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Equipped with these sea level data and the Bureau of Meteorology's tsunami modeling, specially trained JATWC staff then issue a warning that is in keeping with the determined threat level.

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Marine Geology 239: 99¿123 doi:10.1016/j.margeo.20 Goff, J. When an earthquake occurs, this system automatically computes preliminary information on the earthquake's origin time (time at which the earthquake happened), location, depth and magnitude.Because the total energy within the wave does not change, the energy is transferred to increasing the wave height (or amplitude). A tsunami is often a series of waves and the first may not necessarily have the greatest amplitude.In the open ocean, even the largest tsunami are relatively small, with wave heights typically tens of centimetres or less away from the initial tsunami generation zone.A tsunami is different from a wind-generated surface wave on the ocean.While wind-generated waves in deep water only cause water movement near the surface, the passage of a tsunami involves the movement of water from the surface to the seafloor.Until recently, tsunami were called tidal waves, but this term is generally discouraged because tsunami generation has nothing to do with tides (which are driven by the gravity of the Earth, Moon and Sun).

Although some tsunami may appear like a rapidly rising or falling tide at the coast, in other situations they can also feature one or more turbulent breaking waves.

Higher oceanic wave heights are sometimes observed very close to the tsunami generation zone (e.g., oceanic waves near two metres were measured close to the source of the 2011 Japan tsunami).

In any case, the shoaling effect can greatly increase open ocean wave heights upon reaching the coast, with some tsunami reaching an onshore height more than ten metres above sea level.

The Bureau of Meteorology issues advice and warnings on identified tsunami threat to emergency management agencies and the public using procedures similar to those used for warnings of other severe weather or hazardous events.

Procedures include: As part of the Australian Tsunami Warning System Project (2005-09), the Attorney-General's Department funded Geoscience Australia to develop the national offshore Probabilistic Tsunami Hazard Assessment (PTHA).

More recently, tsunami continue to be recorded in Australia with most presenting little threat to coastal communities.