Editorial Type:
Article
Article Type:
Research Article

NOTE ON ESTIMATION OF VERTICAL MOTION BY THE OMEGA EQUATION

DUŠAN DJURIC Department of Meteorology, Texas A&M University, College Station, Tex.

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Print Publication:
01 Dec 1969
DOI:
https://doi.org/10.1175/1520-0493(1969)097<0902:NOEOVM>2.3.CO;2
Page(s):
902–904
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Abstract

An interpretation of the ω-equation shows that upward motion is closely related to the advection of vorticity in the upper troposphere and to warm advection in the lower troposphere. Examples are presented to illustrate both effects.

Abstract

An interpretation of the ω-equation shows that upward motion is closely related to the advection of vorticity in the upper troposphere and to warm advection in the lower troposphere. Examples are presented to illustrate both effects.

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