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| 青冰滩冰川水文特征初步分析 | |
| 引用本文： | 魏召才,刘志辉,金爽.青冰滩冰川水文特征初步分析[J].新疆环境保护,2010,32(1):7-9. |
| 作者姓名： | 魏召才 刘志辉 金爽 |
| 作者单位： | 1. 新疆大学资源与环境科学学院,乌鲁木齐,830046;绿洲生态教育部重点实验室 2. 新疆大学资源与环境科学学院,乌鲁木齐,830046;绿洲生态教育部重点实验室;干旱半干旱区可持续发展国际研究中心 3. 西北师范大学地理与环境科学学院,兰州,730070 |
| 基金项目： | 中国沙漠气象科学研究基金 |
| 摘 要： | 通过对青冰滩冰川的综合考察,对该地区2008-08-01日至08-31日的水文、气象以及水环境进行了连续观测。结果表明:冰川表面大量覆盖冰碛增加了冰川表面的反射率,加速了冰川消融;整个8月日均气温在8℃以下,气温的日较差较大,冰川消融期的降水以降雪和冰雹为主;冰川融水的电导率和溶解性固体相关系数可达0.98,两者与气温的相关度也可达到0.8以上。 |
| 关 键 词： | 青冰滩冰川 冰川融水 电导率 溶解性总固体 |
Preliminary Analysis about Hydrologic Characteristics of Qingbingtan Glacier |
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| WEI Zhao-cai,LIU Zhi-hui,JIN Shuang.Preliminary Analysis about Hydrologic Characteristics of Qingbingtan Glacier[J].Environmental Protection of Xinjiang,2010,32(1):7-9. | |
| Authors: | WEI Zhao-cai LIU Zhi-hui JIN Shuang |
| Institution: | 1. College of Resources and Environment Science, Xinjiang University, Urumqi 830046; 2. Key Laboratory of Oasis Ecology and Desert Environment, Xinjiang University , Urumq 830011 ;3. International Cen- ter for Sustainable Development in Arid and Semiarid Areas, Urumqi 830046;4. College of Geography and Environmental Sciences, Northwest Normal University, Lanzhou 730070, China). |
| Abstract: | Based on the general investigation to Qingbingtan glacier, continuous observation including hydrology, weather and water environment of the research area were implemented from Aug. 1 2008 to Aug. 31 2008. The results indicate that large amount moraines on the glacier surface increase the albedo and enhance the speed of glacier melt. The average temperature in August is bellow 8 ~C and daily temperatures change greatly. Snow and hail are the main perception types during the period of glacier melt. The correlation coefficient between conductivity and total dissolved solids is 0.98, and the two factors both have the high correlation coefficient - up to 0.8, with the average temperature. |
| Keywords: | Qingbingtan glacier glacier melt water conductivity total dissolved solids |
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