|
|
F.I. Gonzalez, E.N. Bernard, H.B. Milburn, S. Stalin, V.V. Titov, H.O. Mofjeld, M.C. Eble, J.C. Newman, R.A. Kamphaus, E.F. Burger NOAA / Pacific Marine Environmental Laboratory |
|
|
A deep ocean network, combined with a numerical model database, will improve the speed and accuracy of short-term tsunami forecasting
|
Earthquake!Tsunami? |
Time = 0 |
|
|
Destructive tsunamis originate primarily in subduction zones around the Pacific Rim. |
Not every earthquake generates a tsunami. |
Model simulations combined with real-time tsunami measurements will help assess the hazard. |
|
|
A simulated tsunami generated by a large subduction earthquake (Mw = 8.5) in Alaska-Aleutian Subduction Zone. |
|
|
|
|
Data Network |
|
|
|
Deep-ocean Assesment and Reporting of Tsunamis System |
|
|
|
Quality Control Web Page
|
Surface Buoy and BPR Deployment |
|
Simulated Tsunami and DART Reporting Modes |
|
| |
|
Model & Data Assimilation |
|
|
|
Tsunami Propagation Database Interface |
Output: Time Series
|
Output: Maximum Wave Heights
|
|
Site-Specific Tsunami Inundation Modeling |
| |
|
Tsunami Forecast Guidance |
Time = 1 hour |
Hawaii Civil Defense must decide whether to call a tsunami evacuation within an hour of a Pacific earthquake.
The integrated DART/model database system will provide more rapid and accurate guidance to emergency managers. Schedule:
An operational network of six DART stations will be deployed over the next two years.
The data-assimilation scheme and database for Hawaii are presently under development, to be completed by 2003.
|
|
Tsunami Warning Center |
|
| |
Support provided by NOAA, the U.S. National Tsunami Hazard Mitigation Program and NASA/DoD Solid Earth and Natural Hazards Program
Home | Tsunami Forecasting | Research | DART | Events | Info
| | |
| | |