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Geochemical characterization of supraglacial debris via in situ and optical remote sensing methods: a case study in Khumbu Himalaya, Nepal

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Academic year: 2020

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Figure

Fig. 1. Spectral and spatial resolution of Hyperion, ALI, Landsat ETM+, ASTER and MODIS sensors shown with respect to visible tothermal infrared atmospheric transmission (revised after (K¨a¨ab, 2005)).
Fig. 2. Landsat TM (31 October 2009) true color composite ofthe Khumbu Himalaya study area
Table 2. A listing of the satellite products and scene dates used for the optical remote sensing methods evaluated in this study.
Fig. 3. Khumbu glacier snow, ice and debris field collected surfacereflectance. Note the reduction in VNIR reflectance with increasingdust and debris compared to clean snow and bare ice signatures,and SWIR dominant schistic supraglacial debris signature
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