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Abstract
This study reveals a near doubling of monsoon depressions (MDs) over the North Arabian Sea between 2001-2022 compared to 1981-2000. This increase is attributed to changes in dynamic and thermodynamic conditions, including heightened sea surface temperature, moisture flux, and convergence. A poleward shift in the low-level jet, influenced by East Asian jet variability, plays a significant role. This increase contrasts with a decline in MDs over the Bay of Bengal and contributes to increased rainfall over northwestern India.
Publisher
npj Climate and Atmospheric Science
Published On
Aug 09, 2024
Authors
Nagaraju Chilukoti, Mahendra Nimmakant, Jasti S. Chowdary
Tags
monsoon depressions
North Arabian Sea
climate change
rainfall
sea surface temperature
low-level jet
moisture flux
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