Linear baroclinic instability in the Martian atmosphere

A spherical quasi-geostrophic model is used in an examination of linear baroclinic instability in such zonal-mean flows as those of the Martian atmosphere in winter, under both relatively nondusty and very dusty conditions. These zonal flows, which possess both vertical and meridional shear, are cha...

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Veröffentlicht in:Journal of the atmospheric sciences 1984-05, Vol.41 (9), p.1536-1550
1. Verfasser: Barnes, J. R.
Format: Artikel
Sprache:eng
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