3D Surface velocity retrieval of mountain glacier using an offset tracking technique applied to ascending and descending SAR constellation data: a case study of the Yiga Glacier. Issue 6 (3rd June 2019)

• Record Type: Journal Article
• Authors: Wang, Qun; Fan, Jinghui; Zhou, Wei; Tong, Liqiang; Guo, Zhaocheng; Liu, Guang; Yuan, Weilin; Sousa, Joaquim João; Perski, Zbigniew
• Is Part Of: International journal of digital earth. Volume 12:Issue 6(2019)
• Page Start: 614
• Page End: 624
• Publication Date: 2019-06-03
• Subjects: Mountain glacier -- inversion of 3D movement -- offset tracking -- SAR constellation data; Geographic information systems -- Periodicals; Sustainable development -- Information technology -- Periodicals; Social planning -- Information technology -- Periodicals; 910.285
• DOI: 10.1080/17538947.2018.1470690
• Languages: English
• ISSNs: 1753-8947

Abstract

ABSTRACT: COSMO-SkyMed is a constellation of four X-band high-resolution radar satellites with a minimum revisit period of 12 hours. These satellites can obtain ascending and descending synthetic aperture radar (SAR) images with very similar periods for use in the three-dimensional (3D) inversion of glacier velocities. In this paper, based on ascending and descending COSMO-SkyMed data acquired at nearly the same time, the surface velocity of the Yiga Glacier, located in the Jiali County, Tibet, China, is estimated in four directions using an offset tracking technique during the periods of 16 January to 3 February 2017 and 1 February to 19 February 2017. Through the geometrical relationships between the measurements and the SAR images, the least square method is used to retrieve the 3D components of the glacier surface velocity in the eastward, northward and upward directions. The results show that applying the offset tracking technique to COSMO-SkyMed images can be used to derive the true 3D velocity of a glacier's surface. During the two periods, the Yiga Glacier had a stable velocity, and the maximum surface velocity, 2.4 m/d, was observed in the middle portion of the glacier, which corresponds to the location of the steepest slope.