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Meteorological Conditions of Extreme Heavy Rains over Coastal City Mumbai

Shyama MohantyaSchool of Earth Ocean and Climate Sciences, Indian Institute of Technology Bhubaneswar, Odisha, India
bDepartment of Agronomy, Purdue University, West Lafayette, Indiana

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Madhusmita SwainaSchool of Earth Ocean and Climate Sciences, Indian Institute of Technology Bhubaneswar, Odisha, India
bDepartment of Agronomy, Purdue University, West Lafayette, Indiana

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Raghu NadimpalliaSchool of Earth Ocean and Climate Sciences, Indian Institute of Technology Bhubaneswar, Odisha, India
cIndia Meteorological Department, New Delhi, India

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K. K. OsuridDepartment of Earth and Atmospheric Sciences, National Institute of Technology Rourkela, Odisha, India

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U. C. MohantyaSchool of Earth Ocean and Climate Sciences, Indian Institute of Technology Bhubaneswar, Odisha, India

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Pratiman PatelbDepartment of Agronomy, Purdue University, West Lafayette, Indiana

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Dev NiyogibDepartment of Agronomy, Purdue University, West Lafayette, Indiana
eJackson School of Geosciences, The University of Texas at Austin, Austin, Texas
fDepartment of Civil, Architectural and Environmental Engineering, Cockrell School of Engineering, The University of Texas at Austin, Austin, Texas

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Abstract

The city of Mumbai, India, frequently receives extreme rainfall (>204.5 mm day−1) during the summer monsoonal period (June–September), causing flash floods and other hazards. An assessment of the meteorological conditions that lead to these rain events is carried out for 15 previous cases from 1980 to 2020. The moisture source for such rain events over Mumbai is generally an offshore trough, a midtropospheric cyclone, or a Bay of Bengal depression. The analysis shows that almost all of the extreme rain events are associated with at least two of these conditions co-occurring. The presence of a narrow zone of high sea surface temperature approximately along the latitude of Mumbai over the Arabian Sea can favor mesoscale convergence and is observed at least 3 days before the event. Anomalous wind remotely supplying copious moisture from the Bay of Bengal adds to the intensity of the rain event. The presence of midtropospheric circulation and offshore trough, along with the orographic lifting of the moisture, give a unique meteorological setup to bring about highly localized catastrophic extreme rainfall events over Mumbai. The approach adopted in this study can be utilized for other such locales to develop location-specific guidance that can aid the local forecasting and emergency response communities. Further, it also provides promise for using data-driven/machine learning–based pattern analysis for developing warning triggers.

Significance Statement

We have identified the meteorological conditions that lead to extreme heavy rains over Mumbai, India. They are that 1) at least two of these rain-bearing systems, offshore trough, midtropospheric circulation, and Bay of Bengal depression moving north-northwestward are concurrently present, 2) an anomalous high SST gradient is present along the same latitude as Mumbai, and 3) the Western Ghats orography favors the rainfall extreme to be highly localized over Mumbai.

© 2023 American Meteorological Society. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/PUBSReuseLicenses).

Publisher’s Note: This article was revised on 24 March 2023 to correct errors in the list of author affiliations, and to insert text to the Acknowledgements section that was mistakenly omitted when originally published.

Corresponding author: Dev Niyogi, happy1@utexas.edu

Abstract

The city of Mumbai, India, frequently receives extreme rainfall (>204.5 mm day−1) during the summer monsoonal period (June–September), causing flash floods and other hazards. An assessment of the meteorological conditions that lead to these rain events is carried out for 15 previous cases from 1980 to 2020. The moisture source for such rain events over Mumbai is generally an offshore trough, a midtropospheric cyclone, or a Bay of Bengal depression. The analysis shows that almost all of the extreme rain events are associated with at least two of these conditions co-occurring. The presence of a narrow zone of high sea surface temperature approximately along the latitude of Mumbai over the Arabian Sea can favor mesoscale convergence and is observed at least 3 days before the event. Anomalous wind remotely supplying copious moisture from the Bay of Bengal adds to the intensity of the rain event. The presence of midtropospheric circulation and offshore trough, along with the orographic lifting of the moisture, give a unique meteorological setup to bring about highly localized catastrophic extreme rainfall events over Mumbai. The approach adopted in this study can be utilized for other such locales to develop location-specific guidance that can aid the local forecasting and emergency response communities. Further, it also provides promise for using data-driven/machine learning–based pattern analysis for developing warning triggers.

Significance Statement

We have identified the meteorological conditions that lead to extreme heavy rains over Mumbai, India. They are that 1) at least two of these rain-bearing systems, offshore trough, midtropospheric circulation, and Bay of Bengal depression moving north-northwestward are concurrently present, 2) an anomalous high SST gradient is present along the same latitude as Mumbai, and 3) the Western Ghats orography favors the rainfall extreme to be highly localized over Mumbai.

© 2023 American Meteorological Society. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/PUBSReuseLicenses).

Publisher’s Note: This article was revised on 24 March 2023 to correct errors in the list of author affiliations, and to insert text to the Acknowledgements section that was mistakenly omitted when originally published.

Corresponding author: Dev Niyogi, happy1@utexas.edu
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