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Technical CommentsResponse to Comment on "The Great Sumatra-Andaman Earthquake of 26 December 2004"
We support the revised estimate of tsunami source length (
1 Earth Sciences Department, University of California, Santa Cruz, CA 95064, USA. 800 km) obtained by Neetu et al. Sea-level monitoring with a high sampling rate, good azimuthal coverage, and real-time access, along with detailed bathymetry data around the stations, would improve source region estimation from tsunami arrival times.
2 Institute of Geophysics and Planetary Physics, University of California, Santa Cruz, CA 95064, USA. 3 Seismological Laboratory, California Institute of Technology, MS 252-21, Pasadena, CA 91125, USA. 4 Department of Geosciences, The Pennsylvania State University, 440 Deike Building, University Park, PA 16802, USA. 5 Department of Earth and Planetary Sciences, Harvard University, 20 Oxford Street, Cambridge, MA 02138, USA. 6 Department of Earth and Environmental Science and Geophysical Research Center, New Mexico Institute of Mining and Technology, Socorro, NM 87801, USA. 7 Department of Geosciences, The University of Arizona, Gould-Simpson Building #77, Tucson, AZ 85721, USA. 8 Department of Geology and Geophysics, University of WisconsinMadison, 1215 West Dayton Street, Madison, WI 53706, USA. 9 Geology Department, Miami University, Oxford, OH 45056, USA. 10 IRIS Consortium, 1200 New York Avenue, NW, Washington, DC 20005, USA. 11 Geological Survey of Japan, Advanced Industrial Sciences and Technology, Site C7 1-1-1 Higashi, Tsukuba 305-8567 Japan. 12 National Earthquake Information Center, U.S. Geological Survey, Golden, CO 80401, USA. * To whom correspondence should be addressed. E-mail: thorne{at}pmc.ucsc.edu
The editors suggest the following Related Resources on Science sites:In Science Magazine
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Science. ISSN 0036-8075 (print), 1095-9203 (online)