[1] Wang Zongtai. Glacier Inventory of China I: Qilian Mountains[M]. Lanzhou: Lanzhou Institute of Glaciology and Geocryology, Academia Sinica, 1981: 1-249.[2] Liu Shiyin, Shen Yongping, Sun Wenxin, et al. Glacier variation since the maximum of the Little Ice Age in the Western Qilian Mountains, Northwest China[J]. Journal of Glaciology and Geocryology, 2002, 24(3): 227-233.[刘时银, 沈永平, 孙文新, 等. 祁连山西段小冰期以来的冰川变化研究[J]. 冰川冻土,2002,24(3): 227-233.][3] Shi Yafeng. Estimation of the water resources affected by climatic warming and glacier shrinkage before 2050 in West China [J]. Journal of Glaciology and Geocryology, 2001, 23(4): 333-341. [施雅风. 2050年前气候变暖冰川萎缩对水资源影响情景预估[J]. 冰川冻土,2001, 23(4): 333-341.][4] Shen Yongping, Liu Shiyin, Zhen Lili,et al. Fluctuations of glacier mass balance in watersheds of Qilian Mountain and their impact on water resources of Hexi region [J].Journal of Glaciology and Geocryology, 2001, 23(3): 244-250. [沈永平, 刘时银, 甄丽丽, 等. 祁连山北坡流域冰川物质平衡波动及其对河西水资源的影响[J]. 冰川冻土, 2001, 23(3): 244-250.][5] Yang Yong, Chen Rensheng, Ji Xibin. Variations of glaciers in the Yeniugou watershed of Heihe River Basin from 1956 to 2003[J]. Journal of Glaciology and Geocryology, 2007, 29(1): 100-106. [阳勇,陈仁升,吉喜斌. 近几十年来黑河野牛沟流域的冰川变化[J]. 冰川冻土, 2007, 29(1): 100-106.][6] Du Wentao, Qin Xiang, Liu Yushuo, et al. Variation of the Laohugou Glacier No.12 in the Qilian Mountains[J]. Journal of Glaciology and Geocryology, 2008, 30(3): 373-379. [杜文涛,秦翔,刘宇硕,等. 1958-2005年祁连山老虎沟12号冰川变化特征研究[J]. 冰川冻土, 2008, 30(3): 373-379.][7] Yang Junhua, Qin Xiang, Wu Jinkui, et al. Distribution and variation of spring snow cover in Laohugou watershed of the Qilian Mountains[J]. Journal of Glaciology and Geocryology, 2012, 34(5): 1091-1098. [杨俊华, 秦翔, 吴锦奎, 等. 祁连山老虎沟流域春季积雪属性的分布及变化特征[J]. 冰川冻土, 2012, 34(5): 1091-1098.][8] Dang Suzhen, Liu Changming, Wang Zhonggen, et al. Analyses on temporal variations of snowmelt runoff time in the upper reaches of Heihe River and its climate causes[J]. Journal of Glaciology and Geocryology, 2012,34(4): 920-926. [党素珍,刘昌明,王中根,等. 黑河流域上游融雪径流时间变化特征及成因分析[J]. 冰川冻土, 2012,34(4): 920-926.][9] Lan Yongchao, Shen Yongping, Gao Qianzhao, et al. Changes of climate and runoff in mountain area of Danghe River Basin under global warming [J]. Journal of Glaciology and Geocryology,2011,33(6): 1259-1267. [蓝永超, 沈永平, 高前兆, 等. 祁连山西段党河山区流域气候变化及其对出山径流的影响与预估[J]. 冰川冻土, 2011,33(6): 1259-1267.][10] Gansu Institute of Geo-Environment Monitoring.Investigation and Research of Groundwater Circulation and Water Quantity Balance in Sugan River Basin. Lanzhou: Gansu Institute of Geo-Environment Monitoring, 2009.[甘肃省地质环境监测院. 苏干湖水系地下水循环与水量平衡调查研究. 兰州: 甘肃省地质环境监测院, 2009.][11] 00926 Department of the PLA. The 1:200 000 Regional Hydrogeological Survey Report of Huahaizi Basin, Qinghai Province. Xining: 00926 Department of the PLA,1977.[中国人民解放军00926部队. 青海省花海子盆地1: 20万区域水文地质普查报告.西宁:中国人民解放军00926部队, 1977.][12] Gansu Provincial Environmental Protection Bureau. Ecological Environment Survey Report of Gansu Province. Lanzhou: Gansu Provincial Environmental Protection Bureau, 2001.[甘肃省环境保护局. 甘肃省生态环境现状调查报告. 兰州: 甘肃省环境保护局, 2001.][13] Zhang Zonghu, Li Lierong, Zhao Cheng, et al. Groundwater Resources Evaluation of Gansu Province [M]. Beijing: SinoMaps Press, 2004.[14] Zhao Cheng, Chen Zhihui. Groundwater Resources Evaluation of Shule River Basin in Hexi Corridor, Gansu Province.Lanzhou: Gansu Institute of Geo-Environment Monitoring, 2001.[赵成, 陈志辉. 甘肃省河西走廊疏勒河流域地下水资源评价. 兰州: 甘肃省地质环境监测院, 2001.] |