ABSTRACT

The tsunami of 26 December 2004 in the Indian Ocean has been analyzed and studied in detail by several authors (Kowalik et al., 2005a, b; Murty et al., 2005a-e; Murty et al., 2006; Nirupama et al., 2005a-b). About a dozen different physical oceanographic processes need to be invoked to explain the detailed physical characteristics of this tsunami.