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单词 equivalent barotropic model
释义 equivalent barotropic model
[i`kwiv·ǝ·lǝnt bar·ǝ`träp·ik `mäd·ǝl]
METEOROLOGY
A model atmosphere characterized by frictionless and adiabatic flow and by hydrostatic quasigeostrophic equilibrium, and in which the vertical shear of the horizontal wind is assumed to be proportional to the horizontal wind itself.
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