Two dimensional temperature measurements by X-Y scanning of Er end doped silica fiber sensor

Author(s):  
Kentaro Morita ◽  
Asuka Okabe ◽  
Sakiko Ito ◽  
Hiroaki Aizawa ◽  
Tooru Katsumata ◽  
...  
2008 ◽  
Vol 62 (7) ◽  
pp. 778-783 ◽  
Author(s):  
Johan Zetterberg ◽  
Zhongshan Li ◽  
Mikael Afzelius ◽  
M. Aldén

1992 ◽  
Vol 17 (24) ◽  
pp. 1821
Author(s):  
Anbo Wang ◽  
George Z. Wang ◽  
Kent A. Murphy ◽  
Richard O. Claus

1974 ◽  
Vol 13 (68) ◽  
pp. 243-254 ◽  
Author(s):  
Gary T. Jarvis ◽  
Garry K. C. Clarke

Ice temperature measurements have been made in Steele Glacier to a depth of 114 m. All measured temperatures were below 0° C, the coldest being –6.5° C at a depth of 114 m. The temperature profile indicates an anomalously warm layer of ice between 30 m and 50 m, which is probably due to the freezing of water in crevasses opened during the 1965–66 surge. A two-dimensional model of a cold glacier with partially water-filled crevasses predicts temperature profiles very similar to that observed.


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