干旱区生态环境知识资源中心(Arid): 疏勒河上游径流组分及其变化特征定量模拟

Arid

	疏勒河上游径流组分及其变化特征定量模拟
其他题名	Quantitative simulation of the runoff components and its variation characteristics in the upstream of the Shule River
	李洪源 1; 赵求东 2; 吴锦奎 3; 丁永建 3; 秦甲 2; 韦虹 1; 曾帝 1
来源期刊	冰川冻土
ISSN	1000-0240
出版年	2019
卷号	41 期号:4 页码:907-917
中文摘要	气候变化背景下,西北干旱区内陆河流域的水文过程发生显著变化,制约着地区经济社会和生态建设的稳定发展。定量分析和评估高寒山区径流的变化,有助于加强西北地区水资源的规划管理,实现水资源的可持续利用,保障区域水安全。选取位于青藏高原东北边缘、祁连山西段的疏勒河上游作为研究区,利用包含冰雪消融模块的寒区水文模型分布式SPHY模型(Spatial Processes in Hydrology model)对流域的径流过程进行定量模拟,根据模拟结果分析了疏勒河上游近45 a径流组成及径流与各组分的变化特征。结果表明:(1)率定期日径流和月径流模拟的Nash效率系数分别为0.62和0.86,验证期达到0.79和0.95,模拟的月径流与实测月径流过程基本一致;(2)径流由四部分组成,冰川径流占总径流的年平均比例为30.5%,融雪径流的占比为12.9%,降雨径流的占比为13.5%,基流的占比为43.1%;(3)由于气温升高、降水增多,冰川径流与降雨径流均呈增加的趋势,平均增加幅度分别为4.66 * 10~6 m~3·a~(-1)和2.46 * 10~6 m~3·a~(-1),融雪径流呈减少的趋势,平均减少幅度为1.01 * 10~6 m~3· a~(-1);(4)近45 a年径流增加了69.6%,冰川融水对流域径流增加的贡献率达到48%,非冰川区降水增加的贡献率达到52%。
英文摘要	The hydrological process of inland river basins in the arid area of Northwest China has changed significantly under climate change,which restricts the stable development of regional economic society and ecological construction. Quantitative analysis and evaluation the change of runoff in the alpine area will help to strengthen the planning and management of water resources in the Northwest China,to realize the sustainable utilization of water resources and ensure regional water security. Using a fully distributed,high-resolution cryospheric-hydrological model called SPHY model to simulate runoff process in the upstream of the Shule River,which located in the northeast edge of the Tibetan Plateau and the western of Qilian Mountains. According to the simulation results,the characteristics of runoff composition and the variation of runoff and its components in the upstream of the Shule River were analyzed. Results show that:(1)the Nash-Sutcliffe efficiency coefficients of daily runoff and monthly runoff in calibration period(1971 - 2008)were 0.62 and 0.86,respectively,and in the validation period(2009 - 2015)were 0.79 and 0.95,and the simulated monthly runoff process was in accordance with the measured monthly runoff process. (2)The runoff was composed of four parts,of which the glacier melt runoff and snowmelt runoff accounted for an annual average proportion of 30.5% and 12.9% to the total runoff,and the proportion of rainfall runoff and baseflow was 13.5% and 43.1%,respectively. (3)Due to increasing in temperature and precipitation,both the glacier runoff and rainfall runoff are increasing,with an average increase rate of 4.66 * 10~6 m~3·a~(-1) and 2.46 * 10~6 m~3·a~(-1),respectively. Snowmelt runoff showed a decreasing trend,with an average reduction rate of 1.01 * 10~6 m~3·a~(-1). (4)The annual runoff has increased by 69.6% over the past 45 years,with the contribution rate of glacier meltwater to increase in runoff of 48%,and the contribution rate of precipitation in non-glacierized area of 52%.
中文关键词	SPHY模型 ; 水文过程 ; 径流组分 ; 变化特征 ; 疏勒河上游
英文关键词	SPHY model hydrological process runoff components variation characteristics upstream of the Shule River
语种	中文
收录类别	CSCD
WOS类目	GEOSCIENCES MULTIDISCIPLINARY
WOS研究方向	Geology
CSCD记录号	CSCD:6615640
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/316325
作者单位	1.中国科学院西北生态环境资源研究院;;中国科学院大学, 中国科学院内陆河流域生态水文重点实验室;;, 兰州;;, 甘肃;;北京 730000;;100049, 中国; 2.中国科学院西北生态环境资源研究院;;中国科学院西北生态环境资源研究院, 中国科学院内陆河流域生态水文重点实验室;;冰冻圈科学国家重点实验室, 兰州;;兰州, 甘肃;;甘肃 730000;;730000, 中国; 3.中国科学院西北生态环境资源研究院;;中国科学院西北生态环境资源研究院;;中国科学院大学, 中国科学院内陆河流域生态水文重点实验室;;冰冻圈科学国家重点实验室;;, 兰州;;兰州;;, 甘肃;;甘肃;;北京 730000;;730000;;100049, 中国
推荐引用方式 GB/T 7714	李洪源,赵求东,吴锦奎,等. 疏勒河上游径流组分及其变化特征定量模拟[J],2019,41(4):907-917.
APA	李洪源.,赵求东.,吴锦奎.,丁永建.,秦甲.,...&曾帝.(2019).疏勒河上游径流组分及其变化特征定量模拟.冰川冻土,41(4),907-917.
MLA	李洪源,et al."疏勒河上游径流组分及其变化特征定量模拟".冰川冻土 41.4(2019):907-917.