Comment on "The Great Sumatra-Andaman Earthquake of 26 December 2004"

Author:

Neetu S.123,Suresh I.123,Shankar R.123,Shankar D.123,Shenoi S. S. C.123,Shetye S.R.123,Sundar D.123,Nagarajan B.123

Affiliation:

1. National Institute of Oceanography, Dona Paula, Goa 403004, India.

2. The Institute of Mathematical Sciences, Chennai 600113, India.

3. Geodetic and Research Branch, Survey of India, Dehra Dun 248001, India.

Abstract

Lay et al . (Research Articles, 20 May 2005, p. 1127) estimated a 600-km length for the tsunami source region. Adding tide-gauge data from Paradip, the northernmost of the Indian east-coast stations and therefore the most critical constraint on the northern extent of the source, we estimate that its length was greater by ∼30%.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference7 articles.

1. The Great Sumatra-Andaman Earthquake of 26 December 2004

2. G. A. Ramadass personal communication 2005.

3. Earth Planets Space

4. The travel times as observed in the SOI tide gauges are Chennai 156 min; Visakhapatnam 161 min; and Paradip 151 min.

5. Methods are available as supporting material on Science Online.

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