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Effects of a bottom boundary layer parameterization in a coarse-resolution model of the North Atlantic Ocean
SMHI, Research Department, Climate research - Rossby Centre.
2000 (English)In: Journal of Atmospheric and Oceanic Technology, ISSN 0739-0572, E-ISSN 1520-0426, Vol. 17, no 5, 698-707 p.Article in journal (Refereed) Published
Abstract [en]

The bottom boundary layer model approach of Beckmann and Doscher has been adopted for application in a coarse-resolution model of the North Atlantic Ocean. Both components of the approach (advective and conditional diffusive) are found to affect the deep water stratification and circulation. A significant deepening of the downward spreading North Atlantic Deep Water (NADW) is the major effect. This is associated with an enhanced spatial coverage of the NADW cell in the meridional circulation.

Place, publisher, year, edition, pages
2000. Vol. 17, no 5, 698-707 p.
National Category
Climate Research
Research subject
Climate
Identifiers
URN: urn:nbn:se:smhi:diva-1500DOI: 10.1175/1520-0426(2000)017<0698:EOABBL>2.0.CO;2ISI: 000087329100011OAI: oai:DiVA.org:smhi-1500DiVA: diva2:847726
Available from: 2015-08-21 Created: 2015-08-17 Last updated: 2015-08-21Bibliographically approved

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