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- W1987895767 abstract "We derive the simple partial differential equations satisfied by the basic state of 3D vortex motions. There exist those basic patterns that low-pressure convergence leads to uplift motion and high-pressure divergence leads to down-flow in the atmospheric vortex motions. These basic states of 3D velocity field can be described in terms of stream function and convective velocity potential decompositions, and there are spiral structures in these motions. When Re → ∞, vortex motion degenerates as geostrophic wind, and corresponding vortex motion approximation is replaced by geostrophic approximation." @default.
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- W1987895767 date "2003-07-01" @default.
- W1987895767 modified "2023-09-23" @default.
- W1987895767 title "From 2D Geostrophic Wind to 3D Vortex Motions" @default.
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- W1987895767 doi "https://doi.org/10.1002/cjg2.3384" @default.
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