The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
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Articles | Volume XLVI-4/W3-2021
Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., XLVI-4/W3-2021, 155–160, 2022
https://doi.org/10.5194/isprs-archives-XLVI-4-W3-2021-155-2022
Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., XLVI-4/W3-2021, 155–160, 2022
https://doi.org/10.5194/isprs-archives-XLVI-4-W3-2021-155-2022
 
10 Jan 2022
10 Jan 2022

PERFORMANCE OF SITE VELOCITY PREDICTION IN SUNDALAND

A. H. Kamaludin1, W. A. Wan Aris1, T. A. Musa1, A. H. Omar1, and A. Z. Sha’ameri2 A. H. Kamaludin et al.
  • 1Geomatic Innovation Research Group, Faculty of Built Environment and Surveying, Universiti Teknologi Malaysia
  • 2School of Electrical Engineering, Faculty of Engineering, Universiti Teknologi Malaysia

Keywords: Site Velocity, Plate Motion, Least Square Collocation, Crustal Deformation, Tectonic Geodesy

Abstract. Global Positioning System (GPS) technique has been extensively implemented in determination of crustal deformation globally. With the ability of providing solution up to milimeter (mm) level, this technique has proven to provide a precise estimate of site velocity that represents the actual motion of tectonic plate over a period. Therefore, this study aims to evaluate the site velocity estimation from GPS-derived daily position of station, respective to the global plate motion model and predicted site velocity via Least-Squares Collocation (LSC) method within the tectonically active region of Sundaland. The findings have indicated that stations with precise velocity estimates were consistent with global plate model and predicted velocity, with velocity residuals of 5 mm – 10 mm. However, stations that were severely impacted by continuous earthquake events such as in Sumatra were believed to be induced by the impact with consistently large velocity residuals up to 37 mm. Following the outcomes, this study has provided an insight on the post-seismic decay period plate motion which are induced by continuous tectonic activities respective to modelled plate motion.