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首页> 外文期刊>Selected Topics in Applied Earth Observations and Remote Sensing, IEEE Journal of >Dry and Wet Snow Cover Mapping in Mountain Areas Using SAR and Optical Remote Sensing Data
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Dry and Wet Snow Cover Mapping in Mountain Areas Using SAR and Optical Remote Sensing Data

机译:利用SAR和光学遥感数据绘制山区干湿雪覆盖图

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Snow cover in mountain areas is a key factor controlling regional energy balances, hydrological cycle, and water utilization. Optical remote sensing data offer an effective means of mapping snow cover, although their application is limited by solar illumination conditions, conversely, synthetic aperture radar (SAR) offers the ability to measure snow wetness changes in all weather. In this study, a novel method, which can be approached in two steps by using SAR and optical data, has been developed for dry and wet snow cover recognition in mountain areas. First, two ground-based synchronous observations were implemented, respectively, for snow-accumulation period and snow-melt period. Then, the RADARSAT-2 interferometric coherence images and the backscattering coefficient images of the two periods are analyzed, adopting snow-covered and snow-free areas obtained from GF-1 satellite observations as the “ground truth.” A dynamic thresholding algorithm was proposed to identify snow cover by taking the polarization mode, local incidence angle, and underlying surface type into consideration. Finally, 36 polarimetric parameters obtained from Pauli, H/A/α, Freeman, and Yamaguchi decomposition were analyzed; the results indicate that P vol from Pauli, λ3 from H/A/α, and Y vol from Yamaguchi are more applicable to discriminate dry and wet snow. These three factors, combined with training samples from Nagler algorithm and in situ data, were used to build a support vector machine to classify the extracted snow cover to dry and wet snow. The classification results demonstrate that the dry and wet snow cover extraction can achieve an accuracy of 90.3% compared with in situ measurements.
机译:山区的积雪是控制区域能源平衡,水文循环和水资源利用的关键因素。尽管光学遥感数据的应用受到太阳光照条件的限制,但光学遥感数据提供了一种有效的方法来绘制积雪图,相反,合成孔径雷达(SAR)可以测量所有天气中的积雪湿度变化。在这项研究中,已开发出一种新方法,该方法可通过使用SAR和光学数据分两步进行,以识别山区的干湿积雪。首先,分别对积雪期和融雪期进行了两个地面同步观测。然后,使用从GF-1卫星观测获得的积雪和无雪区域作为“地面真相”,分析了两个时期的RADARSAT-2干涉相干图像和后向散射系数图像。提出了一种动态阈值算法,通过考虑极化模式,局部入射角和下垫面类型来识别积雪。最后,分析了从Pauli,H / A /α,Freeman和Yamaguchi分解获得的36个极化参数。结果表明,Pauli的P vol,H / A /α的λ3和Yamaguchi的Y vol更适用于区分干雪和湿雪。这三个因素与来自Nagler算法的训练样本和原位数据相结合,用于构建支持向量机,将提取的积雪分类为干雪和湿雪。分类结果表明,与原位测量相比,干法和湿法积雪提取的精度可达到90.3%。

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