Hargreaves公式在塔克拉玛干沙漠腹地的适用性

王永东1; 李生宇1; 徐新文1; 雷加强1; 金小军1; 2; 3; 王 强3; 邸 鲲3; 张忠良3

doi:10.7522/j.issn.1000-694X.2013.00051

中国沙漠 >

2013 , Vol. 33 >Issue 2: 367 - 373

DOI: https://doi.org/10.7522/j.issn.1000-694X.2013.00051

生物与土壤

Hargreaves公式在塔克拉玛干沙漠腹地的适用性

王永东1 ,
李生宇1 ,
徐新文1 ,
雷加强1 ,
金小军1 ,
2 ,
3 ,
王强3 ,
邸鲲3 ,
张忠良3

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1.中国科学院新疆生态与地理研究所, 新疆乌鲁木齐 830011;
2.中国科学院研究生院, 北京 100049; 3.中国石油天然气股份有限公司塔里木油田公司, 新疆库尔勒 841000

收稿日期: 2012-01-31

修回日期: 2012-02-28

网络出版日期: 2012-02-28

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Applicability of the Hargraeves Method in Estimating Reference Evapotranspiration in the Taklamakan Desert Hinterland

WANG Yong-dong1 ,
LI Sheng-yu1 ,
XU Xin-wen ,
LEI Jia-qiang1 ,
JIN Xiao-jun1 ,
2 ,
3 ,
WANG Qiang3 ,
DI Kun3 ,
ZHANG Zhong-liang3

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1.Xinjiang Institute of Ecology and Geography, Chineses Academy of Sciences, Urumqi 830011, China;
2.Graduate University, Chinese Academy of Sciences, Beijing 100049, China;
3.Tarim Branch,Petro China Company Limited,Kurle 841000, Xinjiang, China

Received date: 2012-01-31

Revised date: 2012-02-28

Online published: 2012-02-28

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摘要

对运用Hargreaves公式计算参考作物蒸散量(ET0)在干旱区的适用性存在不同观点。为了求证Hargreaves公式在极端干旱区塔克拉玛干沙漠腹地的适用性,利用2005—2010年塔克拉玛干沙漠研究站的气象资料,以利用Penman-Monteith公式计算的结果为标准,对利用Hargreaves公式计算的ET0进行了对比分析,并对两种计算结果差异的成因进行了阐释。结果表明:在年时间尺度上,利用Hargreaves公式计算的结果略大于利用Penman-Monteith公式计算的结果,标准差介于32.86~35.00 mm,年参考作物蒸散量计算结果呈现弱变异程度；在月时间尺度上,用两种方法计算的参考作物蒸散量呈现中等变异程度,蒸散量绝对偏差介于-3.26~8.73 mm,相对偏差介于-12.20%~29.02%,除了10月与11月,其余月份相对偏差均保持在10%之内。用两种方法计算的10月与11月份ET0产生差异的最主要原因在于有较高的温度较差。最后,经过对年、月参考作物蒸散量进行t-检验及建立回归方程,表明Hargreaves公式适用于极端干旱的塔克拉玛干沙漠腹地。

关键词： 极端干旱区; 塔克拉玛干沙漠; 参考作物蒸散量; Hargreaves; Penman-Monteith

本文引用格式

王永东1 , 李生宇1 , 徐新文1 , 雷加强1 , 金小军1 , 2 , 3 , 王强3 , 邸鲲3 , 张忠良3 . Hargreaves公式在塔克拉玛干沙漠腹地的适用性[J]. 中国沙漠, 2013 , 33(2) : 367 -373 . DOI: 10.7522/j.issn.1000-694X.2013.00051

Abstract

There are different opinions on the applicability of the Hargreaves method in calculating reference crop evapotranspiration (ET0) in arid land. In order to test the applicability of the Hargreaves method in the Taklamakan Desert hinterland, we carried out the current study using the metadata in 2005-2010 collected at the meteorological station in the Taklamakan Desert hinterland. The Penman-Monteith method was set as standard to compare the difference between the two methods. The results showed that at annual scale, the ET0 calculated with the Hargreaves equation was a little higher than that obtained by Penman-Monteith method, the standard deviation were 32.86~35.00 mm, and the annual reference crop evapotranspiration (ET0) presented weak variation; at monthly scale, the reference crop evapotranspiration (ET0) presented a middle variation, the absolute deviation of monthly ET0 was -3.26~8.73 mm between the two methods, and the monthly relative deviation was -12.20%~29.02%, and the ET0 deviations were all not more than 10% except for October and November. It was documented that the difference for the calculating ET0 between the two methods was resulted from the higher temperature range. Based on the estimated ET0 at annual and monthly scales by the two methods, our results indicated that the ET0 calculated with the Hargreaves method was applicable in the extreme arid area of the Taklamakan Desert hinterland.

Key words： extreme arid land; Taklimakan Desert; reference crop evapotranspiration; Hargreaves; Penman-Monteith

参考文献

[1]李玲玲,黄高宝.绿洲灌区参考作物蒸散量的测算[J].中国沙漠,2011,31(1):142-148.

[2]王素萍.近40 a江河源区潜在蒸散量变化特征及影响因子分析[J].中国沙漠,2009,29(5):960-965.

[3]候兰功,肖洪浪,邹松兵,等.额济纳绿洲生长季参考作物蒸散法敏感性分析[J].中国沙漠,2011,31(5):1255-1259.

[4]冯起,张艳武,司建华,等.土壤植被大气模式中水分和能量传输研究进展[J].中国沙漠,2009,29(1):143-150.

[5]胡广录,赵文智,武俊霞.绿洲灌区小麦水分生产率及其影响因素的灰色关联分析[J].中国沙漠,2010,30(2):369-375.

[6]Allen R G,Smith M,Pereira L S.An update for the definition of reference evapotranspiration [J].ICID Bulletion,1994,43（2）:1-34.

[7]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.

[8]Pereia A R.Prutit W O.Adaptation of the Thornthwaite scheme for estimating daily reference evapotranspiration[J].Agricultural Water Management,2004,66（3）:251-257.

[9]Irmak S,Allen R G,Whitty E B.Daily grass and alfalfa-reference evapotranspiration estimates and alfalfa-to-grass evapotranspiration ratio in Florida[J].Journal of Irrigation and Drainage Engineering,2003,129（5）:360-370.

[10]Trajkortic S.Temperature-based approaches for estimating reference evapotranspiration[J].Journal of Irrigation and Drainage Engineering,2005,131（4）:316-325.

[11]闫浩芳,史海滨,薛涛,等.内蒙古河套灌区ET0不同计算方法的对比研究[J].农业工程学报,2008,24(4):103-106.

[12]李晓军,李取生.东北地区参考作物蒸散确定方法研究[J].地理科学,2004,24(2):212-216.

[13]刘晓英,李玉中,王庆锁.几种基于温度的参考作物蒸散量计算方法的评价[J].农业工程学报,2006,22（6）:12-18.

[14]王声锋,段爱旺,张展羽.半干旱地区不同水文年Hargreaves和PM公式的对比分析[J].农业工程学报,2008,24(7):29-33.

[15]王新华,郭美华,徐中民.分别利用Hargreaves和PM公式计算西北干旱区ET0的比较[J].农业工程学报,2006,22(10):21-25.

[16]顾世祥,王士武,袁宏源.参考作物腾发量预测的径向基函数法[J].水科学进展,1999(2):123-128.

[17]高传昌,朱明锋,秦海霞.Hargraeves公式计算参考作物腾发量在新疆地区的适用性研究[J].灌溉排水学报,2008,27（3）:60-62.

[18]Hargreaves G H,Allen R G.History and evaluation of Hargreaves evapotranspiration equation[J].Journal of Irrigation and Drainage Engineering,2003,129(1):53-63.

[19]Temesgen B,Eching S,Davidoff B,et al.Comparison of some reference evapotranspiration equations for California[J].Journal of Irrigation and Drainage Engineering,2005,131(1):73-84.

[20]胡庆芳,杨大文,王银堂,等.Hargreaves公式的全局校正及适用性评价[J].水科学进展,2011,22(2):160-161.

[21]Allen R G.Evaluation of Procedure for Estimating Mean Monthly Solar Radiation from Air Temperature[R].Rome: FAO,1995.

[22]Droogers P,Allen R G.Estimating reference evapotranspiration under inaccurate data conditions[J].Irrigation Drainage System,2002(16):33-45.

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