The change of Ningchan River Glacier No. 3 at Lenglongling, east Qilian Mountain, China  

作　　者：YuShuo Liu Xiang Qin Tong Zhang MingJie Zhang WenTao Du 

机构地区：[1]Qilian Shan Station of Glaciology and Ecologic Environment, State Key Laboratory of Cryospheric Science, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences [2]College of Earth and Environmental Science, Lanzhou University [3]State Key Laboratory of Cryospheric Science, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences

出　　处：《Research in Cold and Arid Regions》2013年第6期709-714,共6页寒旱区科学（英文版）

基　　金：supported by the State Natural Science Fund projects(41071046 and 41201067);the project from the State Key Laboratory of Cryospheric Sciences(SKLCS-ZZ-2012-01-05);the Project for Incubation of Specialists in Glaciology and Geocryology of Nation-al Natural Science Foundation of China(J0930003/J0109)

摘　　要：In July, 2009, we investigated the Ningchan River Glacier No. 3. A control network was established around the glacier and the expedition used a GPS-RTK to measure glacial area, terminal and surface altitude, and used an EKKO GPR to measure glacier thickness. We used a topographic map based on 1972 aerial photo, two TM images in 1995, 2009, and GPS-RTK data in 2009, to analyze the change of the Ningchan River Glacier No. 3 since 1972. Through analysis we found this glacier has been seriously shrinking over the past 37 years. The glacier terminal retreated about 6%, the area was reduced about 13.1%, the volume was reduced about 35.3%, and glacier shrinkage is mainly in the form of thinning. Glacier average thickness reduced from 36.8 m in 1972, to 27.4 m in 2009. Meteorological data around the study area shows that this region in recent decades has undergone differential warming which is the main reason for rapid glacier shrinkage.In July, 2009, we investigated the Ningchan River Glacier No. 3. A control network was established around the glacier and the expedition used a GPS-RTK to measure glacial area, terminal and surface altitude, and used an EKKO GPR to measure glacier thickness. We used a topographic map based on 1972 aerial photo, two TM images in 1995, 2009, and GPS-RTK data in 2009, to analyze the change of the Ningchan River Glacier No. 3 since 1972. Through analysis we found this glacier has been seriously shrinking over the past 37 years. The glacier terminal retreated about 6%, the area was reduced about 13.1%, the volume was reduced about 35.3%, and glacier shrinkage is mainly in the form of thinning. Glacier average thickness reduced from 36.8 m in 1972, to 27.4 m in 2009. Meteorological data around the study area shows that this region in recent decades has undergone differential warming which is the main reason for rapid glacier shrinkage.

关 键 词：Ningchan River Glacier No. 3 Qilian Mountains glacier changes glacier shrink 

分 类 号：P343.6[天文地球—水文科学]