The Life Cycle of a Stationary Cloud Cluster during the Indian Summer Monsoon: A Microphysical Investigation Using Polarimetric C-Band Radar

Multiplatform observations of the life cycle of a tropical continental mesoscale cloud cluster (CC) during the Indian summer monsoon, which contributed more than ~70 mm of rainfall over the arid peninsular Indian region, are presented in this study. The CC was characterized by a deep warm cloud laye...

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Bibliographic Details
Published in:Monthly weather review 2021-11, Vol.149 (11), p.3761-3780
Main Authors: Samanta, Soumya, Murugavel, P., Gurnule, Dinesh, Rao, Y. Jaya, Vivekanandan, Jothiram, Prabha, Thara V.
Format: Article
Language:English
Subjects:
Agglomeration
Aggregates
Aggregation
C band
Cloud microphysics
Clouds
Clusters
Convective cells
Convective clouds
Crystal structure
Crystals
Cumulus clouds
Electrification
Hail
Hydrometeors
Ice
Ice crystals
Life cycle
Life cycles
Melting
Monsoons
Polarimetric radar
Polarimetry
Radar
Rain
Raindrops
Rainfall
Summer
Summer monsoon
Tropical climate
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Summary:Multiplatform observations of the life cycle of a tropical continental mesoscale cloud cluster (CC) during the Indian summer monsoon, which contributed more than ~70 mm of rainfall over the arid peninsular Indian region, are presented in this study. The CC was characterized by a deep warm cloud layer with isolated convective cells in the initiation phase, merging of several deep cumulus clouds (~6 km) during the mature phase, growing up to ~15 km with mixed-phase and ice-phase cloud microphysical processes. Throughout the life cycle of the CC, polarimetric radar analyses revealed size sorting of falling raindrops, growth of dendritic particles, riming, aggregation, the occurrence of a saggy bright band, etc. The formation of big raindrops is observed during the initial convective rain, associated with the melting of hail. The stratiform counterpart is primarily associated with aggregates, ice crystals, and melting snow, resulting in surface rainfall. Aggregates are found to be the spatially dominant hydrometeor followed by ice crystals. The presence of vertically oriented ice crystals indicates active cloud electrification processes during the spatial aggregation of convective clouds. The dominant microphysical processes and precipitation pathways are illustrated. The study forms a benchmark case for model intercomparisons and evaluations.
ISSN:0027-0644
1520-0493
DOI:10.1175/MWR-D-20-0274.1