Unusual formation and movement of a deep depression over Rajasthan during the monsoon season
DOI:
https://doi.org/10.54302/mausam.v25i3.5246Abstract
An unusual formation arid intensification of a monsoon depression over Rajasthan is discussed. The upper air advection of positive vorticity in association with troughs in easterlies and westerlies on a pre-existing sea level system is found to be responsible for deepening. The uncommon southerly/south-eastern movement of the system is also explained.
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Published
01-07-1974
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[1]
K. . VEERARAGHAVAN and S. K. . GHOSH, “Unusual formation and movement of a deep depression over Rajasthan during the monsoon season”, MAUSAM, vol. 25, no. 3 & 4, pp. 399–402, Jul. 1974.
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