基于GNIP的黄土高原区大气降水同位素特征研究
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摘要
以GNIP为数据源,选取研究了黄土高原区7个站点(兰州、银川、靖边、西安、平凉、包头、太原)降水中稳定同位素的时空变化特征,分析了除靖边站之外的其他站点降水同位素与温度和降水量的关系,揭示了该地区降水中稳定同位素的变化规律。结果表明:(1)黄土高原大气降水稳定同位素在不同的区域有着相似的时间变化特征和不同的空间变化特征;(2)建立了黄土高原区域大气降水线方程δD=7.0δ18O+0.36‰;(3)黄土高原各站点降水同位素的温度效应和雨量效应表现出较为显著的空间特性;(4)黄土高原区在冬季风期间较夏季风期间风速大、湿度低且蒸发强烈。
Based on the data of GNIP, we investigat ed the temporal and spacial variation characteristics of stable isotope of 7 stations(Lanzhou,Yinchuan,Jingbian,Xi'an,Pingliang,Baotou,Taiyuan)in Loess Plateu,except for Jingbian,and analyzed the correlation between the precipitation isotopic content and temperature,as well as precipitation,so as to reveal the regularity of the stable isotope related. The results show that:(1) the stable isotopes of precipitation in the Loess Plateau has a similar temporal change characteristics in different regions, and different spatial change characteristics;(2) the Local Meteoric Water Line: δD =7.0δ18 O +0.36‰ was established for the Loess Plateau;(3)there are significant spatial characteristics of the temperature and rainfall effect at the stations in the Loess Plateau;(4) there higher wind speed, lower humidity and stronger evaporation in winter than those in summer in the Loess Plateau.
Based on the data of GNIP, we investigat ed the temporal and spacial variation characteristics of stable isotope of 7 stations(Lanzhou,Yinchuan,Jingbian,Xi'an,Pingliang,Baotou,Taiyuan)in Loess Plateu,except for Jingbian,and analyzed the correlation between the precipitation isotopic content and temperature,as well as precipitation,so as to reveal the regularity of the stable isotope related. The results show that:(1) the stable isotopes of precipitation in the Loess Plateau has a similar temporal change characteristics in different regions, and different spatial change characteristics;(2) the Local Meteoric Water Line: δD =7.0δ18 O +0.36‰ was established for the Loess Plateau;(3)there are significant spatial characteristics of the temperature and rainfall effect at the stations in the Loess Plateau;(4) there higher wind speed, lower humidity and stronger evaporation in winter than those in summer in the Loess Plateau.
引文
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[18]张应华,忤彦卿.黑河流域中上游地区降水中氢氧同位素研究[J].冰川冻土,2009,31(1):34-39.(ZHANG Yinghua,WU Yanqing.Oxygen and hydrogen isotopes in precipitation in Heihe River basin,China[J].Journal of Aciology and Geocryology,2009,31(1):34-39.(in Chinese))
[19]杨俊华,秦翔,吴锦奎,等.修正BW方法在中国大气降水δ18O空间分布研究中的应用[J].冰川冻土,2014,36(6):1430-1439.(YANGJunhua,QIN Xiang,WU Jinkui,et al.The application of modified BW method in studying spatial distribution ofδ18O in precipitation China[J].Journal of Glaciology and Geocryology,2014,36(6):1430-1439.(in Chinese))
[20]吴锦奎,杨淇越,丁永建,等.黑河流域大气降水稳定同位素变化及模拟[J].环境科学,2011,32(7):1857-1866.(WU Jinkui,YANGQiyue,DING Yongjian,et al.Variations and simulation of stable isotopes in precipitation in the Heihe River basin[J].Environmental Science,2011,32(7):1857-1866.(in Chinese))
[21]王毅荣,吕世华.黄土高原降水对气候暖响应的敏感性研究[J].冰川冻土,2008,30(1):43-51.(WANG Yirong,LV Shihua.Sensitivity analysis of the response of precipitation to climate change over China Loess Plateau[J].Journal of Glaciology and Geocryology,2008,30(1):43-51.(in Chinese))
[22]李敏蕊,张岩.黄土高原不同时空尺度降水空间变异性研究[D].北京:北京林业大学,2012.6.(LI Minrui,ZHANG Yan.Study on Spatial Variability of Precipitation of Different Spatial and Temporal Scales on Loess Plateau[D].Beijing:Beijing Forestry University,2012.6.(in Chinese))
[23]魏虹,赵松岭,伍光和.黄土高原半干旱区集水农业的气候学初探[J].干旱区资源与环境,1996,10(1):64-70.(WEI Hong,ZHAOSongling.Climatic study on water harvesting agriculture in the semiarid region of loess plateau:a case study on the semiarid region of Gansu loess plateau[J].Journal of Arid Land Resources and Environment,1996,10(1):64-70.(in Chinese))
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