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dc.contributor.authorSrivastava, Kirti-
dc.contributor.authorDimri, V.P.-
dc.contributor.authorRani, V. Swaroopa-
dc.contributor.authorKumar, R. Krishna-
dc.contributor.authorNarain, Likhita-
dc.date.accessioned2011-11-18T04:21:31Z-
dc.date.available2011-11-18T04:21:31Z-
dc.date.issued2011-10-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://hdl.handle.net/123456789/13071-
dc.description620-623en_US
dc.description.abstractTsunami 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.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.40(5) [October 2011]en_US
dc.subjectTsunamien_US
dc.subjectMakranen_US
dc.subjectRatnagirien_US
dc.subjectMumbaien_US
dc.subjectWave heighten_US
dc.subjectShelf widthen_US
dc.titleWould Makran tsunami skip Mumbai, India? No it would reach 8 minutes later than Ratnagirien_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.40(5) [October 2011]

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