Deep convection in the Irminger Sea observed with a dense mooring array

Deep convection is a key process in the Atlantic Meridional Overturning Circulation, but because it acts at small scales, it remains poorly resolved by climate models. The occurrence of deep convection depends on weak initial stratification and strong surface buoyancy forcing, conditions that are sa...

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Bibliographic Details
Published in:Oceanography
Main Authors: de Jong, M. Femke, Oltmanns, Marilena, Karstensen, Johannes, de Steur, Laura
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/525942/
https://nora.nerc.ac.uk/id/eprint/525942/1/31-1_de_jong.pdf
https://doi.org/10.5670/oceanog.2018.109