The effect of diabatic heating on the change of surface pressure
DOI:
https://doi.org/10.54302/mausam.v38i1.2659Abstract
The equation of pressure tendency has been modified to consider the effect of atmospheric diabatic heating. The inclusion of heating shows a marked difference in estimated pressure for different altitudes. Thirtytwo cases of partially clear sky Conditions were examined. The layer 300/100mb seems to have the greatest effect on pressure variation.
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