METHODS OF COMPUTING VERTICAL MOTION IN THE ATMOSPHERE

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  • 1 New York University
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Abstract

The theory of a number of different techniques for the computation of vertical motion in the atmosphere is discussed. A comparison of two independent techniques shows that both usually yield vertical velocities of the correct sign and order of magnitude.

Abstract

The theory of a number of different techniques for the computation of vertical motion in the atmosphere is discussed. A comparison of two independent techniques shows that both usually yield vertical velocities of the correct sign and order of magnitude.

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