Rapid communication of upper‐ocean salinity anomaly to deep waters of the Iceland Basin indicates an AMOC short‐cut

Chafik, Léon; Holliday, N. Penny ORCID: https://orcid.org/0000-0002-9733-8002. 2022 Rapid communication of upper‐ocean salinity anomaly to deep waters of the Iceland Basin indicates an AMOC short‐cut. Geophysical Research Letters, 49 (3). 10.1029/2021GL097570

Before downloading, please read NORA policies.

Preview

Text Geophysical Research Letters - 2022 - Chafik - Rapid Communication of Upper‐Ocean Salinity Anomaly to Deep Waters of the.pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (1MB) | Preview

Abstract/Summary

The mooring observations of the Overturning in the Subpolar North Atlantic Program reveal a significant freshening of the Iceland Scotland overflow waters that did not involve the Nordic Seas, the source of the dense Deep North Atlantic Water (Devana et al., 2021, https://doi.org/10.1029/2021GL094396). Their study suggests that this freshening at depth in the Iceland Basin stems from the largest upper-ocean freshening event in 120 years that rapidly communicated through entrainment with the Iceland Scotland Overflow Waters. This communication, which is very likely driven by strong wintertime heat losses, strongly adds to our thinking that the progression of this extreme freshening event is providing us with a natural tracer that is helping to identify and understand key processes that determine the strength and variability of the overturning circulation and its sensitivity to ongoing climate change. Continued monitoring of the overturning in the North Atlantic is therefore necessary.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1029/2021GL097570
ISSN:	0094-8276
Date made live:	07 Feb 2022 19:28 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/531907

Actions (login required)

View Item

Document Downloads

More statistics for this item...