A FOUR-LEVEL BAROCLINIC MODEL FOR THE STEADY PERTURBATIONS IN THE WESTERIES
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Abstract
The steady perturbations in the westeries are analysed by means of a four-levels barodinic model. It is shown that the intensity of the steady perturbations with wave number 1-2 caused by topography increases upward in the stratasphere during winter, and decreases upward in summer.
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