Convection in the central Irminger Sea; insights into variability and the roles of surface forcing and stratification from 19 years of high resolution mooring data
Transformation of light to dense waters by atmospheric cooling is key to the Atlantic Meridional Overturning in the Subpolar Gyre. Convection in the center of the Irminger Gyre determines the transformation of the densest waters east of Greenland. We present a 19-year (2002-2020) weekly time series...
Main Authors: | , , , , |
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Format: | Other/Unknown Material |
Language: | unknown |
Published: |
Authorea, Inc.
2023
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Subjects: | |
Online Access: | http://dx.doi.org/10.22541/essoar.170224470.00172869/v1 |