Abstract
The barotropic and baroclinic disturbances axisymmetrized by the barotropic basic vortex are examined in an idealized modeling framework consisting of two layers. Using a Wentzel-Kramers-Brillouin approach, the radial propagation of a baroclinic disturbance is shown to be slower than a barotropic disturbance, resulting in a slower linear axisymmetrization for baroclinic disturbances. The slower-propagating baroclinic waves also cause more baroclinic asymmetric kinetic energy to be transferred directly to the barotropic symmetric vortex than from barotropic disturbances, resulting in a faster axisymmetrization process in the nonlinear baroclinic wave case than in the nonlinear barotropic wave case.
| Original language | English |
|---|---|
| Pages (from-to) | 1256-1266 |
| Number of pages | 11 |
| Journal | Advances in Atmospheric Sciences |
| Volume | 31 |
| Issue number | 6 |
| DOIs | |
| State | Published - Sep 1 2014 |
Keywords
- asymmetry
- baroclinicity
- vortex axisymmetrization