Hello all, We discussed the physics of tsunami propagation at the last LSST SWG meeting, and a recent talk by Jay Melosh was quoted, saying that the dangers of these events has been overestimated. I just finished reading the papers by Hills and Mader, and by Ward and Asphaug; I would very much like to understand what, if anything, they did incorrectly in their calculations. Ward and Asphaug use simple energy arguments to predict the size of water waves from an impact, and propagate them with linear theory (and thus no run-up when the wave hits the continental shelf). Hills and Mader use empirical data from what I understood to be nuclear tests to come to similar conclusions, but push this further to estimate the effects of run-up and breaking; they claim that historical tsunamis show an increase of height of a factor 10-25 from the deep-water tsunami. The statement at the SWG meeting was that Melosh claims that the propagation of relatively short-wavelength waves from an impact is qualitatively different from these. I poked a bit around on the web, and wasn't able to find anything by him on this subject. This is of tremendous importance; does anyone have suggestions on how we can gain further understanding of this? Would it make sense to write to Melosh directly? Thanks, Michael LSST LSST LSST LSST LSST Mailing List Server LSST LSST LSST LSST LSST LSST LSST LSST This is message 34 in the lsst-general archive, URL LSST http://www.astro.princeton.edu/~dss/LSST/lsst-general/msg.34.html LSST http://www.astro.princeton.edu/cgi-bin/LSSTmailinglists.pl/show_subscription?list=lsst-general LSST The index is at http://www.astro.princeton.edu/~dss/LSST/lsst-general/INDEX.html LSST To join/leave the list, send mail to lsst-request@astro.princeton.edu LSST To post a message, mail it to lsst-general@astro.princeton.edu LSST LSST LSST LSST LSST LSST LSST LSST LSST LSST LSST LSST LSST LSST LSST LSST LSST