两个相反标志的准地转浅水涡旋斑块的稳定性和演化

IF 1.1 4区 地球科学 Q3 ASTRONOMY & ASTROPHYSICS Geophysical and Astrophysical Fluid Dynamics Pub Date : 2020-05-13 DOI:10.1080/03091929.2020.1756283
M. Jalali, D. Dritschel
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引用次数: 11

摘要

在准地转近似下,研究了单层浅水流中具有相反符号、均匀位涡异常的两个斑块的平衡形式、线性稳定性和非线性演化。我们广泛地改变了涡旋面积比、位涡异常比以及罗斯比变形长度,以揭示该系统中可能相互作用的全部复杂性。在之前的一项研究中(Jalali和Dritschel 2018,《地球物理学》)全面研究了相反符号的涡旋相互作用,结果证明比它们的同类符号要丰富得多。12,54。流体动力学,2018,112,375)。不稳定的平衡可能演变成无数种形式,许多是不稳定的和非周期性的,最初的两个漩涡块可能分裂成许多块,这些块可以存活很长时间,也许是无限期的。
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Stability and evolution of two opposite-signed quasi-geostrophic shallow-water vortex patches
We examine the equilibrium forms, linear stability and nonlinear evolution of two patches having opposite-signed, uniform potential vorticity anomalies in a single-layer shallow-water flow, under the quasi-geostrophic approximation. We widely vary the vortex area ratio, the potential vorticity anomaly ratio, as well as the Rossby deformation length to unravel the full complexity of possible interactions in this system. Opposite-signed vortex interactions turn out to be far richer than their like-signed counterparts, comprehensively examined in a previous study (Jalali and Dritschel 2018, Geophys. Astrophys. Fluid Dyn. 2018, 112, 375). Unstable equilibria may evolve into a myriad of forms, many unsteady and aperiodic, and the original two vortex patches may break up into many patches which survive for long times, perhaps indefinitely.
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来源期刊
Geophysical and Astrophysical Fluid Dynamics
Geophysical and Astrophysical Fluid Dynamics 地学天文-地球化学与地球物理
CiteScore
3.10
自引率
0.00%
发文量
14
审稿时长
>12 weeks
期刊介绍: Geophysical and Astrophysical Fluid Dynamics exists for the publication of original research papers and short communications, occasional survey articles and conference reports on the fluid mechanics of the earth and planets, including oceans, atmospheres and interiors, and the fluid mechanics of the sun, stars and other astrophysical objects. In addition, their magnetohydrodynamic behaviours are investigated. Experimental, theoretical and numerical studies of rotating, stratified and convecting fluids of general interest to geophysicists and astrophysicists appear. Properly interpreted observational results are also published.
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