[PDF] Top 20 Application of Mwp to the Great December 26, 2004 Sumatra Earthquake

Application of Mwp to the Great December 26, 2004 Sumatra Earthquake

... A great earthquake of ...northwestern Sumatra (3.30N, 95.96E) at 00:58:53 on De- cember 26, 2004 (UTC) causing an unprecedented tsunami ...(Harvard) earthquake then occurred ... See full document

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Long distance traveling ionospheric disturbances caused by the great Sumatra Andaman earthquake on 26 December 2004

... By using data from the GPS network, we observed exceptional intensive quasi-periodical perturbations of the total electron content (TEC) caused by the great Sumatra-Andaman earthquake on 26 ... See full document

7

Study of Tsunamis by Dimensional Analysis

... Sunday, 26 December 2004, the greatest earthquake in 40 years occurred about 150 kilometers off the west coast of northern Sumatra Island in ...in Sumatra, the Nicobar and An- ... See full document

6

Crustal deformations associated with the great Sumatra Andaman earthquake deduced from continuous GPS observation

... the Sumatra-Andaman earthquake of December 26, ...about 26 cm is found at Phuket in Thailand about 600 km away from the epicenter, about twice as large as that at Sampari, the nearest ... See full document

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Aftershock distribution of the 26 December 2004 Sumatra Andaman earthquake from ocean bottom seismographic observation

... of great importance to observe seismic ac- tivity closely soon after a large earthquake to unveil the ge- ometry and dynamics of the subducting plate in and around the rupture ...In Sumatra Island, ... See full document

7

Transient postseismic mantle relaxation following 2004 Sumatra earthquake: implications of seismic vulnerability in the Andaman-Nicobar region

... the earthquake. We have in- vestigated the possible role of the 26 December 2004 great earthquake and its postseismic deformation in promoting the 10 August 2009 event and its ... See full document

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Differences in tsunami generation between the December 26, 2004 and March 28, 2005 Sumatra earthquakes

... Because earthquake rupture speeds are substantially greater than tsunami phase speeds, coseismic displacement is often assumed to occur instanta- neously for tsunami generation, although for long rupture ... See full document

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Large surface wave of the 2004 Sumatra Andaman earthquake captured by the very long baseline kinematic analysis of 1 Hz GPS data

... The 26 December 2004 Sumatra-Andaman great earthquake had a −1500 km long rupture of more than 600 seconds duration, and may have involved a complex rupture process including ... See full document

5

The Great Tsunami of 26 December 2004: A description based on tide gauge data from the Indian subcontinent and surrounding areas

... An earthquake with a moment magnitude M w = ...Aceh, Sumatra, Indonesia) at 0059 UTC (all times reported in this paper are in UTC, unless otherwise stated) on 26 December 2004 (Bilham, ... See full document

5

Premonitory changes in seismicity prior to the Great Sumatra Andaman earthquake of December 26, 2004

... of less than 2%. We found changes in seismicity consistent with this conclusion using a popular and statistically com- prehensive approach. Jiang and Wu (2005) concluded that a reliable preshock AMR process existed ... See full document

5

Brief communication “Seismic and acoustic-gravity signals from the source of the 2004 Indian Ocean Tsunami”

... The great Sumatra-Andaman earthquake of 26 December 2004 caused seismic waves propagating through the solid Earth, tsunami waves propagating through the ocean and infrasound or ... See full document

8

Feasibility study on the potential of satellite altimetry for detecting seismic geoid changes due to the 2004 Sumatra Andaman earthquake

... an earthquake of magnitude 9 could possibly be detected by satellite altimetry through the change in SSH because such a geoid change would theoreti- cally be expected to reach the order of centimeters (Sun and ... See full document

5

Moment release budget at oblique convergence margin as revealed by the 2004 Sumatra Andaman earthquake

... and Sumatra areas refuse similar interpre- tation. For the Sumatra area, the stress regime indicates vertical or horizontal faults with slip motions incompati- ble with the expected transcurrent movement of ... See full document

9

GPS detection of total electron content variations over Indonesia and Thailand following the 26 December 2004 earthquake

... However, the calculated results shown in Fig. 5 repre- sent that it takes more than 30 min for the acoustic waves to reach the location of 1200 km from the epicenter, while TEC enhancements were observed to start 20 min ... See full document

7

Forearc collapse, plate flexure, and seismicity within the downgoing plate along the Sunda Arc west of Sumatra

... However, offshore Sumatra there are shallow compressional earthquakes within the downgoing oceanic plate outboard of the region of high slip in the 2004 Aceh-Andaman earthquake, occurrin[r] ... See full document

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Seismic dynamo effects associated with the M7 1 earthquake of 26 May 2003 off Miyagi Prefecture and the M6 4 earthquake of 26 July 2003 in northern Miyagi Prefecture, NE Japan

... An earthquake of M7.1 occurred off Miyagi Prefecture, NE Japan, on May 26, 2003 at the depth of about 70 ...July 26, 2003, another shallow earthquake of ...M7.1 earthquake and about 100 ... See full document

6

Changes in groundwater levels or pressures associated with the 2004 earthquake off the west coast of northern Sumatra (M9 0)

... the 2004 earthquake off the west coast of northern Sumatra, changes in groundwater levels or pressures were observed at many observation stations in Japan which are more than 5000 km from the ... See full document

7

Sedimentary deposits of the 26 December 2004 tsunami on the northwest coast of Aceh, Indonesia

... The tsunami here reached ﬂow depths of more than 25 m, and ﬂowed at speeds estimated up to 10 m/s (Kamataki and Nishimura, 2005). The number of waves that struck the area, and how soon after the earthquake the ... See full document

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An improved double difference earthquake location algorithm using s P phases: application to the foreshock and aftershock sequences of the 2004 earthquake offshore of the Kii peninsula, Japan (Mw=7 5)

... Locating earthquakes in offshore regions is problematic due to the uncertainties in the local velocity structure, the lack of near-source recordings, and poor azimuthal cover- age of stations. We included the travel ... See full document

8

Dispersive Study on Tsunami Propagation of The Indian Ocean Tsunami, 26 December 2004

... In order to eliminate the error terms into the same form of dispersive terms in the WNB model equations, fourth-order accuracy of numerical scheme for time stepping and first- order spatial derivatives are used [12]. ... See full document

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