Journal
JOURNAL OF PHYSICAL OCEANOGRAPHY
Volume 38, Issue 9, Pages 2104-2107Publisher
AMER METEOROLOGICAL SOC
DOI: 10.1175/2008JPO3827.1
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Funding
- Natural Environment Research Council [NER/T/S/2002/00481, soc010007] Funding Source: researchfish
- NERC [soc010007] Funding Source: UKRI
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It is demonstrated that current level models, both with and without assimilation, generate too shallow an overturning in the North Atlantic (just like their predecessors) because they do not reproduce the descent of plumes of cold water from the Greenland and Norwegian Seas. Consequently, the prediction of decadal change from one such model reported by C. Wunsch and P. Heimbach is queried.
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