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- W2127128875 abstract "The geostrophic adjustment, i.e. the relaxation of the rotating stratified fluid to the geostrophic equilibrium is a key process in geophysical fluid dynamics. We study it in idealized plan-parallel and axisymmetric configurations (semi-geostrophic adjustment) in a hierarchy of models of increasing complexity: rotating shallow water equations, two-layer rotating shallow water equations, and continuously stratified hydrostatic Boussinesq equations. We show that the use of Lagrangian variables allows for substantial advances in understanding the semigeostrophic adjustment and related issues: existence of the adjusted state (“slow manifold”), wave emission, wave trapping, and wave breaking, pulsating front solutions, symmetric/inertial instability, and frontogenesis." @default.
- W2127128875 created "2016-06-24" @default.
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- W2127128875 date "2010-01-01" @default.
- W2127128875 modified "2023-09-26" @default.
- W2127128875 title "Lagrangian Dynamics of Fronts, Vortices and Waves: Understanding the (Semi-)geostrophic Adjustment" @default.
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- W2127128875 doi "https://doi.org/10.1007/978-3-642-11587-5_4" @default.
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