Publikationsdatum:
2023-09-29
Beschreibung:
Monitoring the water level of reservoirs, lakes, and other inland water bodies is essential for hydrology. The lake system is a complex interaction between the atmosphere, surface and groundwater, revealing climatic changes. Many techniques exist to estimate the mass change or water level, and satellite altimetry is one of those techniques to monitor the water level changes of lakes or reservoirs. In recent years, the accuracy of altimetry has improved to centimeter-level, which enables studies on surface water more precisely. The accuracy of altimetry depends on factors such as water body width, radar waveform and the altimeter used. For the same region, the accuracy of altimetry observations can differ depending upon the aforementioned factors. This study has compared altimetry data (Database for Hydrological Time Series of Inland Waters - DAHITI) with the in-situ observations for Gandhi Sagar reservoir. DAHITI database provides the hydrological time series of water bodies using multi-mission satellite altimetry. For this study, 7 years of data (2013-2020) have been taken, consisting of Jason 2/3 and Sentinel 3A, optical and microwave images. In comparison, it is observed that some altimetry observations show significant variation from the in-situ observations. For pre-monsoon and post-monsoon, the coefficient of determination (r squared) is 0.921 and 0.933, respectively, but relatively low (0.873) for monsoon. The role of the surface water area and radar waveform to account for these variations is explored.
Sprache:
Englisch
Materialart:
info:eu-repo/semantics/conferenceObject
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