Full text: Technical Commission VIII (B8)

       
   
      
   
  
  
   
  
  
  
  
   
  
   
   
    
  
  
   
   
    
   
  
   
  
   
  
   
   
   
   
     
   
   
  
    
  
  
   
  
   
     
   
   
  
     
ons of 
'ehavior 
1e years 
6km? 
153km 
2 
17km? 
to retreat 
masses 
1 data 
lifficult, 
pulated 
ological 
lues of 
outhern 
climate 
of the 
at there 
e in the 
36 until 
agonian 
ckly to 
y are 
that is, 
blation, 
. affects 
at these 
»laciers' 
f them. 
lysis of 
ed more 
detailed studies in order to we be able 
to conclude that these variations in the body of 
the glaciers are really caused by global 
warming. However, it appears that the recent 
rapid recession is a response to the recent 
world-wide warming trend. 
4. ACKNOWLEDGEMENTS 
The authors are grateful to United States 
Geological Survey (USGS) and National 
Institute for Space Research (INPE) by images. 
5. REFERENCES 
ANIYA, M., 1988. Glacier inventory for the 
Northern Patagonia Icefield, Chile, and variations 
1944/45 to 1985/86. Arctic and Alpine Research, 
20: 179-187. 
ANIYA (1) M. and SKVARCA, P., 1992. 
Characteristics and variations of Upsala and 
Moreno glaciers, southern Patagonia, Bulletin of 
Glacier Research, 10:39-53. 
ANIYA (2), M., NARUSE, R., SHIZUKUISHI, 
M., SKVARCA, P. and CASASSA, G., 1992. 
Monitoring recent glacier variations in the 
Southern Patagonia Icefield, utilizing remote 
sensing data, International Archives of 
Photogrammetry and Remote Sensing, 29(B7):87- 
94. 
ANIYA, M., SATO, H. NARUSE R, 
SKVARCA, P. and CASASSA, G., 1996. The use 
of satellite and airbone imagery to inventory 
outlet glaciers of the Southern Patagonia Icefield, 
South America. Photogrammetric Engineering 
and Remote Sensing, 62, pag. 1361-1369. 
CASASSA, G., 1992. Radio-echo sounding of 
Tyndall Glacier, southern Patagonia. Bulletin of 
Glacier Research, 10: 69-74. 
CHANDER, G., MARKHAM, B., 2003. Revised 
Landsat-5 TM Radiometric — Calibration 
Procedures and Post calibration Dynamic Ranges, 
IEEE Transactions on Geoscience and Remote 
Sensing, Vol. 41, N° 11. 
IWATA, S., 1983. Further advance of Pio XI 
Glacier. In Glaciological and Meteorological 
Studies in Patagonia, Chile, by Japanese 
Research Expeditions in 1967-1982 (Data Center 
for Glacier Researches, Japanese Society of Snow 
and Ice), 14- 17. 
KRIMMEL, R. M., 1988. Terminus of Glacier 
O'Higgins, southern Chile. Journal of Glaciology, 
34 (116): 142. 
LEMKE, P., et al. 2007., Observations: Changes 
in snow, ice and frozen ground, in Climate 
Change 2007: The Physical Science Basis. 
Contribution of Working Group I to the Fourth 
Assessment Report of the Intergovernmental 
Panel on Climate Change, edited by S. Solomon 
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York. 
RAYMOND, C., NEUMANN, I., RIGNOT, E., 
ECHELMEYER, K., RIVERA A. and CASASSA 
G., 2005. Retreat of Tyndall glacier, Patagonia, 
over the last half century. Journal of Glaciology. 
ROOT, H, STUEFER M, SIEGEL. A, 
SKVARCA P. and ECKSTALLER A, 1998. 
Mass fluxes and dynamics of Moreno Glacier, 
Southern Patagonia  Icefield. ^ Geophysical 
Research Letters, 25 (9), 1407-1410. 
RIVERA, A. and Casassa G., 1999. Volume 
changes of Pío XI glacier: 1975-1995. Global and 
Planetary Change, 22(1-4), 233. 
SKVARCA, P., SATOW, K., NARUSE, R. and 
LEIVA, J., 1995. Recent thinning, retreat and 
flow of Upsala Glacier, Patagonia, Bulletin of 
Glacier Research, 13:11-20. 
STUEFER, M., 1999.. Investigations on mass 
balance and dynamics of Moreno Glacier based 
on field measurements and satellite Imagery. PhD 
dissertation, Leopold-Franzens-Univesitat, 
Innsbruck, p. 173. 
WARREN, C.R. and SUGDEN, D.E., 1993. The 
Patagonian Icefields: A glaciological review, 
Arctic and Alpine Research, 25(4]:316-331.
	        
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