Rapid Freshening of Iceland Scotland Overflow Water Driven by Entrainment of a Major Upper Ocean Salinity Anomaly
Author:
Affiliation:
1. Rosenstiel School of Marine and Atmospheric Sciences University of Miami Miami FL USA
2. Woods Hole Oceanographic Institute Woods Hole MA USA
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GL094396
Reference36 articles.
1. Hydrographic Variability in the Bottom Layer of the Iceland Basin
2. Overflow Waters at the Iceland–Faroe Ridge Observed in Multiyear Seaglider Surveys
3. Propagation of the “Great Salinity Anomaly” of the 1990s around the northern North Atlantic
4. Subpolar Mode Water in the northeastern Atlantic: 2. Origin and transformation;Brambilla E.;Journal of Geophysical Research,2008
5. Discovery of an unrecognized pathway carrying overflow waters toward the Faroe Bank Channel
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