PPT-Tsunami

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. 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. By: Conrad Ricks, Liz Anderson, Melissa Prater & Michelle Carleton. Source: http://www.bbc.co.uk/programmes/b011vg9w. Source: http://cempaka-nature.blogspot.com/2009/12/indonesias-next-big-quake-due-under.html. . Presented by Valisha Edwards, LMSW. The Silent Tsunami: Mental Health and Stress in the Workplace. Mental health issues and stress are a silent tsunami in the workplace, . one . that could engulf organizations . 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://. 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: . NTHMP Annual Report. February 2, 2011. Kevin J Richards. Hawaii’s – Accomplishments. NA5 - FY09. Mapping and Modeling Status*. Outreach Activities. School Visits. Committee Meetings. Workshops & Seminars . 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 . 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 . 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 . Eric Boldt. Warning Coordination Meteorologist. NOAA’s National Weather Service. 520 N. Elevar St. . Oxnard CA 93030. 805-988-6615. March 15, 2005. National Weather Service Mission Statement. " The National Weather Service (NWS) provides weather, hydrologic, and climate forecasts and warnings for the United States, its territories, adjacent waters and ocean areas, for the protection of life and property and the enhancement of the national economy. " .