Articles

Daily Glacier Runoff Estimation Methods—A Case Study of Koxkar Glacier

  • WANG Jian ,
  • LIU Shiyin ,
  • QING Wenwu ,
  • HAN Haidong ,
  • KANG Ersi ,
  • CHEN Rensheng
Expand
  • Cold and Arid Regions Environmental and Engineering Research Institute, CAS, Lanzhou 730000, China

Received date: 2008-04-11

  Revised date: 2008-06-25

  Online published: 2008-09-10

Abstract

Using hydrometeorological data from June 1, 2005 to May 31, 2006 obtained by several automatic stations of Koxkar Glacier (total drainage area is 117.6km2 among which 83.6km2 is covered glacier), and combining it with 1:50 000 topographic map, TM, FY-2C and NCEP/NCAR data, the authors have created total 10 different distributed runoff models with 60m×60m spatial resolution and 1d time-step. All the models simulate the daily mean runoff well, and they are better than the statistical models. Using FY-2C total cloud cover data and solar radiation parameterized methods could calculate the solar radiation well in China, and it may use global radiation to estimate glacier runoff in some period well. In a year, the relationship between air temperature and glacier runoff is exponential, while in the ablation season, it is linear. That is, the degree-day method is more suitable in the ablation season. In such large glacier basin (glacier coverage is about 71%) as Koxkar watershed, the precipitation measurements neglected in the past in China is very important. With direct or global radiation being added, the temperature-index ice melting model will simulate the glacier runoff better. The authors also for the first time have given 3 simple energy-balanced models in China to estimate the glacier runoff, and the models all estimate the daily mean runoff well. In the Koxkar glacier watershed, improvment should be made for the research on evapotranspiration, sublimation, coagulation and refreezing, especially the runoff concentration processes which are very complex due to its melting Kast in the glacier. Many instruments were installed on the glacier in July, 2007, such as the eddy covariance system, a 10m meteorological tower and two automatic stations, etc. In the next few years, more glacier runoff estimation methods in different glacier with different character and size need to be found.

Cite this article

WANG Jian , LIU Shiyin , QING Wenwu , HAN Haidong , KANG Ersi , CHEN Rensheng . Daily Glacier Runoff Estimation Methods—A Case Study of Koxkar Glacier[J]. Advances in Earth Science, 2008 , 23(9) : 942 -951 . DOI: 10.11867/j.issn.1001-8166.2008.09.0942

References

[1] Shi Yafeng,Liu Chaohai,Wang Zongtai,et al. Short Glacier Inventory of China[M]. Shanghai: Shanghai Popular Science Press,2005.[施雅风,刘潮海,王宗太,. 简明中国冰川编目[M]. 上海: 上海科学普及出版社,2005.]

[2] Yang Zhenniang. Glacier Water Resources in China[M]. Lanzhou: Gansu Science and Technology Publishing House,1991.[杨针娘. 中国冰川水资源[M]. 兰州: 甘肃科学技术出版社,1991.]

[3] Liu Shiyin,Ding Yongjian,Zhang Yong,et al. Impact of the glacial change on water resources in the Tarim river basin[J]. Acta Geographica Sinica,2006,615):482-490.[刘时银,丁永建,张勇,. 塔里木河流域冰川变化及其对水资源影响[J]. 地理学报,2006,615):482-490.]

[4] Liu Shiyin,Ding Yongjian,Li Jing,et al. Glaciers in response to recent climate warming in western China[J]. Quaternary Sciences,2006,265):762-771.[刘时银,丁永建,李晶,. 中国西部冰川对近期气候变暖的响应[J]. 第四纪研究,2006,265):762-771.]

[5] Xie Zichu,Wang Xin,Kang Ersi,et al. Glacial runoff in China: An evaluation and prediction for the future 50 years[J]. Journal of Glaciology and Geocryology,2006,284):457-466.[谢自楚,王欣,康尔泗,.中国冰川径流的评估及其未来50年变化趋势预测[J]. 冰川冻土,2006,284):457-466.]

[6] Qing Wenwu,Chen Rensheng,Liu Shiyin. Research progress in glacier hydrological model[J]. Advances in Water Science,2008inprinted.[卿文武,陈仁升,刘时银.冰川水文模型研究进展[J]. 水科学进展,2008:19(待刊).]

[7] Zhang Yong,Liu Shiyin. Progress of the application of degree-day model to study glaciers and snow cover[J]. Journal of Glaciology and Geocryology,2006,281):101-107. [张勇,刘时银. 度日因子模型在冰川与积雪研究中的应用进展[J]. 冰川冻土,2006,281):101-107.]

[8] Shi Yafeng,Yao Tandong,Huang Maohuan,et al. Glaciers and Their Environments in China—The Present,Past and Future[M]. Beijing: Science Press,2000. [施雅风,姚檀栋,黄茂桓,. 中国冰川与环境——现在、过去和未来[M]. 北京: 科学出版社,2000.]

[9] Su Zhen,Song Guoping,Wang Lilun. Modern glaciers in Mt. Tuomuer[C]Glacial and Meteorology in Mt. Tuomuer District,Tianshan. Urümqi: Xinjiang People’s Publishing House,1985.[苏珍,宋国平,王立伦. 托木尔峰地区的现代冰川[C]天山托木尔峰地区的冰川与气象.乌鲁木齐:新疆人民出版社,1985.]

[10] Xie Changwei,Ding Yongjian,Liu Shiyin,et al. Variation of Keqikaer glacier terminus in Tomur peak during last 30 years[J]. Journal of Glaciology and Geocryology,2006,285):672-677.[谢昌卫,丁永建,刘时银,. 30年来托木尔峰南麓科其喀尔冰川冰舌区变化[J]. 冰川冻土,2006,285):672-677.]

[11] NOAA-CIRES Climate Diagnostic Center. NCEP/NCAR Reanalysis 1[M]. Boulder Colorado: NOAA-CIRES Climate Diagnostic Center,2004.

[12] National Satellite Meteorological Center. China Satellite Data Service CenterCSDSC[Z]. http://satellite.cma.gov.cn/,2008.[国家卫星气象中心.中国卫星遥感数据服务网[Z]. http://satellite.cma.gov.cn/,2008.]

[13] Chen Rensheng,Lü Shihua,Kang Ersi,et al. An hourly solar radiation model under actual weather and terrain conditions: A case study in Heihe river basin[J]. Energy,2007,32:1 148-1 157.

[14] Chen Rensheng,Lu Shihua,Kang Ersi,et al. A distributed water-heat coupled model for mountainous watershed of an inland river basin in Northwest ChinaI model structure and equations[J]. Environmental Geology,2007,53:1 299-1 309.

[15] Chen Rensheng,Gao Yanhong,Kang Ersi,et al. A distributed water-heat coupled model for mountainous watershed of an inland river basin in northwest Chinausing the outputs from Mesoscale model version 5[J]. Environmental Geology, 2007,53:763-768.

[16] Kang E S,Cheng G D,Lan Y C,et al. A model for simulating the response of runoff from the mountainous watershed of inland river basins in the arid area of northwest China to climatic changes[J]. Science in China Series D,1999,42suppl.:52-63.

[17] Hock R. A distribute temperature-index ice-and snowmelt model including potential direct solar radiation[J]. Journal of Hydrology,1999,45149:101-111.

[18] Munro D S. Comparison of melt energy computations and ablatometer measurements on melting ice and snow[J]. Arctic and Alpine Research,1990,222:153-162.

[19] Zhang Yinsheng,Yao Tandong,Pu Jianchen. The response of continental-type glaciers to climate change in China[J]. Journal of Glaciology and Geocryology,1998,201:3-8.[张寅生,姚檀栋,蒲建辰. 我国大陆型山地冰川对气候变化的响应[J]. 冰川冻土,1998,201:3-8.]

[20] Yang Zhenniang,Zeng Qunzhu. Glacier Hydrology[M]. Chongqing: Chongqing Press,2001. [杨针娘,曾群柱. 冰川水文学[M].重庆:重庆出版社,2001.]

[21] Kang Ersi. A parameterized energy balance model of glacier melting on the Tianshan mountain[J]. Acta Geographica Sinica,1994,495:467-476.[康尔泗.天山冰川消融参数化能量平衡模型[J]. 地理学报,1994,495:467-476.]

[22] Wang Jian,Ding Yongjian,Xu Junli,et al. Hydrochemical characteristic analysis of melting water flow in Keqikaer glacier, TianshanWest mountains[J]. Environmental Science,2006,267:1 305-1 311.[王建,丁永建,许君利,.西天山科其喀尔冰川消融径流的水化学分析[J]. 环境科学,2006,267:1 305-1 311.]

Outlines

/