Full text: Technical Commission VII (B7)

    
  
  
   
   
   
   
   
  
   
  
  
  
  
  
   
   
  
   
  
  
  
   
   
  
   
   
   
   
  
  
  
  
  
  
  
  
  
  
   
  
  
  
  
  
  
   
   
   
    
International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XXXIX-B7, 2012 
XXII ISPRS Congress, 25 August — 01 September 2012, Melbourne, Australia 
lidated by Lu, Z, Dzurisin, D., Jung, H. S., et al., 2010. Radar image and 
| proposed data fusion for natural hazards characterisation. International 
Journal of Image and Data Fusion, 1: 3, pp. 217 -242. 
ial change Lu, A., Yao, T., Liu, S., et al., 2002. Glacier Change in the 
River from Geladandong area of the Tibetal Plateau monitored by remote 
esand two sensing. Journal of Glaciology and Geocryology, 24 (5), pp. 
rate during 559-562. 
1 fast, with 
Richardson, S. D., Reynolds, J. M., 2000. An overview of 
glacial hazards in the Himalaya. Quaternary International, 
65/66, pp. 31-47. 
Su, Z., Liu, Z., Wang, W., et al., 1999. Glacier Response to the 
Climatic Change and its Trend Forecast in the Qinghai-Tibetan 
Plateau. Advance in Earth Sciences, 14(6), pp. 607- 612. 
Wang, Z., Liu, C., 2001. Geographical Characteristics of the 
Distribution ofGlaciers in China. Journal of Glaciology and 
Geocryology, 23(3), pp. 231-237. 
Zhou, J, Li, Z, Xing, Q., 2010. Deriving Glacier Border 
Information Based on Analysis of Decorrelation in SAR 
Interferometry. Journal of Glaciology and Geocryology, 32(1), 
pp. 133-138. 
  
ata: (a) 
543); (b) 
ACKNOWLEDGEMENTS 
This research is supported by the National High Technology 
Research and Development Program, China, under project 
um. number 2011AA120402 and funds from CASM (No. 7771203 
nics in east and No. K201001). ERS SAR and ENVISAT ASAR data are 
y, 41(139), copyrighted and provided by European Space Agency (ESA). 
Landsat TM image is provided by the U.S. Geological Survey. 
monitoring 
Annals of 
3. Textural 
on Systems 
al. Climate 
f Working 
Jniv. Press, 
al, 2005. 
Land Ice 
n, 99, pp. 
coherence 
ence and 
1e Glacier 
olarimetric 
oc. Inter. 
.504-1506 
of Glacier 
ta. Remote 
 
	        
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