Glacier shrinkage in the Daxue and Danghenan ranges of the western Qilian Mountains, China, from 1957 to 2010

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• 作者：Puyu Wang ; Zhongqin Li ; Guobin Yu ; Huilin Li ; Wenbin Wang…
• 关键词：Fractal analysis ; Glacier change ; Regional differences ; Western Qilian Mountains
• 刊名：Environmental Earth Sciences
• 出版年：2016
• 出版时间：January 2016
• 年：2016
• 卷：75
• 期：2
• 全文大小：1,271 KB
• 参考文献：Bahr DB, Meier MF, Peckham SD (1997) The physical basis of glacier volume-area scaling. J Geophys Res 43:557–562
  Bahr DB, Dyurgerov M, Meier MF (2009) Sea-level rise from glaciers and ice caps: a lower bound. Geophys Res Lett 36:L03501CrossRef
  Cao B, Pan BT, Gao HS et al (2010) Glacier variation in the Lenglongling range of eastern Qilian Mountains from 1972 to 2007. J Glaciol Geocryol 32(2):242–246
  Chai HX, Cheng WM, Zhou CH et al (2013) Climate effects on an inland alpine lake in Xinjiang, China over the past 40 years. J Arid Land 5(2):188–198CrossRef
  Chen J, Ohmura A (1990) Estimation of alpine glacier water resources and their change since the 1870’s. IAHS Publ 193:127–135
  Chen YN, Yang Q, Luo Y et al (2012) Ponder on the issues of water in the arid region of northwest China. Arid Land Geogr 35(1):1–8
  Cui Y, Yuan YJ, Jin HL et al (2007) Reconstruction and analysis of 467 year spring precipitation series in the Urumqi River Head. Arid Land Geogr 30(4):496–500
  Ding HW, Wei YG, Li AJ et al (2001) The change characteristics and the trend prediction of streamflow at the debouchure of Shulehe River. Arid Zone Research 18(3):48–53
  Dong S, Xu JH, Chen YN et al (2009) Fractal characteristics of annual mean temperature of the Tarim Basin. Arid Land Geogr 32(1):17–22
  Fan YT, Chen YN, Li WH et al (2011) Impacts of temperature and precipitation on runoff in the Tarim River during the past 50 years. J Arid Land 3(3):220–230CrossRef
  Gao WY, Li ZQ, Li KM et al (2011) Glacier variation in the Kukesu River basin during 1963–2004 based on remote sensing data and GIS techniques. Arid Land Geogr 34(2):252–258
  Hall DK, Bayr KJ, Schfner W et al (2003) Consideration of the errors inherent in mapping historical glacier positions in Austria from ground and space (1893–2001). Remote Sens Environ 86:566–577CrossRef
  Investigation Team of the Ice/Snow Utilization of Chinese Academy of Science (1959) Report of the investigation of modern glaciers in the Qilian Mrs. No. 1. Science Press, Beijing. pp 290–291
  Jia WX, He YQ, Li ZX et al (2008) The regional difference and catastrophe of climate change in Qilian Mt. Region. Acta Geogr Sin 63(3):257–269
  Li DL, Wei L, Cai Y et al (2003) The present facts and the future tendency of the climate change in Northwest China. J Glaciol Geocryol 25(2):135–142
  Li ZQ et al (2011) Progress and application of research on glacier No. 1 at headwaters of Urumqi River, Tianshan, China. Meteorological Press, Beijing
  Liu SY, Shen YP, Sun WX et al (2002) Glacier variation since the maximum of the little ice age in the western Qilian Mountains Northwest China. J Glaciol Geocryol 24(3):227–233
  Liu SY, Sun WX, Shen YP et al (2003) Glacier changes since the little ice age maximum in the west Qiliang Shan, northwest China, and consequences of glacier runoff for water supply. J Glaciol 49:117–124CrossRef
  Liu Y, Li XL, Hu AY et al (2007) Response of runoff to precipitation changes: a case of Weihe. Arid Land Geogr 30(1):49–52
  Lu AX, Yao TD, Liu SY et al (2002) Glacier change in the Geladandong area of the Tibetan Plateau monitored by remote sensing. J Glaciol Geocryol 24(5):559–562
  Macheret YY, Cherkasov PA, Bobrova LI (1988) The thickness and volume of Dzhungarskiy Alatau glaciers from airborne radio echosounding data. Mater Glyatsiol Issled 62:59–70
  Mandelbrot B (1977) Fractals. Form, chance, and dimension. Freeman and Co., San Francisco
  Mandelbrot B (1982) The fractal geometry of nature. Freeman and Co., San Francisco
  Paul F, Kääb A, Maisch M et al (2002) The new remote sensing derived Swiss glacier inventory: I. Methods. Annu Glaciol 34:355–361CrossRef
  Raup B, Racoviteanu A, Jodha S et al (2007) The GLIMS geospatial glacier database: a new tool for studying glacier change. Global Planet Chang 56(1–2):101–110CrossRef
  Shen YP, Liu SY, Zhen LL et al (2001) Fluctuations of glacier mass balance in watersheds of Qilian Mountain and their impact on water resources of Hexi region. J Glaciol Geocryol 23(3):244–250
  Shi YF (2000) Glacier and environment in China: present, past and future. Science Press, Beijing
  Shi YF, Shen YP, Hu RJ (2002) Preliminary study on signal, impact and foreground of climatic shift from warm-dry to warmhumid in Northwest China. J Glaciol Geocryol 24(3):219–226
  Silverio W, Jaquet JM (2005) Glacial cover mapping (1987–1996) of the Cordillera Blanca (Peru) using satellite imagery. Remote Sens Environ 95(3):342–350CrossRef
  Wang ZC (2010) The changes of Lop Nur Lake and the disappearance of Loulan. J Arid Land 2(4):295–303
  Wang ZT, Liu CH, Pu JC et al (1981) Glacier inventory (I): Qilian Mountains. Lanzhou Institute of Glaciology and Cryopedology, Chinese Academy of science, Lanzhou
  Wang YT, Hou SG, Lu AX (2008) Response of glacier variations in the eastern Tianshan Mountains to climate change, during the last 40 years. Arid Land Geogr 31(6):813–819
  Wang PY, Li ZQ, Cao M et al (2011a) Ice surface elevation changes of glacier No. 4 of Sigong River in Bogda, Tianshan Mountains, during the last 50 years. Arid Land Geogr 34(3):464–469
  Wang PY, Li ZQ, Gao WY et al (2011b) Glacier changes in the Heihe River Basin over the past 50 years in the context of climate change. Resour Sci 33(3):399–407
  Xie ZC, Wu GH, Wang LL (1985) Memoirs of Lanzhou Institute of Glaciology and Geocryology, Chinese Academy of Science, No. 5. Science Press, Beijing. pp 82–90
  Yang ZN, Zeng QZ (2001) Glacier hydrology. Chongqing Press, Chongqing, pp 1–40
  Yang Y, Chen RS, Ji XB (2007) Variations of glaciers in the Yeniugou watershed of Heihe River Basin from 1956 to 2003. J Glaciol Geocryol 29(1):100–106
  Zhang HW, Lu AX, Wang LH et al (2011) Glacier change in the Shulenan Mountain monitored remote sensing. J Glaciol Geocryol 33(1):8–11
  
• 作者单位：Puyu Wang (1) (2)
  Zhongqin Li (1) (2) (3)
  Guobin Yu (4)
  Huilin Li (1) (2)
  Wenbin Wang (1)
  Baojuan Huai (1)
  Ping Zhou (1)
  Shuang Jin (1)
  Lin Wang (1)
  Hui Zhang (1)
  
  1. State Key Laboratory of Cryospheric Sciences/Tianshan Glaciological Station, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, 730000, China
  2. RWTH Aachen University, 52056, Aachen, Germany
  3. College of Geography and Environment Science, Northwest Normal University, Lanzhou, 730070, China
  4. Gansu Fundamental Geographic Information Center, Lanzhou, 730000, China
  
• 刊物类别：Earth and Environmental Science
• 刊物主题：None Assigned
• 出版者：Springer Berlin Heidelberg
• ISSN：1866-6299

文摘

Changes in glaciers in the Daxue and Danghenan ranges were analyzed based on topographic maps, satellite images and a digital elevation model (DEM). The results indicate that from 1957/1966 to 2010, the total area and ice volume for the investigated glaciers declined by 17.21 and 24.10 % in these respective ranges. From 1957 to 2010, the total area and ice volume in the glaciers in the Daxue Range declined by 16.03 % (0.30 % a−1) and 22.40 %, respectively, with a mean reduction of 0.133 km2 for an individual glacier. These glaciers retreated by an average of 258 m (3.4 m a−1). From 1966 to 2010, the total area and ice volume for the glaciers in the Danghenan Range declined by 18.32 % (0.42 % a−1) and 25.70 %, with a mean reduction of 0.111 km2 for an individual glacier. These glaciers retreated by an average of 159 m (3.6 m a−1). The rate of glacier retreat on the south-facing slopes was faster than that on the north-facing slopes. The area of glaciers on the south and north slopes of the Daxue Range declined by 22.82 and 15.51 %, respectively, and the area of glaciers on the south and north slopes of the Danghenan Range declined by 22.39 and 16.76 %, respectively. An analysis of the general trend of climatic change in the study area revealed that rapidly rising air temperatures were most likely the major factor causing the loss of glacier ice within the study area. Compared with other glaciers in the eastern and middle Qilian Mountains, glaciers in the western Qilian Mountains appeared to be losing mass at a slower rate. The differences of glacier changes in the eastern, middle, and western Qilian Mountains are mainly caused by the combination of climatic conditions and glacier morphologic factors. Keywords Fractal analysis Glacier change Regional differences Western Qilian Mountains