Quasigeostrophic ellipsoidal vortices in a two-dimensional strain field

被引:17
作者
Hashimoto, H [1 ]
Shimonishi, T [1 ]
Miyazaki, T [1 ]
机构
[1] Univ Electrocommun, Dept Mech & Control Engn, Chofu, Tokyo 1828585, Japan
关键词
geophysical fluid motion; quasigeostrophic equation; two-dimensional strain field; exact solution; linear instability;
D O I
10.1143/JPSJ.68.3863
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
Vortex motions in a stably stratified rotating fluid are considered theoretically, based on the quasigeostrophic approximation. A class of exact stationary solution is obtained, which represents an ellipsoidal volume with uniform potential vorticity Qa embedded in a two-dimensional uniform strain field (e) over cap with uniform background vorticity 2<(gamma)over cap>. In a pure strain held (<(gamma)over cap> = 0), stationary solutions are allowed for \(e) over cap/Q(0)\ < about 0.15. Similarly, stationary solutions are allowed for (e) over cap/Q(0) > shout -0.1 in a simple shear flow (<(gamma)over cap> = (e) over cap). We study the stability of these exact solutions against infinitesimal disturbances. In a pure strain field: highly elongated ellipsoids are shown to be unstable to Lame-modes whose order m is higher than 2. In a simple shear now, a highly elongated ellipsoid whose major asis is perpendicular to the Aom direction, is unstable, whereas any ellipsoidal vortex seems to be stable, if the major axis is parallel to the now direction.
引用
收藏
页码:3863 / 3880
页数:18
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