Nancy N. Soreide, D.W. Denbo, Y. Wei, D. Arcas, V.V. Titov NOAA Center for Tsunami Research NOAA PMEL, Seattle, WA.

Slides:



Advertisements
Similar presentations
A 8.0 magnitude earthquake occurred offshore in the Solomon Islands. The earthquake occurred at a depth of 28.7 km (17.8 miles) and a tsunami warning was.
Advertisements

Tsunamis!.  A tsunami is a series of ocean waves generated by sudden movement in the sea floor.  In the deep ocean, the tsunami wave may only be a few.
Instrumentation and Quantification of Tsunamis With an Emphasis on the Santa Barbara Channel.
Magnitude 8.9 (9.0) earthquake near Sendai, east coast of Honshu, Japan Friday, March 11, 2011 at 05:46:23 UTC Japan was struck by a magnitude 8.9 (9.0)
Russian Academy of Sciences Far East Branch Institute of Marine Geology & Geophysics Yu. Korolev THE RETROSPECTIVE SHORT-TERM TSUNAMI FORECAST Novosibirsk.
Coupled with the DART 4G system, PMEL is working on the next generation Tsunami Forecast System. New modeling capability will use NOAA supercomputers to.
NOAA Tsunami Forecasting System: Design and Implementation Using Service Oriented Architecture D.W. Denbo 1, K.T. McHugh 1, J.R. Osborne 2, P. Sorvik 1,
Tsunami. Intro Video…
19 April 2005 JISAO Review University of Washington Seattle, WA Frank González Leader, Tsunami Research Program National Oceanic and Atmospheric Administration.
President’s Proposed Expansion of Tsunami Warning System Eddie Bernard Director, Pacific Marine Environmental Laboratory (PMEL)/NOAA Member, National Tsunami.
TSUNAMIS EXAMPLES AND DAMAGE.
Integrated Analyses for Monitoring and Rapid Source Modeling of Earthquakes and Tsunamis Brendan Crowell Subduction Zone Observatory Seminar May 13, 2015.
Next Slide  Most Tsunamis are caused by earthquakes generated in a subduction zones, an area where an oceanic plate is being forced down into.
Diego Arcas, Chris Moore, Stuart Allen NOAA/PMEL University of Washington.
-for saving innocent lives
Seismic waves Section 4.
Tsunami Warning System Elements IOC Assessment Mission to Indonesia 29 August-1 September 2005.
Today  Hand in any work needed.  Check the list in the back, if you owe something.  Get out a small piece of paper, PUT YOUR NAME ON IT.  When bell.
Hawaii’s Tsunami Warning System Aja Toscano KAPCC ICS 101.
Tsunamis GEOL 4093 Risk Assessment. Tsunamis Also known as “seismic sea waves” Generating force is not wind, but movement of the sea floor, volcano, landslide,
Using YouTube Videos to Communicate Science Nancy N. Soreide, Tracey Nakamura, Michael Dunlap NOAA Pacific Marine Environmental Laboratory AMS Meeting,
Tsunami Warning and Mitigation System Masahiro Yamamoto Tsunami Unit Intergovernmental Oceanographic Commission (IOC) UNESCO.
The 2004 Sumatra Tsunami and U.S. Tsunami Preparedness Harold Mofjeld NOAA/PMEL and NOAA Tsunami Research Program Seattle, Washington Harold Mofjeld NOAA/PMEL.
NOAA’s Role in Weather Forecasting and Community Preparedness Decision Support NOAA remains focused on supporting high impact events where weather is a.
NOAA Center for Tsunami Research Tweb: A Web-Based Tsunami Model Forecast Tool System Architecture and Development Eugene F. Burger 1, Linus Kamb 2, Tracey.
Magnitude 9.0 NEAR THE EAST COAST OF HONSHU, JAPAN Friday, March 11, 2011 at 05:46:23 UTC Japan was struck by a magnitude 9.0 earthquake off its northeastern.
1 Status on NOAA’s Plan to Strengthen the Tsunami Warning Program A Presentation to the NOAA Science Advisory Board Brig. Gen. David L. Johnson, USAF (Ret.)
TSUNAMI BASIC INFO 1.) Tsunami are NOT tidal waves, they have nothing to do with tides 2.) They are caused by “BIG SPLASHES” from… *earthquake motion (Fig.
Design and Implementation of an Operational Tsunami Forecast Tool Donald W. Denbo, John R. Osborne, Clinton K. Pells and Mike A. Traum Joint Institute.
U.S. National Tsunami Hazard Mitigation Program 5-Year Review David Green, NOAA Tsunami Program Manager National Oceanic and Atmospheric Administration.
Tsunami Warning System of SCS
Tsunami! Tidal waves of destruction CHAPTER 2, CRO #7.
Tsunamis: More Than a Splash Presentation By: Ka’ai Young, Ellie Goodrich, Geri Trower, & Ivan Maurer PHYSICS 1010.
NTHMP Warning Coordination Subcommittee Meeting February 1, 2011 Charles McCreery Director NOAA Pacific Tsunami Warning Center Pacific Tsunami Warning.
1 Building a Weather-Ready Nation. SITREP for March 21, 2011 FY 12 Budget Request SITREP for March 21, 2011 FY 12 Budget Request National Weather Service.
George Crawford, Washington Emergency Management Division June 25,2007 UW Educational Outreach – Tsunami Science & Preparedness Program (Su 07) Sponsored.
Tsunami Warning Services for the Pacific Northwest
Aim: What destructive events can be triggered from earthquakes? Japan Earthquake/Tsunami 2011 Japan Earthquake/Fire 2011.
California Tsunami Program Richard Eisner, FAIA, Administrator OES Coastal Region & Tsunami Program.
Diego Arcas NOAA/PMEL University of Washington. Illustration of Deep Water Linearity.
Caribbean Training Course in Seismology and Tsunami Warnings June 25-30, 2007, St. Augustine, Trinidad Tsunami Warning Center Operations: Caribbean Simulations.
IMPACTS OF THE M8.2 EARTHQUAKE OFFSHORE CHILE April 1-2, 2014 Walter Hays, Global Alliance for Disaster Reduction, Vienna, Virginia, USA.
Caribbean Training Course in Seismology and Tsunami Warnings June 25-30, 2007, St. Augustine, Trinidad Sea Level Monitoring for Tsunami Confirmation and.
Earthquake Hazards images from the National Geophysical Data Center Natural Hazards Slide Sets
A Catastrophic Event C. Al-Dahr, M. Karns, S. Martinez, L. Sprague, D. Welling Designing and Producing Educational Technology Course; CMP555 Mark Clauburg;
How can the tsunami danger be reduced? This lesson we’ll see that although it’s impossible to stop earthquakes and tsunamis happening, good preparation.
State of Tsunami Science and Early Warnings Dr. François Schindelé, CEA-DASE Chairman of the International Coordination Group for the Tsunami Warning System.
Today  Hand in any work needed.  Check the list in the back, if you owe something.  Get out a small piece of paper, PUT YOUR NAME ON IT.  When bell.
Measuring and Predicting Natural Disasters
Tsunami-driven Traveling Ionospheric Disturbances (TIDs) From Artru et al., 2005.
© 2014 Pearson Education, Inc. W Waves and Water Dynamics Chapter 8 Tsunami and Wave Energy.
BY K.MOUNIKA CSE 4 TH YEAR. What is a Tsunami? A tsunami is a wave in the ocean or in a lake that is created by a geologic event characterized by a series.
EARTHQUAKE REPORT SOUTH AMERICA WEEK OF FEBRUARY 3 RD TO FEBRUARY 9 TH, 2016 OLIVIA HELPRIN.
EARTHQUAKE AND TSUNAMI. BASIC CONCEPTS: THERMAL EVOLUTION OF OCEANIC LITHOSPHERE Warm mantle material upwells at spreading centers and then cools Because.
Tsunami : Evaluating the Hazard in Southern California.
Aim: What destructive events can be triggered by earthquakes? Japan Earthquake/Tsunami 2011 Japan Earthquake/Fire 2011.
Cabled systems for near-field tsunami early warning: An observation system simulation experiment (OSSE) offshore Portugal A. Babeyko1, M. Nosov2 and.
8.3 Destruction from Earthquakes
Real-Time Tsunami Forecast Animations for SOS
Do Now: In your notes, list some of the similarities and differences between an earthquake’s P and S wave.
Japan’s Earthquake &Tsunami 2011
Session 6 - 7: Major Coastal Hazards (Session 7: Part II)
Tsunami Formation As a tsunami leaves the deep ocean and travels toward the shallow coast, it transforms. A tsunami moves at a speed related to the water.
8.3 Destruction from Earthquakes
Seismic Waves Chapter 15 Section 4.
Aim: What destructive events can be triggered from earthquakes?
Typical Vertical Resolution
Tsunami.
Presentation transcript:

Nancy N. Soreide, D.W. Denbo, Y. Wei, D. Arcas, V.V. 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 … or play from YouTube or local video file YouTubelocal video fileYouTubelocal video file 2

NOAA Center for Tsunami Research 3 Earthquake! Data network Model & data assimilation Tsunami forecast guidance

Courtesy V.K. Gusiakov Earthquake Magnitude Tsunami Intensity 4 The intensity of the earthquake alone does not predict the size of a tsunami … or even if a tsunami will occur.

 DART® tsunami buoys measure the size of a tsunami, in the open ocean, before it comes ashore 5

 Real-time, high resolution buoy data is used to refine the forecast - while the tsunami is still propagating through the ocean. DART® Earthquake 6

 Combines Earthquake seismic information Real-time tsunami buoy measurements in the deep ocean Computer models to predict tsunami propagation and coastal flooding  Provides Real-time tsunami propagation forecasts Real-time coastal flooding forecasts*  Installed at the NOAA Tsunami Warning Centers in Alaska and Hawaii NOAA Center for Tsunami Research 7 * For selected coastal communities

Unit earthquake source locations are co-located with earthquake locations 8 NOAA Center for Tsunami Research

9 Maximum tsunami amplitude with travel time contours overlaid (Chile tsunami February 27, 2010)

NOAA Center for Tsunami Research 10

Flooding and Harbor Currents for Hilo, HI, computed in real time during the event (Chile tsunami February 27, 2010) 11 NOAA Center for Tsunami Research

Located at NOAA PMEL in Seattle, WA 12 Maximum tsunami amplitude Chile tsunami February 27, 2010

13 NOAA Center for Tsunami Research

Chile tsunami event (Feb 27, 2010) Video & Media Player embedded in slide … or play from YouTube or local video file YouTubelocal video fileYouTubelocal video file 14