The parameterization of baroclinic instability in a minimal model

Wirth, A. (2000) The parameterization of baroclinic instability in a minimal model Journal of Marine Research, 58 . pp. 571-583. DOI 10.1357/002224000321511025.

s3-2.pdf - Published Version

Download (182Kb) | Preview

Supplementary data:


Baroclinic instability of zonally forced flow in a two mode quasi-geostrophic numerical model with periodic boundary conditions is considered. Only the largest scale of the baroclinic mode is forced and the scale dependence of a diffusive parameterization of baroclinic layer thickness is determined. It is shown that the effect of baroclinic instability is a decreasing function of scale with an exponent of about half of that corresponding to the commonly used Laplace operator. We furthermore show that there is no linear relation between the time averaged amplitude of the large scale streamfunction (or quasi-geostrophic potential vorticity) and the bolus velocity.

Document Type: Article
Research affiliation: OceanRep > Institute for Marine Science Kiel
Refereed: Yes
DOI etc.: 10.1357/002224000321511025
ISSN: 0022-2402
Date Deposited: 18 Feb 2008 17:24
Last Modified: 28 Nov 2017 13:26

Actions (login required)

View Item View Item

Document Downloads

More statistics for this item...