PPT-Tsunami Forecast Software

Nancy N Soreide DW Denbo Y Wei D Arcas VV Titov NOAA Center for Tsunami Research NOAA PMEL Seattle WA NOAA Center for Tsunami Research Chile tsunami event Feb 27 2010 YouTube video embedded in slide . A tsunami is a series of large ocean waves usually caused by a major oor, a landslide, or volcanic activity. Tsunamis the whole water column is moving, not just the surface. A tsunami can When tsuna The main tsunami threat to Greater Victoria comes from a subduction earthquake o the West Coast.A tsunami created elsewhere in the Paci c Basin would, at most, a ect low-lying coastal areas in Gre 2015 PDC. Mark . Boslough & Barbara Jennings. Sandia National Labs. Albuquerque, NM. Sandia is a . multiprogram. laboratory operated by Sandia Corporation, a Lockheed Martin Company,. for the United States Department of Energy under contract DE-AC04-94AL85000.. Year 8. Bell Work- Notes in Back of Book. Do you recognise this Newspaper?. What’s it about?. Where were you when this happened?. Lesson Objectives. . I understand what a tsunami is and can explain how it is caused. videos. Science of Big Waves . (KQED). Garrett McNamara . w/ . GoPro. , 90’+. Teahupoo. raw. 2013 . The energy of a wave travels ahead but the water itself does not. Why are there consistently bigger waves in the Pacific?. Tsunamis. Homework Questions. Would you live in an area at risk for tsunamis? If so, where?. What level of risk from tsunamis is acceptable to you? (How would you know if the risk was assessed accurately?). San Diego, CA February 8-9, 2012. Tsunami Modules . by . Comet. Erv. Petty. Alaska Division of Homeland Security and Emergency Management. https://www.meted.ucar.edu/. Multiple Tsunami Modules. October 2010. Waves part 2. Tsunami. Tsunami terminology. Japanese term meaning “. harbour. wave”. Also called “seismic sea waves”. Created by movement of the ocean floor by:. Underwater fault movement. Underwater avalanches. Earthquake Risk. Earthquakes are likely wherever plate movement stores energy in the rock along faults.. Geologists can determine earthquake risk by locating where faults are active and where past earthquakes have occurred.. Agenda. Agree how we work within the Earthquake and Tsunami group. . how to . trigger. the System. (for EQS and TSU). GMPEs (or in term of MMI) vs population density for EQs. Expected tsunami height for . ( see tsunami lessons 10 a and 10b). CASE STUDY JAPAN EARTHQUAKE AND TSUNAMI 2011. (see Tsunami lesson 10b….). The . Eyjafjallajokull. Volcano, Iceland 2010. ( Predominant volcanic hazards- ash and . Inundation Mapping . for Alaska Coastal . Communities. Alaska Highlights for 2011. NTHMP - CC Meeting. . San Diego, CA February 8-9, 2012. Ervin Petty. , Alaska Division of Homeland Security & Emergency Management. Donald W. Denbo, John R. Osborne. , . Clinton . K. Pells and Mike A. Traum. Joint Institute for the Study of the Atmosphere and Ocean (JISAO), University . of . Washington, Seattle, WA. NOAA/. PMEL NOAA Center for Tsunami Research, Pacific Marine Environmental Laboratory, Seattle, WA. VarthagamSoft - India\'s best ERP software provider