IASPEI - Picture Gallery
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IUGG XXIV General Assembly July 2-13, 2007 Perugia, Italy (S) - IASPEI - International Association of Seismology and Physics of the Earth's Interior JSS002 Poster presentation 1820 Finite Fault Modelling for Tsunamigenic Earthquakes in Australasia using Seismic and Sea Level Data Dr. Phil Cummins Geospatial and Earth Monitoring Division Geoscience Australia IASPEI Toshitaka Baba, Hong Kie Thio, Ming-Hai Jia Since the 2004 Sumatra-Andaman earthquake and Indian Ocean Tsunami, there has been a vast increase in the monitoring of large earthquakes and tsunami-related sea level changes, especially in the Australasian region. The increase in data has resulted in much better coverage of tsunami sources in this region, much of it in real-time. In this presentation we consider how well this increased monitoring allows us to characterise these sources, by performing finite fault inversions using combinations of seismic, sea level and GPS data. While tide gauge data is often limited by its sensitivity to poorly known local bathymetry, there are an increasing number of ocean bottom pressure measurements which record tsunami waveforms unaffected by shallow bathymetry, and we investigate the potential of these for constraining earthquake source properties. Two fundamental questions investigated are: (1) Can earthquake source models be inferred with sufficient accuracy to be used to validate teletsunami modeling (2) Can accurate source models be developed in near-real-time We discuss our results for modelling recent tsunamigenic earthquakes with a view towards answering these questions. Keywords: earthquake, tsunami, modeling
IUGG XXIV General Assembly July 2-13, 2007 Perugia, Italy (S) - IASPEI - International Association of Seismology and Physics of the Earth's Interior JSS002 Poster presentation 1821 Tsunami Risk in the Northern Bay of Bengal Dr. Phil Cummins Geospatial and Earth Monitoring Division Geoscience Australia IASPEI This presentation isa synthesis of the results of geologic and geodetic studies of the northern Bay of Bengal, combined with an analysis of historical accounts of the 1762 Arakan earthquake and a simulation of the tsunami that may have accompanied it. I show that these are all consistent with active subduction in the Myanmar subduction zone, and hypothesize that the seismogenic zone associated with it extends into the Bay of Bengal beneath the Bengal Fan. These results suggest that a very large and vulnerable population is exposed to a high earthquake and tsunami risk. Other reports that have characterised this hazard as low may have not considered the possibility that the seismogenic zone extends offshore, as is suggested by GPS surveys, the active Bengal Fold System, and the historical accounts of subsidence on the coast of Chittagong during the 1762 Arakan earthquake. Although the2004 Indian Ocean Tsunami was difficult to foresee, some of the warning factors were there and should have been recognized by the earth science community. This presentation attempts to draw attention to similar warning factors in the Bay of Bengal, where the cost in human lives of a large earthquake and tsunami may be much larger.
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IUGG XXIV General Assembly July 2-13, 2007 Perugia, Italy<br />
(S) - <strong>IASPEI</strong> - International Association of Seismology and Physics of the Earth's<br />
Interior<br />
JSS002 Poster presentation 1821<br />
Tsunami Risk in the Northern Bay of Bengal<br />
Dr. Phil Cummins<br />
Geospatial and Earth Monitoring Division Geoscience Australia <strong>IASPEI</strong><br />
This presentation isa synthesis of the results of geologic and geodetic studies of the northern Bay of<br />
Bengal, combined with an analysis of historical accounts of the 1762 Arakan earthquake and a<br />
simulation of the tsunami that may have accompanied it. I show that these are all consistent with active<br />
subduction in the Myanmar subduction zone, and hypothesize that the seismogenic zone associated<br />
with it extends into the Bay of Bengal beneath the Bengal Fan. These results suggest that a very large<br />
and vulnerable population is exposed to a high earthquake and tsunami risk. Other reports that have<br />
characterised this hazard as low may have not considered the possibility that the seismogenic zone<br />
extends offshore, as is suggested by GPS surveys, the active Bengal Fold System, and the historical<br />
accounts of subsidence on the coast of Chittagong during the 1762 Arakan earthquake. Although<br />
the2004 Indian Ocean Tsunami was difficult to foresee, some of the warning factors were there and<br />
should have been recognized by the earth science community. This presentation attempts to draw<br />
attention to similar warning factors in the Bay of Bengal, where the cost in human lives of a large<br />
earthquake and tsunami may be much larger.