The 2004 Sumatra-Andaman earthquake generated remarkable uplift and subsidence at different locations in the Andaman and Nicobar Islands. Previous studies revealed that a southeast tilting phenomenon, i. e., northwest uplift and southeast subsidence, occurred around the Andaman Islands. At more than a dozen points, the amount of subsidence was measured using GPS, but unfortunately there were few GPS sites in the uplifted areas, and it was almost impossible to conduct ground surveys or use photogrammetry owing to the strict control enforced by the Indian government on access to these locations.
The purposes of this study were to determine the amount of coseismic uplift associated with the earthquake at the northwesternmost part of North Andaman Island, Indian Ocean, and to discuss why the largest coseismic uplift occurred there, considering the submarine topography and free-air gravity anomaly in the area. Reef Island, located off the northwesternmost part of North Andaman Island, was chosen as the study area for lack of coseismic movement data.
Around the northwestern part of North Andaman Island, including Reef Island, the amount of uplift seemed to have decreased within several months after the earthquake due to postseismic creep. In this paper, the displacement on Reef Island was measured using satellite imagery obtained immediately after the earthquake. To measure the amount of uplift, first a digital surface model (DSM) was generated using IKONOS and QuickBird single images. Next, the shoreline change, as determined by comparing the preearthquake with the postearthquake images, was interpreted using GIS as a change in the ground height.
As a result, it was found that Reef Island was uplifted by 2.2m shortly after the earthquake. With this method, the standard deviation was 0.8m; however, it is clear that the amount of uplift on Reef Island was not less than 2m, as evidenced by the exposed coral reef margin in the satellite imagery.
Reef Island is the closest to the Sunda Trench. From free-air gravity anomaly data, the northwesternmost part of North Andaman Island is characterized as a high-anomaly area, in comparison with the surroundings. Therefore these tectonic characteristics are expected to be related to the fact that the largest uplift occurred there.
With the use of the high-resolution satellite imagery to measure ground level changes, it was possible to perform a geomorphologic analysis of the region, where the interferometric synthetic aperture radar technique was not applicable due to its theoretical limitations, e. g., its inability to capture large deformations in the ground surface. In the near future, with the increasing accuracy of satellite data, research on the application of satellite data to geomorphology may lead to the development of a much broader range of potential applications.
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