Tsunami Early Warning System Tsunami A sea wave

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Tsunami Early Warning System

Tsunami Early Warning System

Tsunami A sea wave of local or distant origin that results from large-scale seafloor

Tsunami A sea wave of local or distant origin that results from large-scale seafloor displacements associated with large earthquakes, major submarine slides, or exploding volcanic islands.

Regular Wind Generated Wave Speed: 10 -20 mph 10 Feet 300 Feet

Regular Wind Generated Wave Speed: 10 -20 mph 10 Feet 300 Feet

Tsunami in Deep Ocean Speed: 450 -650 mph 1 -2 Feet 316, 800 Feet

Tsunami in Deep Ocean Speed: 450 -650 mph 1 -2 Feet 316, 800 Feet

Tsunami Approaching Shore Speed: 35 -220 mph 10 -100+ Feet 5, 000 – 10,

Tsunami Approaching Shore Speed: 35 -220 mph 10 -100+ Feet 5, 000 – 10, 000 Feet

Tsunami Cycle Underlying Geological Event Water Displaced Detection Opportunities Tidal Surge Wave Propagation Tidal

Tsunami Cycle Underlying Geological Event Water Displaced Detection Opportunities Tidal Surge Wave Propagation Tidal Withdraw

Detection Phase 1 Geologic Activity Phase 2 Wave Activity Phase 3 Coastline Activity

Detection Phase 1 Geologic Activity Phase 2 Wave Activity Phase 3 Coastline Activity

Current State of the Art Satellite Surface Buoy Hydrophone Acoustic Link 5, 000 M

Current State of the Art Satellite Surface Buoy Hydrophone Acoustic Link 5, 000 M Tsunami Detector Anchor Gonzalez, F. I. (1999): Tsunami!. Scientific American, 280(5), 56 -65

Advantages & Drawbacks • Advantages – Deep water pressure produces relatively low false-positives as

Advantages & Drawbacks • Advantages – Deep water pressure produces relatively low false-positives as winddriven waves do not generate deep pressure differentials – Multiple sensors can triangulate epicenter of water displacement and wave propagation can be predicted. – Good advance warning • Drawbacks – – – Expensive equipment High maintenance Requires multiple communication links: • • Sonar Satellite uplink Satellite downlink Last-mile notification to authorities • Authorities must notify coastal dwellers

Genesis Tsunami Coastal Alert Deep sea pressure Seismic Events Surface anomalies Coastal Alarm &

Genesis Tsunami Coastal Alert Deep sea pressure Seismic Events Surface anomalies Coastal Alarm & Detection

Leading Trough The receding sea that precedes a tsunami • • Near-shore subsidence facilitate

Leading Trough The receding sea that precedes a tsunami • • Near-shore subsidence facilitate tsunami penetration inland Theoretical predictions* and field surveys indicate that coastal run-up and inundation will be greater if the trough of the leading wave precedes the crest * Raissa Mazova of the Nizhny Novgorod State Technical University in Russia and by Costas Synolakis of the University of Southern California

Genesis Tsunami Coastal Alert Flares ignited to signal coastal communities Satellite, RF, audible alarms

Genesis Tsunami Coastal Alert Flares ignited to signal coastal communities Satellite, RF, audible alarms execute responsive to contact with trigger Tsunami trough (receding sea) Tsunami trough threshold level Tension in anchor line pulls buoy into contact with trigger Anchor

Genesis Tsunami Coastal Alert Buoy measures tsunami crest – broadcasts satellite data for emergency

Genesis Tsunami Coastal Alert Buoy measures tsunami crest – broadcasts satellite data for emergency response in other areas.

Advantages to Coastal Alert • Direct warning system in third world and emerging industrial

Advantages to Coastal Alert • Direct warning system in third world and emerging industrial countries – – – Flares Audible siren Local RF broadcast on emergency marine VHF channels and terrestrial radio – Can be activated in advance by RF or satellite transmission if deep sea sensors forecast tsunami hit in the area • Low Cost Design – No expensive off-shore installation and maintenance – Multi-use design – can be used for navigation, temperature readings, etc. • Ideal supplement to sophisticated deep sea monitoring

Genesis Tsunami Offshore Alert Responsive to seismic event GTOA releases non-buoyant pressure sensors at

Genesis Tsunami Offshore Alert Responsive to seismic event GTOA releases non-buoyant pressure sensors at multiple depths below normal wave action.

Genesis Tsunami Offshore Alert Satellite Detachable pressure sensors Pressure changes below predetermined depth are

Genesis Tsunami Offshore Alert Satellite Detachable pressure sensors Pressure changes below predetermined depth are indicators of tsunami activity. Pressure readings are relayed to monitoring station. Multiple readings provide more accurate analysis of deep pressure readings.

Genesis Drop Sensor Telemetry and support line. Pressure transducer supplied by Paroscientific, Inc. –

Genesis Drop Sensor Telemetry and support line. Pressure transducer supplied by Paroscientific, Inc. – Quartz crystal detection of flex of Bourdon tube. Sensor is maintained above waterline before release. No fouling or damage from deep sea mounting. Lead weight is adjusted so that rate of decent is controlled so that multiple sensors reach their operating depth in synchronization.

Genesis Tsunami Offshore Alert • No permanent seabed pressure sensor • Pressure readings at

Genesis Tsunami Offshore Alert • No permanent seabed pressure sensor • Pressure readings at multiple depths • Pressure transducer equipment kept out of hostile environment until deployed • Redundancy if a sensor fails • Lower false positives • No ROV needed for maintenance or deployment

Genesis Tsunami System • Costal detection and notification • Offshore monitoring and early warning

Genesis Tsunami System • Costal detection and notification • Offshore monitoring and early warning • Integrated systems provide prediction, notification and warning in a single package. • Low costs for deployment and maintenance • Superior data capture and uptime

The End Baxter Technologies

The End Baxter Technologies