Performance evaluation of reference evapotranspiration equations across a range of Indian climates

Lakshman Nandagiri, Gicy M. Kovoor

Research output: Contribution to journalArticle

80 Citations (Scopus)

Abstract

Reference crop evapotranspiration (ET 0) is a key variable in procedures established for estimation of evapotranspiration rates of agricultural crops. In recent years, there is growing evidence to show that the more physically based FAO-56 Penman-Monteith (PM) combination method yields consistently more accurate ET 0 estimates across a wide range of climates and is being proposed as the sole method for ET 0 computations. However, other methods continue to remain popular among Indian practitioners either because of traditional usage or because of their simpler input data requirements. In this study, we evaluated the performances of several ET 0 methods in the major climate regimes of India with a view to quantify differences in ET 0 estimates as influenced by climatic conditions and also to identify methods that yield results closest to the FAO-56 PM method. Performances of seven ET 0 methods, representing temperature-based, radiation-based, pan evaporation-based, and combination-type equations, were compared with the FAO-56 PM method using historical climate data from four stations located one each in arid (Jodhpur), semiarid (Hyderabad), subhumid (Bangalore), and humid (Pattambi) climates of India. For each location, ET0 estimates by all the methods for assumed hypothetical grass reference crop were statistically compared using daily climate records extending over periods of 3-4 years. Comparisons were performed for daily and monthly computational time steps. Overall results while providing information on variations in FAO-56 PM ET0 values across climates also indicated climate-specific differences in ET 0 estimates obtained by the various methods. Among the ET 0 methods evaluated, the FAO-56 Hargreaves (temperature-based) method yielded ET 0 estimates closest to the FAO-56 PM method both for daily and monthly time steps, in all climates except the humid one where the Turc (radiation-based) was best. Considering daily comparisons, the associated minimum standard errors of estimate (SEE) were 1.35, 0.78, 0.67, and 0.31 mm/day, for the arid, semiarid, subhumid, and humid locations, respectively. For monthly comparisons, minimum SEE values were smaller at 0.95, 0.59, 0.38, and 0.20 mm/day for arid, semiarid, subhumid, and humid locations, respectively. These results indicate that the choice of an alternative simpler equation in a particular climate on the basis of SEE is dictated by the time step adopted and also it appears that the simpler equations yield much smaller errors when monthly computations are made. In order to provide simple ET 0 estimation tools for practitioners, linear regression equations for preferred FAO-56 PM ET 0 estimates in terms of ET 0 estimates by the simpler methods were developed and validated for each climate. A novel attempt was made to investigate the reasons for the climate-dependent success of the simpler alternative ET 0 equations using multivariate factor analysis techniques. For each climate, datasets comprising FAO-56 PM ET 0 estimates and the climatic variables were subject to factor analysis and the resulting rotated factor loadings were used to interpret the relative importance of climatic variables in explaining the observed variabilities in ET 0 estimates. Results of factor analysis more or less conformed the results of the statistical comparisons and provided a statistical justification for the ranking of alternative methods based on performance indices. Factor analysis also indicated that windspeed appears to be an important variable in the arid climate, whereas sunshine hours appear to be more dominant in subhumid and humid climates. Temperature related variables appear to be the most crucial inputs required to obtain ET 0 estimates comparable to those from the FAO-56 PM method across all the climates considered.

Original languageEnglish
Pages (from-to)238-249
Number of pages12
JournalJournal of Irrigation and Drainage Engineering
Volume132
Issue number3
DOIs
Publication statusPublished - 01-06-2006

Fingerprint

Evapotranspiration
Factor analysis
Climate
evapotranspiration
Crops
climate
Food and Agricultural Organization
Radiation
methodology
Linear regression
factor analysis
Temperature
Statistical Factor Analysis
humid zones
Evaporation
evaluation
method
crop
India
crops

All Science Journal Classification (ASJC) codes

  • Agricultural and Biological Sciences (miscellaneous)
  • Water Science and Technology
  • Civil and Structural Engineering

Cite this

@article{8685d3e374de481eb2ea87e149bf0085,
title = "Performance evaluation of reference evapotranspiration equations across a range of Indian climates",
abstract = "Reference crop evapotranspiration (ET 0) is a key variable in procedures established for estimation of evapotranspiration rates of agricultural crops. In recent years, there is growing evidence to show that the more physically based FAO-56 Penman-Monteith (PM) combination method yields consistently more accurate ET 0 estimates across a wide range of climates and is being proposed as the sole method for ET 0 computations. However, other methods continue to remain popular among Indian practitioners either because of traditional usage or because of their simpler input data requirements. In this study, we evaluated the performances of several ET 0 methods in the major climate regimes of India with a view to quantify differences in ET 0 estimates as influenced by climatic conditions and also to identify methods that yield results closest to the FAO-56 PM method. Performances of seven ET 0 methods, representing temperature-based, radiation-based, pan evaporation-based, and combination-type equations, were compared with the FAO-56 PM method using historical climate data from four stations located one each in arid (Jodhpur), semiarid (Hyderabad), subhumid (Bangalore), and humid (Pattambi) climates of India. For each location, ET0 estimates by all the methods for assumed hypothetical grass reference crop were statistically compared using daily climate records extending over periods of 3-4 years. Comparisons were performed for daily and monthly computational time steps. Overall results while providing information on variations in FAO-56 PM ET0 values across climates also indicated climate-specific differences in ET 0 estimates obtained by the various methods. Among the ET 0 methods evaluated, the FAO-56 Hargreaves (temperature-based) method yielded ET 0 estimates closest to the FAO-56 PM method both for daily and monthly time steps, in all climates except the humid one where the Turc (radiation-based) was best. Considering daily comparisons, the associated minimum standard errors of estimate (SEE) were 1.35, 0.78, 0.67, and 0.31 mm/day, for the arid, semiarid, subhumid, and humid locations, respectively. For monthly comparisons, minimum SEE values were smaller at 0.95, 0.59, 0.38, and 0.20 mm/day for arid, semiarid, subhumid, and humid locations, respectively. These results indicate that the choice of an alternative simpler equation in a particular climate on the basis of SEE is dictated by the time step adopted and also it appears that the simpler equations yield much smaller errors when monthly computations are made. In order to provide simple ET 0 estimation tools for practitioners, linear regression equations for preferred FAO-56 PM ET 0 estimates in terms of ET 0 estimates by the simpler methods were developed and validated for each climate. A novel attempt was made to investigate the reasons for the climate-dependent success of the simpler alternative ET 0 equations using multivariate factor analysis techniques. For each climate, datasets comprising FAO-56 PM ET 0 estimates and the climatic variables were subject to factor analysis and the resulting rotated factor loadings were used to interpret the relative importance of climatic variables in explaining the observed variabilities in ET 0 estimates. Results of factor analysis more or less conformed the results of the statistical comparisons and provided a statistical justification for the ranking of alternative methods based on performance indices. Factor analysis also indicated that windspeed appears to be an important variable in the arid climate, whereas sunshine hours appear to be more dominant in subhumid and humid climates. Temperature related variables appear to be the most crucial inputs required to obtain ET 0 estimates comparable to those from the FAO-56 PM method across all the climates considered.",
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Performance evaluation of reference evapotranspiration equations across a range of Indian climates. / Nandagiri, Lakshman; Kovoor, Gicy M.

In: Journal of Irrigation and Drainage Engineering, Vol. 132, No. 3, 01.06.2006, p. 238-249.

Research output: Contribution to journalArticle

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