The Iceland-Faroe Slope Jet: a conduit for dense water toward the Faroe Bank Channel overflow

Dense water from the Nordic Seas passes through the Faroe Bank Channel and supplies the lower limb of the Atlantic Meridional Overturning Circulation, a critical component of the climate system. Yet, the upstream pathways of this water are not fully known. Here we present evidence of a previously un...

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Bibliographic Details
Published in:Nature Communications
Main Authors: Semper, Stefanie, Pickart, Robert S., Våge, Kjetil, Larsen, Karin Margretha H., Hátún, Hjálmar, Hansen, Bogi
Format: Text
Language:English
Published: Nature Publishing Group UK 2020
Subjects:
Article
Faroe Bank
Faroe Islands
Greenland
Denmark Strait
Greenland-Scotland Ridge
Iceland
Nordic Seas
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7585422/
http://www.ncbi.nlm.nih.gov/pubmed/33097704
https://doi.org/10.1038/s41467-020-19049-5
Description
Summary:Dense water from the Nordic Seas passes through the Faroe Bank Channel and supplies the lower limb of the Atlantic Meridional Overturning Circulation, a critical component of the climate system. Yet, the upstream pathways of this water are not fully known. Here we present evidence of a previously unrecognised deep current following the slope from Iceland toward the Faroe Bank Channel using high-resolution, synoptic shipboard observations and long-term measurements north of the Faroe Islands. The bulk of the volume transport of the current, named the Iceland-Faroe Slope Jet (IFSJ), is relatively uniform in hydrographic properties, very similar to the North Icelandic Jet flowing westward along the slope north of Iceland toward Denmark Strait. This suggests a common source for the two major overflows across the Greenland-Scotland Ridge. The IFSJ can account for approximately half of the total overflow transport through the Faroe Bank Channel, thus constituting a significant component of the overturning circulation in the Nordic Seas.

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