Variations of Laohugou Glacier No.12 in the western Qilian Mountains, China, from 1957 to 2015

被引:0
|
作者
LIU Yu-shuo [1 ,2 ]
QIN Xiang [1 ,2 ]
CHEN Ji-zu [1 ,2 ]
LI Zhen-lin [3 ]
WANG Jing [3 ]
DU Wen-tao [1 ,2 ]
GUO Wan-qin [1 ]
机构
[1] State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences
[2] Qilian Shan Station of Glaciology and Ecologic Environment, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences
[3] Geomatics Center of Gansu Province,Gansu Bureau of Surveying, Mapping and Geoinformation
关键词
Glacier changes; Laohugou Glacier No.12; Qilian Mountains; Real-time kinematic; Remote sensing image;
D O I
暂无
中图分类号
P343.6 [冰川];
学科分类号
070501 ;
摘要
Glaciers were solid reservoirs and important water resources in western China,but they were retreating significantly in context of global warming.Laohugou Glacier No.12 was the largest valley glacier in Qilian Mountains.In this study,realtime kinematic(RTK)data,topographic map and World View-2 satellite imagery were used to measure changes in terminus,extent and volume of Laohugou Glacier No.12.Results showed that Laohugou Glacier No.12 was shrinking significantly since 1957.From1960 to 2015,the terminus reduction of Laohugou Glacier No.12 was 402.96 m(3.99%)in total,and glacier length decreased to 9.7 km from 10.1 km.Reduction of glacier area and volume were the most obvious.From 1957 to 2015,glacier area and volume decreased by 1.54 km~2(7.03%)and 0.1816 km~3,respectively.Reduction trend of terminus and area was slowing in 1950-1980s,even stable for a period in the mid-1980s,and then accelerated.Ice core analysis result and nearly meteorological station data shown an increasing trend of temperature in 1957-2015,it was a main reason of continuous retreating of Laohugou Glacier No.12.
引用
收藏
页码:25 / 32
页数:8
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