LT-1 SAR Satellite Constellation for Permafrost Deformation Monitoring Along the Tibetan Plateau Engineering Corridor

Xuefei Zhang, Tao Li, Xiang Zhang, Xiaoqing Zhou, Jing Lu, Xueguang Zhang
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引用次数: 0

Abstract

Abstract. The Tibetan Plateau stands as one of China's largest middle and low latitude permafrost regions. However, the effects of global warming and human activities have led to permafrost thawing, inducing surface instability and posing significant threats to infrastructure and indigenous communities. The deployment of Lu Tan-1 (LT-1), China's premier L-band synthetic aperture radar (SAR) satellite constellation, offers a novel opportunity to assess these changes. This paper evaluates the deformation of critical engineering corridors, such as the Qinghai-Tibet Railway (QTR) and the Qinghai-Tibet Highway (QTH), utilizing time-series InSAR techniques with LT-1 SAR constellation data. We introduce both Stacking InSAR and a multi-baseline persistent scatterer multitemporal (MT-InSAR) method to enhance permafrost and engineering corridor deformation detection capabilities. Results obtained through the MT-InSAR approach reveal line-of-sight (LOS) deformation velocities of permafrost in the Beiluhe region ranging from -90 mm/y to approximately 70 mm/y, with an average velocity amplitude of 0.06 m/y. Differential displacement between alpine meadows and alpine deserts across the Beiluhe region is successfully discerned using LT-1 SAR data. Deformation velocities of QTR, QTH were found to be lower than that of permafrost, with average velocities of 0.027 m/y. These findings underscore the LT-1 SAR constellation's potential to serve as a valuable SAR data source for monitoring engineering corridor deformation within the Tibetan Plateau permafrost region.
LT-1 用于青藏高原工程走廊沿线冻土变形监测的合成孔径雷达卫星星座
摘要青藏高原是中国最大的中低纬度冻土区之一。然而,全球变暖和人类活动的影响导致冻土融化,引发地表不稳定,对基础设施和原住民社区构成重大威胁。中国最重要的 L 波段合成孔径雷达 (SAR) 卫星星座 "路探一号"(LT-1)的部署为评估这些变化提供了一个新的机会。本文利用时间序列 InSAR 技术和 LT-1 SAR 星座数据,评估了青藏铁路 (QTR) 和青藏公路 (QTH) 等重要工程走廊的变形情况。我们引入了堆叠 InSAR 和多基线持久散射体多时(MT-InSAR)方法,以提高冻土和工程走廊变形探测能力。通过 MT-InSAR 方法获得的结果显示,北麓河地区永久冻土的视线(LOS)变形速度范围为 -90 毫米/年至约 70 毫米/年,平均速度振幅为 0.06 米/年。利用 LT-1合成孔径雷达数据,成功地分辨出了整个北流河地区高山草甸和高山荒漠之间的位移差异。发现 QTR、QTH 的变形速度低于冻土,平均速度为 0.027 m/y。这些发现突出表明,LT-1合成孔径雷达星座有可能成为监测青藏高原冻土区工程走廊变形的宝贵合成孔径雷达数据源。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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