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 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. Elder Angela Burns. September 23, 2015. Agenda. Recap. Forward and Introduction. Tsunami . Learning Objectives. Students will synthesize . and incorporate the . materials studied . into everyday life.. Stuart A. Weinstein. 1. , Laura S. L. Kong. 2. , Dailin Wang. 1. , Nathan C. Becker. 1. 1. Pacific Tsunami Warning Center, USA, stuart.weinstein@noaa.gov. 2. International Tsunami Information Center/UNESCO-NOAA, USA, l.kong@unesco.org. 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. Tsunami Outreach Oregon. Oregon Department of . Geology . and Mineral Industries . Earthquake Sources for Tsunamis . Local Oregon Tsunamis. Distant Tsunamis. Map modified from NOAA website: . http://. The name ‘tsunami’ is Japanese. . It means harbor wave. . Tsunamis used to be called tidal waves, but they actually have nothing to do with the tides.. The sudden displacement of huge amounts of water causes tsunamis. . Tsunami Mathematics. Mathematically there are three different but related factors involved in . relation . to a Tsunami.. These are SPEED, HEIGHT, and ENERGY POWER. . Tsunami Mathematics - SPEED. In the open Ocean the speed of a Tsunami is approximately: . 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. U.S. . coastlines minutes after the initial earthquake.. The 4G DART system consists of an anchored seafloor bottom pressure recorder (BPR) and a companion moored surface buoy for real time communications. BPRs are capable of detecting and measuring tsunamis with amplitudes as small as 1 mm in 6,000 m of water.. ( 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. 1Historical Hilo TsunamiHit by damaging tsunami in 1837 1841 1868 twice 1869 1872 1877 1883 1906 1918 1923 1933 1946 1957 1960 1975All but three of the above were caused by distant earthquakesThere ha