The NOAA Tsunami Program is a federal and state partnership dedicated to saving lives and protecting property before, during, and after tsunami impact through applied research, detection, forecasts, archive, mitigation, and international coordination. Updated Tsunami Evacuation Zones: Directors’ Guideline for CDEM Groups No Tsunami Threat to NZ from Vanuatu 6.9 Earthquake National Conference speakers announced and new workshop National Conference Programme and Workshop information CDEM Award winners announced Funding boost to improve NZ’s resilience to natural hazards

Atlantic Ocean Tsunamis: Rare but Possible. NOAA Tsunami Program. A tsunami in the Atlantic Ocean is a rare event. BC's coastal communities are divided into five tsunami notification zones.

Tsunami modelling has been completed for our region for the most likely and highest impact scenario, which is a 9.0 magnitude Cascadia Subduction Zone earthquake. A new detailed tsunami evacuation map shows Coastal Otago residents what properties may need to be evacuated in such an event. Produced collectively by tsunami modelers, geologic hazard mapping specialists, and emergency planning scientists from CGS, Cal OES, and the Tsunami Research Center at the University of Southern California, the tsunami inundation maps for California cover most residentially and transient populated areas along the state’s coastline.

Also, due to its size, a meteor impact is more likely in the Pacific than in other oceans. Tsunami Evacuation Map The NSW State Emergency Service (NSW SES) has released new maps showing evacuation areas in the event of a land-threat tsunami.

The main tsunami threat to Victoria is from a Cascadia Subduction Zone earthquake off the Pacific Coast of Vancouver Island.

British Columbia's Tsunami Notification Zones. Part of the reason for this low incidence of tsunamis is the lack of subduction zones - the most common source of tsunami-causing earthquakes.. 70-80% of tsunamis occur in the Pacific ocean due to the active subduction zones and their associated volcanic arcs (the "ring of fire"). Each zone includes all islands and inlets within it. The maps show one of Dunedin's lowest-lying areas, South Dunedin, would only need to be evacuated in the face of a more than 3m tsunami, on top of a high tide.

Within several minutes of the earthquake, the initial tsunami (Panel 1) is split into a tsunami that travels out to the deep ocean (distant tsunami) and another tsunami that travels towards the nearby coast (local tsunami). The height above mean sea level of the two oppositely traveling tsunamis is approximately half that of the original tsunami (Panel 1).

While the likelihood of a land-threat tsunami on the east coast of Australia is low, the maps show the areas where residents and workers would have to move to higher ground in the event of a land-threat tsunami.

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