利用 D-InSAR 跟踪瑞典湖泊厘米级水位变化

S. Aminjafari, I. Brown, F. V. Mayamey, F. Jaramillo
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引用次数: 0

摘要

湖泊是宝贵的水资源,支撑着水生和陆地生态系统,并为全球农业、工业和城市部门提供淡水。虽然应跟踪水位以监测这些服务,但在大多数湖泊中,传统的测量方法并不可行。本研究采用差分干涉合成孔径雷达(D-InSAR)估算瑞典湖泊中每 6 天小于 2 厘米的微小水位变化。我们在瑞典 30 个湖泊的湖岸验证了该方法,并在 2019 年进行了测量观测。我们使用时间间隔为 6 天的哨兵-1A/B 图像来构建连续干涉图,并累积高一致性像素的相位变化来构建水位时间序列。我们发现,通过 D-InSAR 获得的累积相位变化复制了瑞典南部七个湖泊的水位变化幅度。此外,本研究还展示了 D-InSAR 在所有 30 个湖泊中的应用,以估计水位变化的长期方向(即增加或减少)。这项工作揭示了高时间分辨率水位观测在支持其他卫星水位仪器(如传统高度计和最近发射的地表水和海洋地形图任务)方面的效用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Tracking Centimeter‐Scale Water Level Changes in Swedish Lakes Using D‐InSAR
Lakes are valuable water resources that support aquatic and terrestrial ecosystems and supply fresh water for the agricultural, industrial, and urban sectors worldwide. Although water levels should be tracked to monitor these services, conventional gauging is unfeasible in most lakes. This study applies Differential Interferometric Synthetic Aperture Radar (D‐InSAR) to estimate small water level changes, less than 2 cm, in Swedish lakes over 6‐day intervals. We validated the method across the shores of 30 Swedish lakes with gauged observations in 2019. We used Sentinel‐1A/B images with a 6‐day temporal separation to construct consecutive interferograms and accumulated the phase changes in pixels of high coherence to build a time series of water levels. We find that the accumulated phase change obtained by D‐InSAR replicates the magnitude of water levels in seven lakes in Southern Sweden, where water levels change slowly, less than 2 cm per 6‐day period, as validated by in‐situ gauges. In addition, this study demonstrates the application of D‐InSAR to estimate the long‐term direction of water level change (i.e., increase or decrease) in all 30 lakes. This work reveals the utility of high temporal resolution water level observations in support of other satellite water level instruments such as conventional altimeters and the recently launched Surface Water and Ocean Topography Mission.
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