首页> 外文会议>ACRS 2011;Asian conference on remote sensing >THE METHOD STUDY OF ANTARCTIC ICE SHEET SNOWMELT DETECTION FROM MICROWAVE RADIOMETER MEASUREMENTS
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THE METHOD STUDY OF ANTARCTIC ICE SHEET SNOWMELT DETECTION FROM MICROWAVE RADIOMETER MEASUREMENTS

机译:微波辐射计测量南极冰片的方法研究

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The detecting and monitoring of snowmelt is important for studying global changes in polar regions and for hydrological modelling of snowmelt-runoff in high-latitude and mountainous regions. The most of snowmelting detection methods were developed based on in situ measurement, so, the applicable area of the methods are limited and the operational of the methods is not robust. From this problems, two methods which independent of in situ measurements were proposed: the unsupervised XPGR snowmelt detection method based on generanized Gaussian model and the modified snowmelt detection method based on wavelet transformation edge detection. Through cross comprarison of two methods, the result indicate that two mthods were not only increased the computation efficiency, practicability and operability due to independent of in situ measurement, but also improved the ice sheet snowmelt detection accuracy to some extent. The propsed methods provided the methodology support for Antarctic ice sheet snowmelt detection.
机译:对融雪的检测和监测对于研究极地地区的全球变化以及对高纬度和山区融雪径流的水文模拟非常重要。大多数融雪检测方法都是基于原位测量开发的,因此,该方法的适用范围受到限制,并且该方法的操作性不强。针对这一问题,提出了两种独立于原位测量的方法:基于广义高斯模型的无监督XPGR融雪检测方法和基于小波变换边缘检测的改进融雪检测方法。通过两种方法的互比,结果表明,两种方法不仅提高了计算效率,实用性和可操作性,而且不依赖于原位测量,而且在一定程度上提高了冰盖融雪的探测精度。提出的方法为南极冰盖融雪的探测提供了方法学上的支持。

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