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Discovery of an unrecognized pathway carrying overflow waters toward the Faroe Bank Channel.
Chafik, Léon , Hátún, Hjálmar, Kjellsson, Joakim , Larsen, Karin Margretha H. , Rossby, Thomas and Berx, Barbara (2020) Discovery of an unrecognized pathway carrying overflow waters toward the Faroe Bank Channel. Nature Communications, 11 (1). Art.Nr. 3721. DOI 10.1038/s41467-020-17426-8.
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Abstract
The dense overflow waters of the Nordic Seas are an integral link and important diagnostic for the stability of the Atlantic Meridional Overturning Circulation (AMOC). The pathways feeding the overflow remain, however, poorly resolved. Here we use multiple observational platforms and an eddy-resolving ocean model to identify an unrecognized deep flow toward the Faroe Bank Channel. We demonstrate that anticyclonic wind forcing in the Nordic Seas via its regulation of the basin circulation plays a key role in activating an unrecognized overflow path from the Norwegian slope – at which times the overflow is anomalously strong. We further establish that, regardless of upstream pathways, the overflows are mostly carried by a deep jet banked against the eastern slope of the Faroe-Shetland Channel, contrary to previous thinking. This deep flow is thus the primary conduit of overflow water feeding the lower branch of the AMOC via the Faroe Bank Channel.
Document Type: | Article |
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Keywords: | air-sea interaction; anticyclone; eddy covariance; flow pattern; jet flow; meridional circulation; slope dynamics; wind forcing |
Research affiliation: | OceanRep > GEOMAR > FB1 Ocean Circulation and Climate Dynamics > FB1-ME Maritime Meteorology |
Refereed: | Yes |
Open Access Journal?: | Yes |
Publisher: | Nature Research |
Related URLs: | |
Projects: | Blue-Action, THOR, NACLIM |
Date Deposited: | 03 Aug 2020 07:58 |
Last Modified: | 08 Feb 2023 09:31 |
URI: | https://oceanrep.geomar.de/id/eprint/50245 |
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