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
Published in:Geoscientific Model Development
Main Authors: Heuzé, C., Ridley, J. K., Calvert, D., Stevens, D. P., Heywood, K. J.
Format: Article in Journal/Newspaper
Language:English
Published: 2015
Subjects:
Online Access:https://ueaeprints.uea.ac.uk/id/eprint/54694/
https://ueaeprints.uea.ac.uk/id/eprint/54694/2/HRCSH15.pdf
https://doi.org/10.5194/gmd-8-3119-2015