes, is an integral component of the Atlantic Meridional Overturning Circulation (AMOC). These regions are undergoing rapid warming, associated with a retreat in ice cover. Here we present an analysis covering 195...

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Bibliographic Details
Published in:Nature Communications
Main Authors: Moore, G. W. K., Våge, K., Renfrew, I. A., Pickart, R. S.
Format: Text
Language:English
Published: Nature Publishing Group UK 2022
Subjects:
Article
Nordic Seas
Sea ice
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC8748645/
http://www.ncbi.nlm.nih.gov/pubmed/35013213
https://doi.org/10.1038/s41467-021-27641-6
Description
Summary:Water mass transformation in the Nordic and Barents Seas, triggered by air-sea heat fluxes, is an integral component of the Atlantic Meridional Overturning Circulation (AMOC). These regions are undergoing rapid warming, associated with a retreat in ice cover. Here we present an analysis covering 1950−2020 of the spatiotemporal variability of the air-sea heat fluxes along the region’s boundary currents, where water mass transformation impacts are large. We find there is an increase in the air-sea heat fluxes along these currents that is a function of the currents’ orientation relative to the axis of sea-ice change suggesting enhanced water mass transformation is occurring. Previous work has shown a reduction in heat fluxes in the interior of the Nordic Seas. As a result, a reorganization seems to be underway in where water mass transformation occurs, that needs to be considered when ascertaining how the AMOC will respond to a warming climate.

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