Applicability of FAO56 and ASCE Penman-Monteith equations for reference crop evapotranspiration calculation on turf grass

被引:0
作者
Xu, Junzeng [1 ]
Peng, Shizhang [1 ]
Zhang, Xingnan [1 ]
Ding, Jiali [2 ]
Wang, Weiguang [1 ]
机构
[1] State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University
[2] Bureau of Water Conservancy
来源
Nongye Gongcheng Xuebao/Transactions of the Chinese Society of Agricultural Engineering | 2009年 / 25卷 / 12期
关键词
Crops; Evapotranspiration; Penman-Monteith; Reference crop evapotranspiration; Turf grass; Water;
D O I
10.3969/j.issn.1002-6819.2009.12.006
中图分类号
学科分类号
摘要
In order to reveal the difference between hourly reference crop evapotranspiration(ET0) calculated by FAO56 Penman- Monteith equation and that by ASCE Penman-Monteith , as well as the 24-hour accumulated daily ET0, well watered lysimeter experiment were carried out on turf grass. Hourly ET0 and 24-hour accumulated daily ET0 were calculated based on hourly meteorological data and evaluated by using daily observed grass evapotranspiration derived from well watered lysimeter experiment. There was a certain difference between ET0 calculated by FAO56 Penman-Monteith equation and that by ASCE Penman-Monteith equation, and the difference was more significant when the ET0 values were relative higher. Hourly ET0 were tested to be lower for FAO56 Penman-Monteith equation than for ASCE Penman-Monteith equation in daytime, but just reversed at night. That was ascribed to the difference in Cd values. It was a pity to say that the equation mended by ASCE could not result in improvement in hourly ET0 calculation, when the 24-hour accumulated daily ET0 were compared with observed daily grass evapotranspiration. Daily ET0 calculated by Penman-Monteith equation based on meteorological data at daily time step were test to be the most consistent with that by lysimeter observed. Further evaluation of either FAO56 Penman-Monteith equation or ASCE Penman-Monteith equation was urgent in China, based on hourly or long series daily observed grass evapotranspiration.
引用
收藏
页码:32 / 37
页数:5
相关论文
共 21 条
[1]  
Doorenbos J., Pruitt W.O., Crop Water Requirements, (1975)
[2]  
pp. 50-128, (1995)
[3]  
Allen R.G., Pereira L.S., Raes D., Et al., Crop Evapotranspiration-Guidelines for Computing Crop Water Requirement, (1998)
[4]  
Hossein D., Tahei Y., Velu R., Assessment of evapotranspiration estimation models for use in semi-arid environments, Agricultural Water Management, 64, 2, pp. 91-106, (2004)
[5]  
Trajkovic S., Hargreaves versus Penman-Monteith under Humid Conditions, Journal of Irrigation and Drainage Engineering, ASCE, 133, 1, pp. 38-42, (2007)
[6]  
Liu Y., Preira L.S., Teixira J.L., Update definition and computation of reference evapotranspiration comparison with former method, Journal of Hydraulic Engineering, 28, 6, pp. 27-33, (1997)
[7]  
The ASCE Standardized Reference Evapotranspiration Equation, (2005)
[8]  
Itenfisu D., Elliott R.L., Allen R.G., Et al., Comparison of reference evapotranspiration calculations as a part of the ASCE standardization effort, Journal of Irrigation and Drainage Engineering, ASCE, 129, 6, pp. 440-448, (2003)
[9]  
Su C., Chen Y., Xu B., Recent development and universality evaluation of ET<sub>0</sub> calculation formulas, Advances in Water Science, 19, 1, pp. 129-136, (2008)
[10]  
Du Y., Liu Z., Zhang Y., Evaluation of two reference crop evapotranspiration calculation methods, Journal of Henan Agricultural University, 35, 1, pp. 57-61, (2001)