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Would Makran tsunami skip Mumbai, India? No it would reach 8 minutes later than Ratnagiri

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Field Value
 
Creator Srivastava, Kirti
Dimri, V.P.
Rani, V. Swaroopa
Kumar, R. Krishna
Narain, Likhita
 
Date 2011-11-18T04:21:31Z
2011-11-18T04:21:31Z
2011-10
 
Identifier 0975-1033 (Online); 0379-5136 (Print)
http://hdl.handle.net/123456789/13071
 
Description 620-623
Tsunami from Makran subduction zone in the northern Arabian sea are seen to arrive at Ratnagiri (16°56´24.00˝N, 72°40´12.00˝E) along the west coast of India 8 minutes earlier than Mumbai (18°59´24.00˝N,71°52´12.00˝E) in spite Ratnagiri being 244 km down south of Mumbai. This can give rise to a false signal and could be interpreted as tsunami skipped Mumbai and is traveling towards south. However, this advance information at Ratnagiri could be used for quick evacuation of densely populated coastal areas of Mumbai. Reasons for later arrival of tsunami at Mumbai is mainly due to a wide shelf of greater than 250 km whilst at Ratnagiri the shelf suddenly becomes half that of Mumbai. The importance of shelf width along the west coast of India which plays a great role in the arrival of the tsunami waves and the wave heights at different locations are conferred in the present study.
 
Language en_US
 
Publisher NISCAIR-CSIR, India
 
Rights <img src='http://nopr.niscair.res.in/image/cc-license-sml.png'> <a href='http://creativecommons.org/licenses/by-nc-nd/2.5/in' target='_blank'>CC Attribution-Noncommercial-No Derivative Works 2.5 India</a>
 
Source IJMS Vol.40(5) [October 2011]
 
Subject Tsunami
Makran
Ratnagiri
Mumbai
Wave height
Shelf width
 
Title Would Makran tsunami skip Mumbai, India? No it would reach 8 minutes later than Ratnagiri
 
Type Article