The simulation makes it clear how the tsunami struck the coastlines of Indonesia, Thailand, Sri Lanka and India with such devastating force, then continued as far as East Africa. The video, about 7 MB, can be seen online at http://www.news.cornell.edu/releases/Jan05/tsunamiVid320.html . A 640x480 Quicktime version, about 43 MB, is available at http://www.news.cornell.edu/releases/Jan05/tsunamiVid640.html. (This will take several minutes to load even on a fast Internet connection.) The video compresses 10 hours and 30 minutes in the life of the tidal wave into one minute, showing in contrasting colors the advancing high water and the trough behind it, as well as the receding waters observed along coastlines near the epicenter before the wave struck. It shows high water in red and low in blue. The more intense the color, the greater the displacement from sea level. A clock in the animation starts at the moment of the Sumatra earthquake. The supercomputer simulation was created using a numerical model called the Cornell Multigrid Coupled Tsunami model, or COMCOT, developed by Philip Liu, Cornell professor of civil and environmental engineering, and graduate student Xiaoming Wang. The model was originally created by Japanese scientists, further developed by Liu and several of his students, and most recently refined and updated by Wang. Wang created the final video with Tso-Ren Wu, a Cornell post-doctoral researcher. Liu, who helped develop the Pacific Ocean tsunami warning system, is currently leading a delegation of scientists studying the effects of the tsunami in Sri Lanka, and will report findings at a symposium there Jan. 15. The computer model assumes that the up-and-down motion of the sea floor caused by the earthquake occurred in just a few seconds, so the sea water above was deformed in the same way as the earth below, since there was no time for the water to get out of the way. Tsunamis are created when water is lifted by energy generated by earthquakes and then falls back. Based on earthquake data and information about the topography of the sea floor provided by the U.S. National Oceanic and Atmospheric Administration (NOAA), the COMCOT model calculates the elevation of the sea surface at a series of grid points on a map of the area over a period of time. The video is generated from this information. How closely the simulation corresponds to what actually happened will not be determined until data is collected in the field, Wang said. Accurate seismic data generally is available only after an event is over. With the future development of seismic technology, a more accurate and rapid estimation of seismic data might be provided, he said. It then might be possible to use such simulations to predict tsunami behavior immediately after an earthquake is detected.