A diagnostic study of extreme precipitation over Kerala during August 2018

K. Vijaya Kumari, Challa Venkata Srinivas, Ghouse Basha, Hari Prasad Dasari, Sabique Langodan, M. Venkat Ratnam, Ibrahim Hoteit

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45 Scopus citations

Abstract

The state of Kerala, located on the west coast of India, experienced a record 100-year flood that resulted in major landslides from unprecedented prolonged and extremely heavy rainfall (50–480 mm·day−1) during August 1–19, 2018, causing extensive damage and about 500 causalities. Rainfall observations indicate that the heavy rainfall occurred over two spells (August 7–10 and 14–18) in association with an offshore trough, and a depression over the Bay of Bengal (BOB). High-resolution 38-year climatology data (5 km) and the ERA-Interim reanalysis dataset show a strong low-level jet over the Arabian Sea and a depression over the BOB with a southwestward tilt during the heavy rainfall. Very high-resolution (2-km) mesoscale model simulations suggest that this high convective instability due to the strong westerly jet along with the formation of offshore vortex, the transport of mid-tropospheric moisture under the presence of conducive vertical shear of horizontal wind, and transport of mid-tropospheric moisture from the BOB are the major factors (as shown in the schematic diagram) behind the extreme heavy rainfall over Kerala.
Original languageEnglish (US)
JournalAtmospheric Science Letters
Volume20
Issue number12
DOIs
StatePublished - Nov 28 2019

Bibliographical note

KAUST Repository Item: Exported on 2020-10-01
Acknowledgements: The authors thank the India Meteorological Department (IMD) for providing access to the automatic weather, rain gauge station data, synoptic weather charts, Doppler weather radar products, and gridded rainfall estimates. The model simulations were carried out on the KAUST Supercomputing Facility. H.P.D. and S.L. acknowledge funding from Saudi ARAMCO. Authors gratefully acknowledge the anonymous reviewers for constructive the suggestions and comments to improve the quality of the paper.

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