收藏设为首页 广告服务联系我们在线留言

干旱区地理 ›› 2016, Vol. 39 ›› Issue (1): 130-135.

• 生物与土壤 • 上一篇    下一篇

塔里木盆地绿洲参考作物蒸散量计算方法比较

高飞1,2, 李新虎1   

  1. 1. 中国科学院新疆生态与地理研究所荒漠与绿洲生态国家重点实验室, 新疆 乌鲁木齐 830011;
    2. 中国科学院大学, 北京 100049
  • 收稿日期:2015-08-18 修回日期:2015-11-20 出版日期:2016-01-25
  • 作者简介:高飞(1988-),男,甘肃定西人,硕士研究生,主要从事农田蒸散方面的研究.Email:gaofei12@mails.ucas.ac.cn
  • 基金资助:

    国家重点基础研究发展计划(2013CB429905);国家自然科学基金-新疆联合基金面上项目(U1303181);国家青年科学基金项目(41101100)

Comparison of methods for estimating reference evapotranspiration in oasis of Tarim Basin

GAO Fei1,2, LI Xin-hu1   

  1. 1 State Key Laboratory of Desert and Oasis, Xinjiang Institute of Ecology and Geography, Chinese Academic of Science, Urumqi 830011, Xinjiang, China;
    2 University of Chinese Academic of Sciences, Beijing 100049, China
  • Received:2015-08-18 Revised:2015-11-20 Online:2016-01-25

摘要: 应用FAO-56 Penman-Monteith、1972 Kimberly Penman、FAO PPP-17 Penman、FAO-24 Radiation、1985 Hargreaves、1948 Penman、Priestley-Taylor 和1957 Makkink 8 种公式计算了塔里木盆地绿洲棉区的参考作物蒸散量,并对8 种方法的计算结果进行了比较,结果表明:1972 KimberlyPenman 的计算结果与标准方法FAO-56 Penman-Monteith 的计算结果最接近,FAO-24 Radiation 的计算结果与标准方法FAO-56 Penman-Monteith 的计算结果差异最大.在估算塔里木盆地绿洲棉区的参考作物蒸散量时,可选用1972 Kimberly Penman公式.

关键词: 塔里木盆地绿洲, 参考作物蒸散量, 计算方法

Abstract: Evapotranspiration is a complex process and appears in both water balance equation and land surface energy balance equation. It is practically and scientifically significant for water resources management and ecological restoration to evaluate the applicability of ETo models. Eight alternative ETo methods,including the FAO-56 Penman-Monteith,1972 Kimberly Penman,FAO PPP-17 Penman,FAO-24 Radiation,1985 Hargreaves, 1948 Penman,Priestley-Taylor and 1957 Makkink were evaluated for use in oasis of Traim Basin at Aksu Water Balance Experimental Station during the period of 2008 to 2012. The results showed that:ETo estimates produced by 1972 Kimberly Penman were very near,in general,to those by FAO-56 Penman-Monteith,but ETo estimates produced by FAO-24 Radiation were very far from those by FAO-56 Penman-Monteith. Monthy ETo derived from all the equations appeared to follow the same trend that the ETo value would go up from April to June, reach the maximum in July and go down from August to September. Compared to FAO-56 Penman-Monteith,the results from 1972 Kimberly Penman and 1957 Makkink were lower,while others were higher. The value of D, EF and RMSE ranged from 0.91 to 0.99,0.83 to 0.99 and 0.23 to 0.99,respectively. Therein,the 1972 Kimberly Penman obtained the maximum D and EF of 0.99 and 0.99,respectively,and the minimum RMSE of 0.23,therefore, the 1972 Kimberly Penman is the most suitable method for the calculation of reference evapotranspiration in oasis of Tarim Basin.

Key words: oasis of Traim Basin, reference evapotranspiration, calculation methods

中图分类号: 

  • P333.1