A two-dimensional toy model for geophysical turbulence

被引:11
|
作者
Lindborg, Erik [1 ]
Mohanan, Ashwin Vishnu [1 ]
机构
[1] Royal Inst Technol, Dept Mech, Osquars Backe 18, Stockholm, Sweden
基金
瑞典研究理事会;
关键词
SHALLOW-WATER EQUATIONS; GEOSTROPHIC TURBULENCE; STRATIFIED TURBULENCE; ENERGY-SPECTRUM; INERTIAL-RANGE; GRAVITY-WAVES; DYNAMICS; EVOLUTION; AIRCRAFT; BALANCE;
D O I
10.1063/1.4985990
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
A toy model for large scale geophysical turbulence is constructed by making two modifications of the shallow water model. Unlike the shallow water model, the toy model has a quadratic expression for total energy, which is the sum of Available Potential Energy (APE) and Kinetic Energy (KE). More importantly, in contrast to the shallow water model, the toy model does not produce any shocks. Three numerical simulations with different forcing are presented and compared with the simulation of a full General Circulation Model (GCM). The energy which is injected cascades in a similar way as in the GCM. First, some of the energy is converted from APE to KE at large scales. The wave field then undergoes a forward energy cascade displaying shallow spectra, close to k(-5/3), for both APE and KE, while the vortical field either displays a k(-3)-spectrum or a more shallow spectrum, close to k(-5/3), depending on the forcing. In a simulation with medium forcing wave number, some of the energy which is converted from APE to KE undergoes an inverse energy cascade which is produced by nonlinear interactions only involving the rotational component of the velocity field. The inverse energy cascade builds up a vortical field at larger scales than the forcing scale. At these scales, coherent vortices emerge with a strong dominance of anticyclonic vortices. The relevance of the simulation results to the dynamics of the atmosphere is discussed as in possible continuations of the investigation. Published by AIP Publishing.
引用
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页数:12
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