Tropical cyclone hazard to Mumbai in the recent historical climate
Name
mwr-d-18-0419.1.pdf
Description
Published version
Size
1.92 MB
Format
Adobe PDF
Checksum (MD5)
c86e563aa780457ce9e926239d2d4db1
Author(s)
Emanuel, Kerry Andrew
Date Issued
July 2019
Journal
Monthly weather review
Publisher
American Meteorological Society
Citation
Sobel, Adam H., et al., "Tropical cyclone hazard to Mumbai in the recent historical climate." Monthly weather review 147, 7 (July 2019): p. 2355-66 doi 10.1175/MWR-D-18-0419.1 ©2019 Author(s)
Version
Final published version
Abstract
The hazard to the city of Mumbai, India, from a possible severe tropical cyclone under the recent historical climate is considered. The authors first determine, based on a review of primary sources, that the Bombay Cyclone of 1882, documented in a number of print and Internet sources and claimed to have caused 100 000 or more deaths, did not occur. Two different tropical cyclone hazard models, both of which generate large numbers of synthetic cyclones using environmental data-here taken from reanalyses in the satellite era-as input, are then used to quantify the hazard, in conjunction with historical observations. Both models indicate that a severe cyclone landfall at or near Mumbai is possible, though unlikely in any given year. Return periods for wind speeds exceeding 100 kt (1 kt = 0.5144ms-1) (the threshold for category 3 in the Saffir-Simpson hurricanewind scale) atMumbai itself are estimated to be in the range of thousands to greater than 10 000 years, while the return period for a storm with maximum wind speed of 100 kt or greater passing within 150 km of Mumbai (possibly close enough to generate a substantial storm surge at the city) is estimated to be around 500 years. Return periods for winds exceeding 65 kt (hurricane intensity on the Saffir-Simpson hurricane wind scale) are estimated to be around 200 years at Mumbai itself, and 50-90 years within 150 km. Climate change is not explicitly considered in this study, but the hazard to the city is likely to be increasing because of sea level rise as well as changes in storm climatology. ©2019
MIT Department
Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Terms of Use
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DOI of Published Version
https://doi.org/10.1175/MWR-D-18-0419.1
