Journal Article SAR interferometry using ALOS-2 PALSAR-2 data for the Mw 7.8 Gorkha Nepal earthquake

Natsuaki, Ryo  ,  Nagai, Hiroto  ,  Motohka, Takeshi  ,  Ohki, Msato  ,  Watanabe, Manabu  ,  Thapa, Rajesh Bahadur  ,  Tadono, Takeo  ,  Shimada, Masanobu  ,  Suzuki, Shinichi  ,  夏秋, 嶺  ,  永井, 裕人  ,  本岡, 毅  ,  大木, 真人  ,  渡邉, 学  ,  Thapa, Rajesh Bahadur  ,  田殿, 武雄  ,  島田, 政信  ,  鈴木, 新一

682016-02-01 , Springer
The Advanced Land Observing Satellite-2 (ALOS-2, DAICHI-2) has been observing Nepal with the Phased Array type L-band Synthetic Aperture Radar-2 (PALSAR-2) in response to an emergency request from Sentinel Asia related to the Mw 7.8 Gorkha earthquake on April 25, 2015. PALSAR-2 successfully detected not only avalanches and local crustal displacements but also continental-scale deformation. Especially, by the use of the ScanSAR mode, we are able to make interferograms that cover the entire displacement area of the earthquake. However, we did encounter some fundamental problems with the ScanSAR and incorrect settings of PALSAR-2 operation that have now been fixed. They include (1) burst overlap misalignment between two ScanSAR observations, which limits the number of pairs available and the quality of the interferogram, (2) non-crustal fringes which are derived from co-registration error and/or ionospheric effect and, (3) incorrect setting of the center frequency in the Stripmap beam F2-6. In this paper, we describe their problems and solutions. The number of interferometric pairs are limited by (1) and (3). The accuracy of the interferograms are limited by (2) and (3). The experimental results showed that current solutions for (2) and (3) work appropriately.
Physical characteristics: Original contains color illustrations
形態: カラー図版あり

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