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2000年以来的渭河流域实际蒸散发时空格局分析
  • ISSN号:1000-6060
  • 期刊名称:《干旱区地理》
  • 时间:0
  • 分类:P426.2[天文地球—大气科学及气象学]
  • 作者机构:[1]北京师范大学水科学研究院,北京100875, [2]中国科学院地理科学与资源研究所陆地水循环及地表过程重点实验室,北京100101, [3]中国科学院大学,北京100049, [4]中国水利水电科学研究院流域水循环模拟与调控国家重点实验室,北京100038
  • 相关基金:国家自然科学基金项目(41371043,51209224,41271003)
中文摘要:

基于MOD16遥感蒸散发产品,利用降雨径流资料和全球陆面蒸散发估算数据集(MTE)进行精度评价,通过空间建模、趋势分析、标准差法分析了渭河流域2000-2013年实际蒸散发(ET)的年际和年内时空格局变化,探讨了不同土地利用类型下实际蒸散发的差异性变化特征。结果表明:(1)2000-2013年间渭河流域年ET呈缓慢增加趋势,年际波动较大,空间上呈北低南高的趋势,多年平均蒸散发为509.8 mm。(2)年内ET呈单峰型分布,季节性变化明显,主要集中在5~9月份,最高和最低值分别出现在8月和1月;(3)渭河流域ET变化趋势呈减少、基本不变、增加的区域面积分别占14.9%,24.7%和60.4%,年际波动程度整体呈现中度波动。(4)不同土地利用类型ET的分布总体上林地的年ET均值最高,草地、农田和城镇次之,裸地最低。

英文摘要:

Evapotranspiration(ET),the sum of evaporation from soil and transpiration from vegetation,is of vital importance in the hydrologic cycle and governs the water cycle and energy transport among the biosphere,atmosphere and hydrosphere as a controlling factor. Accurately estimating evapotranspiration is related to issues of climate change,water resources management,crop yield estimation,environmental protection,etc. In recent years,with the development of water resources and ecological problems,particularly the urgent requirement of quantitative water management,quantitative research and pattern analysis of evapotranspiration has important practical significance in rid and semi-arid regions. In this paper,based on MOD16 evapotranspiration product,which were first validated with rainfall,runoff data and global land surface evapotranspiration estimates datasets(MTE),the spatio-temporal variation characteristics of actual evapotranspiration(ET)in the Weihe River Basin during 2000-2013 and the differences for evapotranspiration under different land use types were analyzed with the methods of spatial modeling,trend analysis and standard deviation analysis. The results are as follows :(1)The annual ET showed a slow upward trend and large fluctuations during 2000-2013,with the mean annual ET being 509.8mm. The spatial distribution of mean annual ET was generally high over the south of the Weihe River Basin,but low in the north.(2)The monthly ET showed a unimodal pattern with obvious seasonal difference. It is mainly concentrated from May to September,and its peak and bottom value occurred in August and January,respectively.(3)The areas with evapotranspiration trends of decreased,unchanged,increased accounted for 14.9%,24.7% and 60.4%,respectively. The characteristics of stability presented moderate.(4)The overall distribution of ET was related to land use types,with forest land being the highest,followed by grassland,farmland and towns,bare being the lowest. Besides,the change reasons of spati

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期刊信息
  • 《干旱区地理》
  • 北大核心期刊(2011版)
  • 主管单位:中国科学院出版委
  • 主办单位:中国科学院新疆生态与地理研究所 新疆地理学会
  • 主编:陈曦
  • 地址:乌鲁木齐北京南路818号
  • 邮编:830011
  • 邮箱:aridlg@ms.xjb.ac.cn
  • 电话:0991-7885506
  • 国际标准刊号:ISSN:1000-6060
  • 国内统一刊号:ISSN:65-1103/X
  • 邮发代号:58-45
  • 获奖情况:
  • 1994-1996、1997-1999年度科技期刊质量评比优秀期...,1999-2000年度科技期刊质量评比优秀期刊二等奖
  • 国内外数据库收录:
  • 英国农业与生物科学研究中心文摘,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版),中国北大核心期刊(2000版)
  • 被引量:18207