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1971-2010年三江源地区干湿状况变化的空间特征

Spatial pattern and its variations of aridity/humidity during 1971-2010 in Three-River Source Region on the Qinghai-Tibet Plateau

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【作者】 徐维新古松苏文将江莎校瑞香肖建设张娟

【Author】 XU Wei-xin1,2,GU Song3,1,SU Wen-jiang2,JIANG Sha3,XIAO Rui-xiang2, XIAO Jianshe2,ZHANG Juan2(1 Northwest Institute of Plateau Biology,Chinese Academy of Sciences,Xining 810001,Qinghai,China; 2 Meteorological Institute of Qinghai Province,Xining 810001,Qinghai,China;3 Nankai University,College of Life Sciences,Tianjin 300071,China)

【机构】 中科院西北高原生物研究所青海省气象科学研究所南开大学生命科学学院

【摘要】 依据1971-2010年地面观测气象数据,计算了三江源地区湿润指数。利用经验正交函数分解(EOF)和偏相关系数,对近40 a三江源地区干湿状况变化的时空特征及其影响因素进行了分析。结果表明:三江源地区干湿状况的变化在其北部与南部、东部与西部间存在明显反相位变化特征。北部和东部的部分区域分别在20世纪90年代和21世纪后表现出气候湿润化趋势,其余大部地区的持续干旱化趋势始于20世纪80年代初,其中南部与西部变干趋势显著,其湿润指数线性趋势率达到-8%/10 a。虽然三江源地区干湿状况主要决定于降水量和相对湿度的变化,但20世纪90年代中期后气温的显著上升,使得气温也成为关键的影响因子之一,即使在降水明显增加的背景下,也引起三江源主体区域湿润指数的明显下降。气候变暖情景下,北部和东部地区在近十几年暖湿化趋势明显,其余大部地区表现为不同程度的暖干化趋势。

【Abstract】 The Three-River Source Region(TRSR),the source region of Yangtze River,Yellow River and Mekong River,is located in the hinterland of the Qinghai-Tibetan Plateau.With a typical continental plateau climate and alpine vegetation ecosystem,the water and heat matching is a key to vegetation variation over region.In this study,monthly humidity indexes in TRSR were computed using ground-observed monthly air temperature,precipitation,wind speed,relative humidity and air pressure from 1971-2010,based on the method of Ecological and Meteorological Monitoring Standard which recommended by China Meteorological Bureau.The spatio-temporal variation of aridity/humidity conditions and its dominated factor were analyzed using the method of Empirical Orthogonal Function(EOF),linear correlation and partial correlation analysis.The results show a clear of opposite mode in the zone of northern toward southern and western toward eastern in TRSR.It was found that there is a wet tendency after 1990s and 21st century in the zone of northern and eastern respectively,but a continual dry tendency since 1980s,especially in the zone of southern and western with a remarkable decreased trend(-8%/10a),occurred in other area of TRSR.Aridity/humidity conditions are controlled by precipitation and relative humidity in generally,but the situation is changed evidently after Mid-1990s in the most area of TRSR due to a significant warming,and temperature plays a key of factor to dominate a decreased trend of humidity index even if precipitation increases markedly since then.Under a scenarios of climate warming,it shows a tendency of heat and wet obviously in the zone of northern and eastern and heat and aridity in a certain extent in most area of TRSR.

【基金】 国家自然科学基金项目(41061002);高原气象开放基金项目(LPM20090005);干旱气象基金项目(IAM200812)
  • 【文献出处】 干旱区地理 ,Arid Land Geography , 编辑部邮箱 ,2012年01期
  • 【分类号】P467
  • 【被引频次】51
  • 【下载频次】808
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