The formation of new quasi-stationary vortex patterns from the interaction of two identical vortices in a rotating fluid

被引:4
作者
Sokolovskiy, Mikhail A. [1 ,2 ]
Verron, Jacques [3 ]
Carton, Xavier J. [4 ]
机构
[1] Russian Acad Sci, Inst Water Problems, 3 Gubkina Str, Moscow 119333, Russia
[2] Russian Acad Sci, Shirshov Inst Oceanol, 36 Nahimovskiy Pr, Moscow 117997, Russia
[3] IGE, CS 40 700, F-38058 Grenoble 9, France
[4] UBO, IUEM, Lab Oceanog Phys & Spatiale, Rue Dumont DUrville, F-29280 Plouzane, France
基金
俄罗斯基础研究基金会;
关键词
Vortex interaction; Vortex merger; Filamentation; Triplet; Quasi-Geostrophy; 2-LAYER BAROCLINIC VORTICES; FINITE-CORE HETONS; GEOSTROPHIC VORTICES; MERGER; EVOLUTION; DYNAMICS; INSTABILITY; DIMENSIONS; MECHANISM; SURFACE;
D O I
10.1007/s10236-018-1163-7
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Within the framework of the quasi-geostrophic approximation, the interactions of two identical initially circular vortex patches are studied using the contour dynamics/surgery method. The cases of barotropic vortices and of vortices in the upper layer of a two-layer fluid are considered. Diagrams showing the end states of vortex interactions and, in particular, the new regime of vortex triplet formation are constructed for a wide range of external parameters. This paper shows that, in the nonlinear evolution of two such (like-signed) vortices, the filaments and vorticity fragments surrounding the merged vortex often collapse into satellite vortices. Therefore, the conditions for the formation and the quasi-steady motions of a new type of triplet-shaped vortex structure are obtained.
引用
收藏
页码:723 / 733
页数:11
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