PUMA
Istituto di Scienze Marine     
Crisciani F., Purini R., Severini M. Frictional dissipation at the interface of a two-layer quasi-geostrophic flow. In: Nuovo Cimento Della Societa Italiana Di Fisica C-Geophysics and Space Physics, vol. 31 (3) pp. 327 - 337. Soc Italiana Fisica, 2008.
 
 
Abstract
(English)
In two-layer ocean circulation models the possible dissipation mechanism arising at the interface between the layers is parameterised in terms of the difference between the horizontal velocities of the flow in each layer. We explain and derive such parameterisation by extending the classical Ekman theory, which originally refers to the surface and to the benthic boundary layers, to the interface of a quasi-geostrophic, two-layered flow.
DOI: 10.1393/ncc/i2008-10299-y
Subject ocean circulation model


Icona documento 1) Download Document PDF


Icona documento Open access Icona documento Restricted Icona documento Private

 


Per ulteriori informazioni, contattare: Librarian http://puma.isti.cnr.it

Valid HTML 4.0 Transitional