We support the revised estimate of tsunami source length (∼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.
CITATION STYLE
Lay, T., Kanamori, H., Ammon, C. J., Nettles, M., Ward, S. N., Aster, R., … Sipkin, S. (2005). Response to Comment on “The Great Sumatra-Andaman Earthquake of 26 December 2004.” Science, 310(5753), 1431–1431. https://doi.org/10.1126/science.1119662
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