Forecasting of cirriform clouds over Northern India, Pakistan and Afghanistan from constant pressure charts
DOI:
https://doi.org/10.54302/mausam.v21i3.5405Abstract
Advection of vorticity at an upper air level below tropopause is indicative of the vertical motions in the upper troposphere. It has been shown that the regions of positive advection of vorticity at 300 mb are most probable I regions for the occurrence of high clouds in winter. The forecasting value of this relationship has also been briefly discussed.
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