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王 鹏,穆振侠.KM河流域融雪径流与积雪面积-气温关系分析水资源与水工程学报[J].,2013,24(4):28-31,36
KM河流域融雪径流与积雪面积-气温关系分析
Study on relationship of snowmelt runoff with snow area and temperature in KM River basin
投稿时间:2013-03-08  修订日期:2013-04-07
DOI:10.11705/j.issn.1672-643X.2013.04.007
中文关键词:  融雪径流  积雪消融曲线  高程带  MODIS积雪数据
英文关键词:snowmelt runoff  snow ablation curve  elevation zone  MODIS snow data
基金项目:国家自然科学基金(51209181); 水利部公益性行业科研专项经费(201001065); 新疆农业大学校前期课题(XJAU201005); 新疆水文学及水资源重点学科基金(xjswszydxk20101202) [ZK)〗
作者单位
王 鹏 新疆水利水电勘测设计研究院, 新疆 乌鲁木齐 830000 
穆振侠 新疆农业大学 水利与土木工程学院, 新疆 乌鲁木齐 830052 
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中文摘要:
      为更好地探明气候变化下高寒山区积雪的消融规律及其对径流的影响,以及积雪面积、气温、径流之间存在的关系,本文根据2006-2009年的8日合成MODIS积雪产品数据,以及同时期出山口水文站的径流、气温数据,分析了KM河流域的融雪径流特征,定量分析了积雪面积、气温与融雪径流的关系。结果表明:进入3月份,海拔≤2000m积雪已经消融完结;在3月10日前后,海拔2000~3500m积雪开始消融,到融雪期末积雪基本消融完结;在4月初,海拔3500~4500m才开始融雪,到融雪期末积雪没有消融完结;海拔≥4500m积雪面积在融雪期内变化相对比较稳定。流域各高程带积雪面积与气温都呈抛物线关系,且相关性随高程的上升而减弱。
英文摘要:
      In order to better detect the high snow ablation law and its influence on runoff and the climate change , and study the relations between area, temperature and runoff,according to the MODIS snow product data of eight days from 2006to 2009, as well as the runoff and temperature data of hydrologic station at the same period, the paper analyzed the snow-melt runoff characteristics of KM river basin, the quantitative relations of snow area, temperature and snowmelt runoff. The results indicate that ablation of snow ends at 2000m above sea level in March; snow at 2000to 3500m above sea level began melting on March 10,the ablation is completed at the end period of snow ablation;,snow at elevation of 3500to 4500m starts thaw in early April, and has not completed the melt at the thaw end of the period; the change of snow area in snowmelt period is relatively stable at the elevation of equal or larger than 4500m. The area of snow and temperatures in every elevation zone of watershed has parabolic relation ,and the relevance become weak along with the rise of elevation.
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