地球科学进展 ›› 2011, Vol. 26 ›› Issue (5): 538 -547. doi: 10.11867/j.issn.1001-8166.2011.05.0538

研究论文 上一篇    下一篇

陆面蒸散量观测方法比较分析及其影响因素研究
张强 1,2,3,张之贤 1,3,问晓梅 1,4,王胜 1,3   
  1. 1.中国气象局兰州干旱气象研究所甘肃省干旱气候变化与减灾重点实验室/中国气象局干旱气候变化与减灾重点开放实验室,甘肃兰州730020;2.甘肃省气象局,甘肃 兰州 730020;3.兰州大学大气科学学院,甘肃兰州730000;4.上海市宝山区气象局,上海201901
  • 收稿日期:2010-06-30 修回日期:2011-03-14 出版日期:2011-05-10
  • 通讯作者: 张强 E-mail:zhangqiang@cma.gov.cn
  • 基金资助:

    国家自然科学基金重点项目“黄土高原陆面过程观测与试验研究”(编号: 40830957);国家公益性行业科研专项“西北地区旱作农业对气候变暖的响应特征及其预警和应对技术研究”(编号:GYHY200806021)资助.

Comparisons of Observational Methods of Land Surface Evapotranspiration and Their  Influence Factors

Zhang Qiang 1,2,3, Zhang Zhixian 1,3, Wen Xiaomei 1,4, Wang Sheng 1,3   

  1. 1. Key laboratory of Arid Climatic Change and Reducing Disaster of Gansu Province/Key Open Laboratory of Arid Climatic Change and Disaster Reduction of CMA/ Institute of Arid Meteorology,CMA,Lanzhou730020,China;
    2. Meteorological Bureau of Gansu Province,Lanzhou 730020,China;3.Lanzhou Univerrsity,Lanzhou730000,China;
    4. Baoshan Meteorological Bureau, Shanghai201901, China
  • Received:2010-06-30 Revised:2011-03-14 Online:2011-05-10 Published:2011-05-10

陆面蒸散是陆面水分平衡的主要分量,也是地球系统水分消耗的主要途径,但陆面蒸散量测量技术一直没有得到很好地解决。利用LOPEX试验区内陇中黄土高原定西陆面过程综合观测站的历史观测资料,在参考对照蒸发皿观测的水面蒸发量的基础上,对蒸渗计法、涡动相关法、彭曼方法等3种方法观测的陆面蒸散量的年变化特征进行了比较分析,发现各观测方法测量的蒸散量差异较大。并且,研究了涡动相关法与蒸渗计法之间、彭曼方法和蒸发皿法之间、彭曼方法与蒸发皿法之间的蒸散观测量的差异特征,揭示了各种微气象要素对陆面蒸散观测的影响规律。

Evapotranspiration process is the principal componet of hydrological budget on land surface and is the main form of earth system′s water consumption.However, the land surface evapotranspiration on the measurement and estimation problem has never been a very good solution. In this paper, by using the historical observation data from DIXI land surface′s comprehensive observation station in LOPEX experimental area,the annual variation and integral total amount of the land surface evapotranspiration of lysimeter, eddy correlation method, Penman method, and evaporation pan observation of four methods  are compared and analyzed to find  that different  observational methods  in measurement of  evapotranspiration have quite different results. The annual variation and seasonal variation of the ratio of eddy correlation method and lysimeter、the ratio of Penman and pan,as well as the ratio of Penman method and lysimeter method are studied. At the same time, the ralation of the ratio of the different methods and local micrometeorological characteristics are discussed.

中图分类号: 

[1]Zhang Qiang, Wang Sheng.Processes of water transfer over land surface in arid and semi-arid region of China[J].Arid Meteorology,2007,25(2): 1-4.[张强,王胜. 关于干旱和半干旱区陆面水分过程的研究[J].干旱气象,2007,25(2): 1-4.]
[2]Zhang Qiang,Hu Yinqiao, Cao Xiaoyan,et al.On some problems of arid climate system of Northwest China[J]. Journal of Desert Research, 2000,20(4):357-362.[张强,胡隐樵,曹晓彦,等.论西北干旱气候的若干问题[J].中国沙漠,2000,20(4):357-362.]
[3]Zhang Qiang,Zhao Yingdong,Zhang Cunjie,et al.ISSUES about hydrological cycle and water resource in arid region of Northwest China[J].Arid Meteorology,2008,2(2):1-8.[张强,赵映东,张存杰,等.西北干旱区水循环与水资源问题[J].干旱气象,2008,26(2):1-8.]
[4]Brutsaert W.Evaporation into the Atmosphere[M].Dordrecht D, Holland: Reidel Publishing Company, 1982:299.
[5]Geiger R.The Climate Near the Ground[M]. Cambridge: Harvard University Press, 1965.
[6]Oke T R. Boundary Layer Climate[M].New York: London Methuen and COLTD, 1978.
[7]Huang Ying,Wang Yu.Analysis on temporal and spatial distribution and interannual change of the evaporation capacity in Yunnan province[J].Hydrology,2003,23(1):38-42.[黄英,王宇. 云南省蒸发量时空分布及年际变化分析[J]. 水文,2003,23(1):38-42.]
[8]Liu Bo,Ma Zhuguo,Ding Yuguo.Characteristics of the changes in pan evaporation over Northern China during the past 45 years and the relations to environment factors[J].Plateau Meteorology,2006,25(5):840-848.[刘波,马柱国,丁裕国.中国北方近45年蒸发变化的特征及与环境的关系[J].高原气象,2006,25(5):840-848.]
[9]Ma Jinling,Zhou Hongfei.Analysis on the variation trends of evaporation from water surface different evaporators in the Northwest Tarim Basin, Xinjiang[J].Arid Land Geography,2005,28(3):300-304.[马金玲,周宏飞.塔里木盆地西北部不同类型蒸发器水面蒸发变化趋势分析[J].干旱区地理,2005,28(3):300-304.]
[10]Qiu Xinfa,Liu Changming.Changes of pan evaporation in the recent 40 years over the Yellow River Basin[J].Journal of Natural Resources,2003,18(4):437-442.[邱新法,刘昌明.黄河流域近40年蒸发皿蒸发量的气候变化特征[J].自然资源学报,2003,18(4):437-442.]
[11]Zuo Hongchao,Li Dongliang,Hu Yinqiao, et al.Trend of recent climate change in China and its 40a pan with the observed changes in the relationship between evaporation[J].Chinese Science Bulletin,2005,50(11):1 125-1 130.[左洪超,李栋梁,胡隐樵,等.近40 a中国气候变化趋势及其同蒸发皿观测的蒸发量变化的关系[J].科学通报,2005,50(11):1 125-1 130.]
[12]Hu Yinqiao, Yang Xuanli, Zhang Qiang,et al.The characters of cnergy budget on the Gobi and desert surface in Hexi  region[J].ACTA Mctcor, Sinica,1992, 6(1):82-91.
[13]Zhang Qiang,Hu Yinqiao,Wang Xihong.The characters of micrometeorology on farmland in oasis in HEIHE region[J].Plateau Meteorology,1992,11(4):361-370.[张强,胡隐樵,王喜红.黑河地区绿洲内农田微气象特征[J].高原气象,1992,11(4):361-370.]
[14]Li Pinfang,Li Baoguo.Study on some characteristics of evaporation of sand dune and evapotranspiration of grassland in Mu Us Desert[J].Journal of Hydraulic Engineering,2000,3:24-28.[李品芳,李保国.毛乌素沙地水分蒸发和草地蒸散特征的比较研究[J].水利学报,2000,3:24-28.]
[15]Ke Xiaoxin,Lin Rinuan,Xu Guochang.Manufacture of the large weighing lysimeter[J].Quarterly Journal of Applied Meteorlolgy,1994,5(2):344-353.[柯晓新,林日暖,徐国昌.大型称重式蒸渗计的研制[J].应用气象学报,1994,5(2):344-353.]
[16]Yang Xingguo,Yang Qiguo,Ke Xiaoxin,et al.Comparison of methods for estimating evapotranspiration in rainfed spring wheat field[J].Journal of Desert Research,2004,24(5):651-656.[杨兴国, 杨启国, 柯晓新,等.旱作春小麦蒸散量测算方法的比较[J].中国沙漠,2004,24(5):651-656.]
[17]Boegh E, Soegaard H, Thomsen A. Evaluating evapotranspiration rate and surface condtions using Landsat TM to estimate atmospheric resistance and surface resistance[J]. Remote Sensing of Environment,2002, 79:329-343.
[18]Ridley J, Strawbridge F, Card R,et al. Radar backscatter characteristics of a desert surface[J].Remote Sensing of Environment,1996, 57(2):63-78.
[19]Zhang Qiang,Wang Sheng.On land surface processes and its experimental study in Chinese Loess Plateau[J].Advances in Earth Science,2008,23(2):167-173.[张强,王胜.关于黄土高原陆面过程及其观测试验研究[J].地球科学进展,2008,23(2):167-173.]
[20]Zhang Qiang,Hu Xiangjun,Wang Sheng,et al.Some technological and scientific issues about the experimental study of land surface processes in Chinese Loess Plateau(LOPEX)[J].Advances in Earth Science,2009,24(4):363-371.[张强,胡向军,王胜,等.黄土高原陆面过程试验研究(LOPEX)有关科学问题[J].地球科学进展,2009,24(4):363-371.]
[21]Yang Xingguo,Zhang Qiang,Wang Runyuan,et al.Experimental study on surface energy balance over Loess Plateau of middle part Gansu in summer[J].Plateau Meteorology,2004,23(6):828-834.[杨兴国,张强,王润元,等.陇中黄土高原夏季地表能量平衡观测研究[J].高原气象,2004,23(6):828-834.]
[22]Li Ju,Liu Yunfen,Yang Xiaoguang,et al.Studies on water vapor flux characteristic and the relationship with environment factors over a planted coniferous forest in Qianyanzhou station[J].Acta Ecologica Sinica,2006,26(8):2 449-2 456.[李菊,刘允芬,杨晓光,等.千烟洲人工林水汽通量特征及其与环境因子的关系[J].生态学报,2006,26(8):2 449-2 456.]
[23]Li Yulin,Cui Jianyuan,Zhang Tonghui.Comparative study on calculation methods of reference evapotranspiration[J].Journal of Desert Research,2002,22(4):372-376.[李玉霖, 崔建垣, 张铜会.参考作物蒸散量计算方法的比较研究[J].中国沙漠,2002,22(4):372-376.]
[24]]Wang Jian,Cai Huanjie,Liu Hongying.The estimation of evaportranspiration with PenmanMonteith and evaporator methods[J].Agricultural Reseach in the Arid Areas,2002,20(4):67-71.[王健,蔡焕杰,刘红英.利用PenmanMonteith 法和蒸发皿法计算农田蒸散量的研究[J].干旱地区农业研究,2002,20(4):67-71.]
[25]Hou Qiong,Wang Yingshun,Yang Zelong,et al.Dynamic simulation and definition of crop coefficient for typical steppe in Inner Mongolia,China[J].Chinese Journal of Plant Ecology,2010,34(12):1 414-1 423.[侯琼,王英舜,杨泽龙,等.内蒙古典型草原作物系数的动态模拟与确定[J].植物生态学报,2010,34(12):1 414-1 423.]
[26]Li Jinhua,Yang Xiaoguang,Cao Shiyu.Water requirement and crop coefficient of different planting patterns in Zhangye area of Gansu province[J].Acta Agriculturae Jiangxi,2009,21(4):17-20.[李金华,杨晓光,曹诗瑜.甘肃张掖地区不同种植模式需水特征及作物系数分析[J].江西农业学报,2009,21(4):17-20.]
[27]Zhan Zhigang,Bian Lingen,Lu Longbi.Parameters of Surface Layer Turbulence and It′s Application for Solving Methods[D].Beijing:Academy of Meteorological Sciences,2004.[湛志刚,卞林根,陆龙弊.近地层大气湍流参数求解方法的比较及其应用[D].北京:气象科学研究院,2004.]
[28]Xu Ziwei,Liu Shaomin,Xu Tongren,et al.Comparison of the gap filling methods of evapotranspiration measured by Eddy Covariance system[J].Advances in Earth Science,2009,29(4):372-382.[徐自为,刘绍民,徐同仁,等.涡动相关仪观测蒸散量的插补方法比较[J].地球科学进展,2009,29(4):372-382.]
[29]Sun Shufen.The Land Surface Processes of Physical, Biochemical Mechanism and Model Parameters[M].BeiJing:Meteorological Press,2005:3-4[孙淑芬.陆面过程的物理、生化机理和参数化模型[M].北京:气象出版社,2005:3-4.]
[30]Monteith J L, Unsworth M H. Principles of Environmental Physics[M].London: Second Arnold,UK,1990.
[31]Meng Xianhong,Lü Shihua,Zhang Yu. MODISbased reversion of atmospheric water vapor content over Jinta Oasis [J].Advances in Water Science, 2007,18(2):264-269.[孟宪红, 吕世华, 张宇.基于MODIS 数据的金塔绿洲上空大气水汽含量反演研究[J].水科学进展,2007,18(2):264-269.]
[32]Zhang Qiang,Wen Xiaomei,Wang Sheng.Semiarid Loess Plateau, the climate conditions of dew formation and characteristics of land surface water balance[J].Acta Meteorologica,2011,in press.[张强,问晓梅,王胜.黄土高原半干旱区露水形成的气候条件及陆面水分平衡特征[J].气象学报,2011,待刊.]
[33]Zhang Qiang,Huang Ronghui.Water vapor exchange between siol and atmosphere over a Gobi surface near an oasis in summer[J].Journal of Applied Meterology,2004,43(12):1 917-1 928.

[1] 贾贞贞,刘绍民,毛德发,王志良,徐自为,张茹. 基于地面观测的遥感监测蒸散量验证方法研究[J]. 地球科学进展, 2010, 25(11): 1248-1260.
[2] 徐自为,刘绍民,徐同仁,王介民. 涡动相关涡动相关仪观测蒸散量的插补方法比较[J]. 地球科学进展, 2009, 24(4): 372-382.
[3] 李 林,张国胜,汪青春,时兴合. 黄河上游流域蒸散量及其影响因子研究[J]. 地球科学进展, 2000, 15(3): 256-259.
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