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

H. Wakabayashi, H. Tonooka
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Abstract

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.
利用sentinel-1 c波段SAR数据监测冰面湖泊肉瘤
本文研究了Sentinel-1 c波段SAR数据观测的Saroma湖覆冰后向散射特征。2019年2月,在萨罗马湖100多个采样点对雪深和冰厚进行了现场观测。我们还尝试对2月11日至3月7日期间获得的数据对进行干涉SAR数据分析。VV和VH的c波段SAR后向散射系数在冰厚30 ~ 35 cm处最大,且在湖东部相关性较显著。我们还发现,相位差可能是由湖泊周围几个地区的潮汐变化引起的。在较厚的冰区,相干性随冰厚的增加而降低,这是由主要散射机制的变化引起的。
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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