A note on the derivation of the quasi-geostrophic potential vorticity equation
The derivation of the quasi-geostrophic potential vorticity equation of mathematical meteorology is usually done using fairly sophisticated techniques of perturbation theory, but stops short of deriving self-consistently the stratification parameter of the mean atmospheric state. In this note we sug...
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| Médium: | Journal article |
| Jazyk: | English |
| Vydáno: |
2011
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