Gerstner waves and their generalizations in hydrodynamics and geophysics

被引:6
作者
Abrashkin, A. A. [1 ,2 ]
Pelinovsky, E. N. [1 ,2 ,3 ]
机构
[1] Natl Res Univ Higher Sch Econ, Nizhny Novgorod Branch, Ul B Pecherskaya 25-12, Nizhnii Novgorod 603155, Russia
[2] Russian Acad Sci, Fed Res Ctr Inst Appl Phys, Ul Ulyanova 46, Nizhnii Novgorod 603950, Russia
[3] Nizhnii Novgorod State Tech Univ, Ul Minina 24, Nizhnii Novgorod 603950, Russia
关键词
Gerstner waves; Lagrangian coordinates; vorticity; Cauchy invariants; edge waves; Ptolemaic flows; rotating fluid; f-plane approximation; equatorially trapped waves; EDGE WAVES; WATER-WAVES; DEEP-WATER; CAUCHY INVARIANTS; INSTABILITY; SURFACE; FLOWS; FORMULATION; EQUATION;
D O I
10.3367/UFNe.2021.05.038980
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
To mark 220 years since the appearance of Gerstner's paper that proposed an exact solution to the hydrodynamic equations, an overview of exact solutions for water waves is given, each of which is a generalization of the Gerstner wave. Additional factors are coastal geometry, fluid rotation, varying pressure on the free surface, stratification, fluid compressibility, and background flows. Waves on a rotating Earth are studied in the f-plane approximation, and, in the near-equatorial region, also in the beta-plane approximation. The flows are described in Lagrangian variables. For all waves in the absence of background flows, the trajectories of liquid particles are circles, as in the Gerstner wave (hence, their common name - Gerstner-like).
引用
收藏
页码:453 / 467
页数:15
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