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• Cloud regimes in response to large-scale dynamical states are studied during the Indian monsoon ISO • Dynamical convergence dominates in modulating deep convective and shallow cumulus clouds • Moisture advection preconditions the development of deep convection by 4–6 days
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This page is a summary of: Cloud regime evolution in the Indian monsoon intraseasonal oscillation: Connection to large-scale dynamical conditions and the atmospheric water budget, Geophysical Research Letters, November 2015, American Geophysical Union (AGU),
DOI: 10.1002/2015gl066353.
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