TIROS II Window Radiation and Large Scale Vertical Motion

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  • 1 The Pennsylvania State University
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Abstract

The difference between observed window radiation and radiation expected without clouds was related to various synoptic parameter. The but correlation, 0.72, was obtained with vertical motion computed by the adiabatic methods at 700 mb. Other variables tested were meridional flow and vertical motion at other level.

Abstract

The difference between observed window radiation and radiation expected without clouds was related to various synoptic parameter. The but correlation, 0.72, was obtained with vertical motion computed by the adiabatic methods at 700 mb. Other variables tested were meridional flow and vertical motion at other level.

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