Role of unusual moisture transport across Equatorial Indian Ocean on the extreme rainfall event during Kerala flood 2018 |
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| Institution: | 1. Dept. of Atmospheric Sciences, School of Marine Sciences, Cochin University of Science and Technology, Kochi, India;2. Advance Centre for Atmospheric Radar Research, Cochin University of Science and Technology, Kochi, India;3. Physical Oceanography Division, National Institute of Oceanography, Dona-Paula, India;1. Ocean Analysis and Modelling Laboratory, School of Earth, Ocean and Climate Sciences, Indian Institute of Technology Bhubaneswar, Odisha, India;2. Ocean Observation Systems, National Institute of Ocean Technology, Chennai, India;1. University of Monastir, Faculty of Sciences of Monastir (FSM), UR13ES64, Analysis and Control of PDEs, 5019 Monastir, Tunisia;2. University of Carthage, National Institute of Marine Sciences and Technologies (INSTM), LR16INSTM04, Marine Environment Laboratory, 2025 Salammbô, Tunisia;3. Environmental Modeling Center (EMC), National Oceanic and Atmospheric Administration, MD, USA;1. Department of Earth Sciences, Science and Research Branch, Islamic Azad University, Tehran, Iran;2. Department of Space Physics, Institute of Geophysics, University of Tehran, Iran |
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| Abstract: | Southwestern Indian state, Kerala experienced extreme devastating statewide flood event of the century during 2018 monsoon season. In this study, an attempt has been made to bring out the salient dynamical factors contributed to the Kerala flood. There were 3 active spells over Kerala during 2018 Monsoon season. All the three spells were accustomed with the intrinsic factors of low frequency components of the active spells such as strength of monsoon Low Level Jet (LLJ), Monsoon depressions in the Bay of Bengal, favorable Madden-Julian oscillation (MJO) phases and Western Pacific systems. Though all the common ingredients remain same, the third spell is distinct with the less evaporation flux over Western and Central Arabian Sea and unusual moisture transport from maritime continent through South Equatorial Indian ocean (SEIO) towards the Kerala coast across Equator. Strong meridional pressure gradient force created by the combined effect of high pressure anomaly oriented Northwest-Southeast direction across tropical Indian ocean and anomalous low pressure along monsoon trough might have contributed to this unusual moisture transport across SEIO originating from west of Australia. The anomalous high pressure in South Indian ocean was greatly influenced by the position of the Mascarene high. Subtropical Indian ocean dipole (SIOD) also exhibits an influential role by altering tropical Southern Indian ocean dynamics in favor of the unusual moisture transport. The position of the monsoon depression and presence of typhoons in Western Pacific might have aided to this moisture transport. However, the normal moisture transport from Central Arabian sea towards Kerala coast by virtue of the strong LLJ along with additional moisture transport directly from South of maritime continent through SEIO across the Equator towards Kerala coast might have played a dominant role in the historical flood event over entire Kerala state. |
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| Keywords: | Extreme rainfall Equatorial Indian Ocean Moisture transport Kerala flood |
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