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Effects of a bottom boundary layer parameterization in a coarse-resolution model of the North Atlantic Ocean
SMHI, Forskningsavdelningen, Klimatforskning - Rossby Centre.
2000 (engelsk)Inngår i: Journal of Atmospheric and Oceanic Technology, ISSN 0739-0572, E-ISSN 1520-0426, Vol. 17, nr 5, s. 698-707Artikkel i tidsskrift (Fagfellevurdert) 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.

sted, utgiver, år, opplag, sider
2000. Vol. 17, nr 5, s. 698-707
HSV kategori
Forskningsprogram
Klimat
Identifikatorer
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, id: diva2:847726
Tilgjengelig fra: 2015-08-21 Laget: 2015-08-17 Sist oppdatert: 2018-06-13bibliografisk kontrollert

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