On the mean meridional circulation during the contrasting periods of normal and below normal monsoon activity
DOI:
https://doi.org/10.54302/mausam.v36i1.1577Abstract
For the contrasting periods of normal and below normal monsoon activity, the mean meridional circulation (M.M.C.) over 80 deg. E was computed. It was found that during monsoon months this region is characterized by rising motion over 35 deg. Nand sinking motion over 15 deg. N. During a monsoon break period sinking motion over 15 deg. N is intensified mainly due to local cooling. Strong rising motion occurs over equatorial regions to compensate for this sinking motion.
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