MIPPR 2013: Remote Sensing Image Processing, Geographic Information Systems, and Other Applications 2013
DOI: 10.1117/12.2031083
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A object-oriented glacier mapping method based on multi-temporal Landsat images

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Cited by 2 publications
(3 citation statements)
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“…Optical, Thermal and DEM derived parameters) while working on near homogeneous objects. Therefore, several studies could successfully demonstrate the delineation of debris cover glaciers within in an object-based environment (Rastner et al 2014;Bajracharya, Maharjan, and Shrestha 2014;Bajracharya and Shrestha 2011;Robson et al 2015;Li, Bao, and Huang 2013;Biddle 2015;Jawak, Jadhav, and Luis 2016). (Rastner et al 2014) presented a comparative study of PBIA and OBIA for debris cover classification in three test regions, namely: Coasta Mountains of Canada, Watkin range of Greenland, and Nepal Himalaya.…”
Section: Object-oriented Image Analysismentioning
confidence: 99%
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“…Optical, Thermal and DEM derived parameters) while working on near homogeneous objects. Therefore, several studies could successfully demonstrate the delineation of debris cover glaciers within in an object-based environment (Rastner et al 2014;Bajracharya, Maharjan, and Shrestha 2014;Bajracharya and Shrestha 2011;Robson et al 2015;Li, Bao, and Huang 2013;Biddle 2015;Jawak, Jadhav, and Luis 2016). (Rastner et al 2014) presented a comparative study of PBIA and OBIA for debris cover classification in three test regions, namely: Coasta Mountains of Canada, Watkin range of Greenland, and Nepal Himalaya.…”
Section: Object-oriented Image Analysismentioning
confidence: 99%
“…However, the amount of manual correction required is not known and need further work on this (Robson et al 2015). Another study by Li, Bao, and Huang (2013) delineated full extent of debris cover glacier in the parts of eastern Tienshan Mountain using object image segmentation. This approach is also based on NDSI segmentation and terrain analysis in an object-based environment.…”
Section: Object-oriented Image Analysismentioning
confidence: 99%
“…In the study area, virgin forest is typically found under the elevation value of 3800 m. Mountain rhododendron forest exists in the elevation value above 3800 m. Alpine meadow and brushwood are mainly distributed from 4000 to 4500 m. To determine the elevation value for the tree line or snow line accurately, we carry out two main steps. Surface radiance products of Landsat 5 TM data (Table 2) are employed to derive snow areas and no-snow areas as binary images using an object-oriented glacier mapping method [14]. Seven binary images have been derived.…”
Section: Establishment Of Local Tree Line and Snow Line As A Priori Kmentioning
confidence: 99%