Glacier area shrinkage in eastern Nepal Himalaya since 1992 using high-resolution inventories from aerial photographs and ALOS satellite images

被引:11
作者
Ojha, Sunal [1 ]
Fujita, Koji [1 ]
Asahi, Katsuhiko [2 ]
Sakai, Akiko [1 ]
Lamsal, Damodar [1 ]
Nuimura, Takayuki [3 ]
Nagai, Hiroto [4 ]
机构
[1] Nagoya Univ, Grad Sch Environm Studies, Chikusa Ku, Nagoya, Aichi 4548601, Japan
[2] Shinshu Univ, Inst Mt Sci, Nagano 3994598, Japan
[3] Chiba Inst Sci, Dept Risk & Crisis Management Syst, Choshi, Japan
[4] Japan Aerosp Explorat Agcy JAXA, Tsukuba, Ibaraki, Japan
基金
日本学术振兴会;
关键词
climate change; debris-covered glaciers; glacier delineation; glacier monitoring; remote sensing; MASS-BALANCE; SUMMER-ACCUMULATION; TIBETAN PLATEAU; EVEREST; PRECIPITATION; MOUNTAIN; REGION; BHUTAN; VICINITY; RETREAT;
D O I
10.1017/jog.2016.61
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
To better understand the recent wide-scale changes in glacier coverage, we created and compared two glacier inventories covering eastern Nepal, based on aerial photographs (1992) and high-resolution Advanced Land Observing Satellite (ALOS) imagery (2006-10). The ALOS-derived inventory contained 1034 debris-free and 256 debris-covered glaciers with total and average areas of 440.2 +/- 33.3 and 0.42 km(2) and 1074.4 +/- 206.4 and 4.19 km(2), respectively. We found that the debris-free glaciers have lost 11.2% (0.7 +/- 0.1% a(-1)) of their area since 1992, whereas the number of glaciers increased by 5% because of fragmentation. The area change was significantly correlated by simple linear regression with minimum elevation (r = 0.30), maximum elevation (r = -0.18), altitudinal range (r = -0.50), glacier area (r = -0.62) and mean slope (r = 0.16), confirming that larger glaciers tended to lose a larger area (but a smaller percentage) than smaller glaciers. The infra-regional analysis of the glacier changes clearly showed higher shrinkage rates in the western massifs compared with the eastern massifs. In addition, 61 small glaciers covering an area of 2.4 km(2) have completely disappeared since 1992.
引用
收藏
页码:512 / 524
页数:13
相关论文
共 49 条
[1]   ESTIMATION OF MASS BALANCE COMPONENTS OF A SUMMER-ACCUMULATION TYPE GLACIER IN THE NEPAL HIMALAYA [J].
AGETA, Y ;
HIGUCHI, K .
GEOGRAFISKA ANNALER SERIES A-PHYSICAL GEOGRAPHY, 1984, 66 (03) :249-255
[2]  
[Anonymous], 2011, ASTER GLOBAL DIGITAL
[3]  
[Anonymous], 2010, GLIMS ANAL TUTORIAL
[4]  
[Anonymous], 2003, BULL GLACIOL RES, V20, P29
[5]   The status and decadal change of glaciers in Bhutan from the 1980s to 2010 based on satellite data [J].
Bajracharya, Samjwal Ratna ;
Maharjan, Sudan Bikash ;
Shrestha, Finu .
ANNALS OF GLACIOLOGY, 2014, 55 (66) :159-166
[6]  
Bajracharya SR, 2014, KATHMANDU INT CTR IN, P88
[7]   The influence of debris cover and glacial lakes on the recession of glaciers in Sikkim Himalaya, India [J].
Basnett, Smriti ;
Kulkarni, Anil V. ;
Bolch, Tobias .
JOURNAL OF GLACIOLOGY, 2013, 59 (218) :1035-1046
[8]   Glacier mapping: a review with special reference to the Indian Himalayas [J].
Bhambri, Rakesh ;
Bolch, Tobias .
PROGRESS IN PHYSICAL GEOGRAPHY-EARTH AND ENVIRONMENT, 2009, 33 (05) :672-704
[9]   The State and Fate of Himalayan Glaciers [J].
Bolch, T. ;
Kulkarni, A. ;
Kaab, A. ;
Huggel, C. ;
Paul, F. ;
Cogley, J. G. ;
Frey, H. ;
Kargel, J. S. ;
Fujita, K. ;
Scheel, M. ;
Bajracharya, S. ;
Stoffel, M. .
SCIENCE, 2012, 336 (6079) :310-314
[10]   Multi-decadal mass loss of glaciers in the Everest area (Nepal Himalaya) derived from stereo imagery [J].
Bolch, T. ;
Pieczonka, T. ;
Benn, D. I. .
CRYOSPHERE, 2011, 5 (02) :349-358