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- W1572872859 abstract "Equilibration of two-dimensional shallow water turbulence is examined in the presence of small-scale, isotropic forcing, and two forms of large-scale energy dissipation representative of different geophysical situations: (i) linear friction, as a model of flow over a solid ground; and (ii) thermal damping, as a model of energy loss through long-wave cooling. The simplest case of constant background planetary rotation allows an immediate comparison of the two dissipation mechanisms in purely isotropic, homogeneous turbulence. In each case a population of coherent vortices, containing most of the total kinetic energy of the flow, forms at scales larger than the forcing scale. A simple vortex identification criterion reveals that the number density of vortices as a function of vortex size is independent of dissipation mechanism, but that the intensity of vortices grows with scale more strongly in the case of thermal dissipation than in the case of frictional dissipation. The scaling of the vortex population in physical space is shown to be consistent with the distribution of energy in spectral space, and can be understood in terms of the scale-selectivity of the two dissipation mechanisms." @default.
- W1572872859 created "2016-06-24" @default.
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- W1572872859 date "2009-01-01" @default.
- W1572872859 modified "2023-09-27" @default.
- W1572872859 title "Large-scale energy dissipation and equatorial superrotation in shallow water turbulence" @default.
- W1572872859 doi "https://doi.org/10.1007/978-3-642-03085-7_226" @default.
- W1572872859 hasPublicationYear "2009" @default.
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