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Synergistic approach for mapping debris-covered glaciers using optical-thermal remote sensing data with inputs from geomorphometric parameters

机译:利用光学热遥感数据和地貌参数输入,以协同方式绘制覆盖冰川的地图

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摘要

Debris cover on glacier boundaries critically impedes the global inventorying of glaciers and confounds most of the techniques developed for semi-automated mapping of glaciers. Debris on the glacier (referred as supraglacial debris) and that occurring outside the glacier boundaries (referred as periglacial debris) being derived from a common source, i.e. the valley rock, tend to have a similar spectral response in the reflection region which renders them mutually indistinguishable. However, there exist temperature differences between them. This aspect has been considered in this remote sensing based study to distinguish between the supraglacial and periglacial debris in a test area in the Chenab basin, Himalayas, by inclusion of thermal infrared (TIR) bands in remote sensing data processing. A synergistic multisensor approach for the delineation of debris-covered glacier boundaries is used here which integrates the inputs from thermal (TERRA-ASTER sensor) and optical (IRS-P6-AWiFS sensor) remote sensing data, multispectral classification techniques and the DEM derived geomorphometric parameters. The results of this study corroborate earlier findings on utilization of temperature differences as one of the parameters in glacial studies. The proposed synergistic approach therefore appears useful in accurate mapping of debris-covered glaciers in the Himalayan region.
机译:冰川边界上的碎片覆盖严重阻碍了冰川的全球盘存,并且混淆了为半自动绘制冰川而开发的大多数技术。冰川上的碎屑(称为冰川上碎屑)和冰川边界之外发生的碎屑(称为冰缘碎屑)源自共同的来源,即山谷岩石,在反射区域中往往具有相似的光谱响应,从而使它们相互难以区分。但是,它们之间存在温差。通过在遥感数据处理中加入热红外(TIR)波段,在基于遥感的这项研究中已考虑到了这一方面,以区分喜马拉雅山Chenab盆地测试区的冰川带碎屑和冰缘碎屑。这里使用了一种协同多传感器方法来划定覆盖有冰川的冰川边界,该方法整合了来自热(TERRA-ASTER传感器)和光学(IRS-P6-AWiFS传感器)遥感数据,多光谱分类技术和DEM派生的地貌的输入参数。这项研究的结果证实了先前关于利用温差作为冰川研究参数之一的发现。因此,所提出的协同方法似乎对准确绘制喜马拉雅地区被残骸覆盖的冰川很有用。

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