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MONITORING ICE COVERING LAKE SAROMA BY USING SENTINEL-1 C-BAND SAR DATA

机译:通过使用Sentinel-1 C波段SAR数据监控冰覆盖湖覆盖湖泊

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The objective of this study is to investigate the backscattering characteristics of ice covering Lake Saroma observed by Sentinel-1 C-band SAR data. In-situ observation measuring snow depth and ice thickness was conducted at more than 100 sampling points on Lake Saroma in February 2019. We also tried to apply interferometric SAR data analysis for the data pair acquired during the period from Feb.11 to Mar.7. The C-band SAR backscattering coefficients in both VV and VH have the maximum values at 30 to 35 cm of the ice thickness, and the relatively significant correlation found in the east part of the lake. We also find that the phase difference presumably caused by a tidal change in several areas surrounded the lake. In the relatively thick ice area, the coherence decreases with ice thickness, which is caused by the dominant scattering mechanism change.
机译:本研究的目的是探讨由Sentinel-1 C波段SAR数据观察到的冰覆盖苏马察州的后散射特性。原位观察测量雪深度和冰厚度在2019年2月在苏马州湖的100多个采样点进行。我们还试图为2月11日至3月期间收购的数据对应用干涉测量SAR数据分析。 VV和VH中的C波段SAR背散射系数具有30至35厘米的冰厚度,并且在湖的东部发现的相对显着的相关性。我们还发现,由于湖泊围绕着湖泊的潮气变化导致的相位差。在相对厚的冰面积中,相干性含有冰厚度,这是由显着的散射机制变化引起的。

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