PPT-Tsunami Mathematics

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 . The syllabus for Mathematics I and Mathematics II is based on a single subject Mathematics Advanced GCE Questions on Mathematics II are intended to be more challenging than questions on Mathematics I The syllabus for Mathematics III is wider In desi 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 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?). 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://. . Chapter 5 . Tsunami. Tsunami is a “harbor wave”. Waves rise highest where focused in bays or harbors. Tsunami have many causes. S. udden displacement of large volume of water . Earthquake. Volcanic eruptions. 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. . 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 . HOW TO HELP AND SAVE OUR CHILDREN AND OUR PEOPLE FROM THE EARTHQUAKE AND TSUNAMI DISASTERS? Subanar Fadjar Shadiq SEAMEO QITEP in Mathematics Yogyakarta, Indonesia On 26 December 2004 , in Banda Join us for the TODOS 2020 Conference . Activating Agency for Student Access, Engagement, and Advancement in Mathematics. . June . 25 – 27, 2020. Scottsdale, AZ. https://www.todos-math.org/. . . 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