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Discrimination analysis of wet and dry snow covers from RADARSAT SAR data

机译:雷达特SAR数据的湿热雪盖辨析分析

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This paper focuses on the discrimination between wet and dry snow covers from active microwave data. The backscattering coefficients were extracted from two images of the RADARSAT SAR (Synthethic Aperture Radar) sensor acquired in the standard mode S7 (45°- 49°), during the winter and the spring of 1997. The discrimination analysis is performed in both standard modes S1 (20°-27°) and S7 (45°-49°), using simulation results of the wet snow signal. The latter conducted for several wet snow dielectric and structural properties at the air-snow interface are then compared to the measured dry snow signal. Based on a radiative transfer model, the results show the ability of the S1 mode to provide a good discrimination for wet snow surface characterized by rms height ≤ 5 mm and volumetric snow liquid water content > 1. For the S7 mode, optimal discrimination requires rms height ≤ 7 mm and volumetric snow liquid water content ≥ 3. It is also shown that, the difference between the signal of dry and wet snow decreases with wet snow surface roughness, more so over sparse-forested areas.
机译:本文重点介绍了从活性微波数据中潮湿和干雪盖之间的歧视。从标准模式S7(45° - 49°)中获取的雷达特拉SAR(合成孔径雷达)传感器的两个图像中提取了反向散射系数,在标准模式S7(45° - 49°)中,冬季和1997年春天。在两个标准模式下进行辨别分析S1(20°-27°)和S7(45°-49°),使用湿雪信号的仿真结果。然后将用于几个湿雪介质和结构性能的后者与测量的干冰信号进行比较。基于辐射传输模型,结果显示在S1模式,以提供湿雪面,其特征在于均方根高度≤5mm,并且体积雪液体水含量的良好辨别能力> 1.对于S7模式,最佳鉴别需要均方根高度≤7mm和体积雪液含水量≥3。还表明,干燥和湿雪信号之间的差异随着湿的雪表面粗糙度而减少,更为稀疏森林区域。

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