[1]郝祥云,朱仲元,宋海清,等.锡林河流域积雪时空特征及其对径流的影响[J].水土保持研究,2017,24(06):360-365.
　HAO Xiangyun,ZHU Zhongyuan,SONG Haiqing,et al.Temporal and Spatial Variations of Snow Cover and Its Impact on Runoff in Xilin River Basin[J].Research of Soil and Water Conservation,2017,24(06):360-365.
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锡林河流域积雪时空特征及其对径流的影响

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 24 期数: 2017年06期 页码: 360-365 栏目: 出版日期: 2017-11-24
Title:
Temporal and Spatial Variations of Snow Cover and Its Impact on Runoff in Xilin River Basin
作者:
郝祥云1, 朱仲元1, 宋海清1,2, 席小康1
1. 内蒙古农业大学 水利与土木建筑工程学院, 呼和浩特 010018;
2. 内蒙古自治区生态与农业气象中心, 呼和浩特 010051
Author(s):
HAO Xiangyun1, ZHU Zhongyuan1, SONG Haiqing1,2, XI Xiaokang1
1. College of Hydranlics and Civil Engineering, Inner Mongolia Agricultural, Hohhot 010018, China;
2. Inner Mongolia Autonomous Region Center for Ecology and Agrometeorology, Hohhot 010051, China
关键词:
积雪面积; 时空变化; MOD10A2; 径流
Keywords:
snowfall; spatial-temporal variation; MOD10A2; runoff
分类号:
P343.1
摘要:
寒旱区草原流域地表水资源极为匮乏，融雪径流是寒旱区草原流域重要的水源，冰雪融化对河川径流有着十分显著的影响。利用锡林河流域水文站2000-2013年逐日径流数据、锡林浩特气象站2000-2015年逐日平均气温、降雨、雪深数据及MOD10A2积雪产品数据，分析了锡林河流域积雪面积、雪深年际变化特征，气象因子与积雪面积、雪深之间的相关性，以及径流的影响因素。结果表明：研究区积雪面积、雪深年内变化呈单峰型，冬季积雪面积、雪深均达到最大值，春秋次之，夏季最小。在年际变化上，积雪面积、雪深总体呈现增加趋势，其中冬季的积雪面积呈显著性增加。通过研究区气象因子与积雪的相关性表明，在积雪期，气温、风速和日照时数是影响雪深和积雪面积的主要因素，而在融雪期，气温与降水是影响雪深和积雪面积的主要因素。对径流影响因素的分析可得，气温对径流的影响最大，并且积雪面积、雪深与径流之间也存在很强的相关性，说明积雪的变化也会对径流产生影响。研究积雪动态变化及其对径流的影响对寒旱区草原流域水资源管理、农牧业发展和灾害防御具有重要的现实意义。
Abstract:
The snowmelt runoff is an important water resource in the steppe basin in the cold and arid region. The melting of snow and ice has a significant influence on the runoff. We used daily runoff data from 2000 to 2013 for hydrological stations in the Xilin River Basin, average daily temperature, rainfall, snow depth data in Xilinhot Meteorological Station from 2000 to 2015 and MOD10A2 snow product data, to analyze the characteristics of snow cover and snow depth in the Xilin River Basin, the correlation between meteorological factors and snow cover, snow depth, and the influencing factors of runoff. The results show that the snow cover area and snow depth in the study area are single peaks, in winter, snow cover and snow depth all reached the maximum, followed by spring and autumn and minimum in summer. With respect to the interannual changes, the snow area, snow depth showed an overall increasing trend, in which the snow cover area of winter increased significantly. The correlation between the meteorological factors and snow cover in the study area shows that the main factors affecting the snow depth and snow cover are the temperature, wind speed and sunshine duration during the snow cover, in the snowmelt period, the temperature and precipitation are the main factors affecting snow depth and snow cover. The influence of air temperature on runoff is the most significant, and there is also a strong correlation between snow cover, snow depth and runoff, which indicates that the change of snow cover also affects the runoff. It is of great significance to study the dynamic change of snow cover and its influence on the runoff in the grassland drainage area of the cold and arid region, water resources management, agriculture and animal husbandry development and disaster prevention.

参考文献/References:

[1] 李斐,刘苗苗,王水献.2001-2013年开都河流域上游积雪时空分布特征及其对气象因子的响应[J].资源科学,2016,38(6):1160-1168.
[2] 蔡迪花,郭铌,王兴,等.基于MODIS的祁连山区积雪时空变化特征[J].冰川冻土,2009,31(6):1028-1036.
[3] 李震,施建成.高光谱遥感积雪制图算法及验证[J].测绘学报,2001,30(1):67-73.
[4] 韩庆红,王普才,王玉昆,等.利用MODIS产品分析东北地区积雪覆盖状况及冬季气候特征[J].南京气象学院学报,2007,30(3):396-401.
[5] 万欣,康世昌,李延峰,等.2007-2011年西藏纳木错流域积雪时空变化及其影响因素分析[J].冰川冻土,2013,35(6):1400-1409.
[6] 李倩,李兰海,包安明.开都河流域积雪特征变化及其与径流的关系[J].资源科学,2012,34(1):91-97.
[7] 娄梦筠,刘志红,娄少明,等.2002-2011年新疆积雪时空分布特征研究[J].冰川冻土,2013,35(5):1095-1102.
[8] 希爽,张志富.中国近50a积雪变化时空特征[J].干旱气象,2013,31(3):451-456.
[9] 党素珍,刘昌明,王中根,等.近10年黑河流域上游积雪时空分布特征及变化趋势[J].资源科学,2012,34(8):1574-1581.
[10] 韩兰英,孙兰东,张存杰,等.祁连山东段积雪面积变化及其区域气候响应[J].干旱区资源与环境,2011,25(5):109-112.
[11] 陆智,刘志辉,闫彦.新疆融雪洪水特征分析及防洪措施研究[J].水土保持研究,2007,14(6):256-258.
[12] 李宝富,陈亚宁,陈忠升,等.西北干旱区山区融雪期气候变化对径流量的影响[J].地理学报,2012,67(11):1461-1470.
[13] 段超宇.基于SWAT模型的锡林河流域融雪径流模拟研究[D].呼和浩特:内蒙古农业大学,2014.
[14] 穆振侠,姜卉芳,刘丰.2001-2008年天山西部山区积雪覆盖及NDVI的时空变化特性[J].冰川冻土,2010,32(5):875-882.
[15] 白淑英,史建桥,沈渭寿,等.卫星遥感西藏高原积雪时空变化及影响因子分析[J].遥感技术与应用,2014,29(6):954-962.
[16] 张建同.以Excel和SPSS为工具的管理统计[M].北京:清华大学出版社,2005.
[17] 王鹏,穆振侠. KM河流域融雪径流与积雪面积-气温关系分析[J].水资源与水工程学报,2013,24(4):28-31.
[18] 刘艳,李杨,张璞.玛纳斯河流域融雪径流与积雪-气象因子分析[J].水土保持研究,2010,17(2):145-149.

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备注/Memo

收稿日期:2016-11-18;改回日期:2017-01-02。
基金项目:国家自然科学基金（51669018）；国家自然科学基金（51269014）；内蒙古自治区科技重大计划项目—草原型流域资助项目
作者简介:郝祥云(1992-),女,硕士研究生,主要从事典型草原生态水文研究。E-mail:741331703@qq.com
通讯作者:朱仲元(1956-),男,教授,博士生导师,主要从事水文水资源与天然植被需水方面研究。E-mail:nmgzzy@tom.com

更新日期/Last Update: 1900-01-01