Increasing vertical mixing to reduce Southern Ocean deep convection in NEMO3.4

Increasing vertical mixing to reduce Southern Ocean deep convection in NEMO3.4

Most CMIP5 (Coupled Model Intercomparison Project Phase 5) models unrealistically form Antarctic Bottom Water by open ocean deep convection in the Weddell and Ross seas. To identify the mechanisms triggering Southern Ocean deep convection in models, we perform sensitivity experiments on the ocean mo...

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Bibliographic Details
Main Authors:	C. Heuzé, J. K. Ridley, D. Calvert, D. P. Stevens, K. J. Heywood
Format:	Article
Language:	English
Published:	Copernicus Publications 2015-10-01
Series:	Geoscientific Model Development
Online Access:	http://www.geosci-model-dev.net/8/3119/2015/gmd-8-3119-2015.pdf

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