Estimation of Reference Evapotranspiration during the Irrigation Season Using Nine Temperature-Based Methods in a Hot-Summer Mediterranean Climate

The FAO-56 Penman–Monteith (PM) equation is regarded as the most accurate equation to estimate reference evapotranspiration (ETo). However, it requires a broad range of data that may not be available or of reasonable quality. In this study, nine temperature-based methods were assessed for ETo estima...

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Main Authors: Gonçalo C. Rodrigues, Ricardo P. Braga
Format: Article
Language:English
Published: MDPI AG 2021-02-01
Series:Agriculture
Subjects:
Online Access:https://www.mdpi.com/2077-0472/11/2/124
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spelling doaj-49e62c84b1b44ea3899bb4488a3321302021-04-02T20:20:31ZengMDPI AGAgriculture2077-04722021-02-011112412410.3390/agriculture11020124Estimation of Reference Evapotranspiration during the Irrigation Season Using Nine Temperature-Based Methods in a Hot-Summer Mediterranean ClimateGonçalo C. Rodrigues0Ricardo P. Braga1LEAF—Linking Landscape, Environment, Agriculture and Food, Instituto Superior de Agronomia, Universidade de Lisboa, Tapada da Ajuda, 1349-017 Lisboa, PortugalInstituto Superior de Agronomia, Universidade de Lisboa, Tapada da Ajuda, 1349-017 Lisboa, PortugalThe FAO-56 Penman–Monteith (PM) equation is regarded as the most accurate equation to estimate reference evapotranspiration (ETo). However, it requires a broad range of data that may not be available or of reasonable quality. In this study, nine temperature-based methods were assessed for ETo estimation during the irrigation at fourteen locations distributed through a hot-summer Mediterranean climate region of Alentejo, Southern Portugal. Additionally, for each location, the Hargreaves–Samani radiation adjustment coefficient (k<sub>Rs</sub>) was calibrated and validated to evaluate the appropriateness of using the standard value, creating a locally adjusted Hargreaves–Samani (HS) equation. The accuracy of each method was evaluated by statistically comparing their results with those obtained by PM. Results show that the calibration of the k<sub>Rs</sub>, a locally adjusted HS method can be used to estimate daily ETo acceptably well, with RMSE lower than 0.88 mm day<sup>−1</sup>, an estimation error lower than 4% and a R<sup>2</sup> higher than 0.69, proving to be the most accurate model for 8 (out of 14) locations. A modified Hargreaves–Samani method also performed acceptably for 4 locations, with a RMSE of 0.72–0.84 mm day<sup>−1</sup>, a slope varying from 0.95 to 1.01 and a R<sup>2</sup> higher than 0.78. One can conclude that, when weather data is missing, a calibrated HS equation is adequate to estimate ETo during the irrigation season.https://www.mdpi.com/2077-0472/11/2/124reference evapotranspirationFAO Penman MonteithHargreaves–Samanitemperature-based ET methodsirrigation schedulinghot summer Mediterranean climate
collection DOAJ
language English
format Article
sources DOAJ
author Gonçalo C. Rodrigues
Ricardo P. Braga
spellingShingle Gonçalo C. Rodrigues
Ricardo P. Braga
Estimation of Reference Evapotranspiration during the Irrigation Season Using Nine Temperature-Based Methods in a Hot-Summer Mediterranean Climate
Agriculture
reference evapotranspiration
FAO Penman Monteith
Hargreaves–Samani
temperature-based ET methods
irrigation scheduling
hot summer Mediterranean climate
author_facet Gonçalo C. Rodrigues
Ricardo P. Braga
author_sort Gonçalo C. Rodrigues
title Estimation of Reference Evapotranspiration during the Irrigation Season Using Nine Temperature-Based Methods in a Hot-Summer Mediterranean Climate
title_short Estimation of Reference Evapotranspiration during the Irrigation Season Using Nine Temperature-Based Methods in a Hot-Summer Mediterranean Climate
title_full Estimation of Reference Evapotranspiration during the Irrigation Season Using Nine Temperature-Based Methods in a Hot-Summer Mediterranean Climate
title_fullStr Estimation of Reference Evapotranspiration during the Irrigation Season Using Nine Temperature-Based Methods in a Hot-Summer Mediterranean Climate
title_full_unstemmed Estimation of Reference Evapotranspiration during the Irrigation Season Using Nine Temperature-Based Methods in a Hot-Summer Mediterranean Climate
title_sort estimation of reference evapotranspiration during the irrigation season using nine temperature-based methods in a hot-summer mediterranean climate
publisher MDPI AG
series Agriculture
issn 2077-0472
publishDate 2021-02-01
description The FAO-56 Penman–Monteith (PM) equation is regarded as the most accurate equation to estimate reference evapotranspiration (ETo). However, it requires a broad range of data that may not be available or of reasonable quality. In this study, nine temperature-based methods were assessed for ETo estimation during the irrigation at fourteen locations distributed through a hot-summer Mediterranean climate region of Alentejo, Southern Portugal. Additionally, for each location, the Hargreaves–Samani radiation adjustment coefficient (k<sub>Rs</sub>) was calibrated and validated to evaluate the appropriateness of using the standard value, creating a locally adjusted Hargreaves–Samani (HS) equation. The accuracy of each method was evaluated by statistically comparing their results with those obtained by PM. Results show that the calibration of the k<sub>Rs</sub>, a locally adjusted HS method can be used to estimate daily ETo acceptably well, with RMSE lower than 0.88 mm day<sup>−1</sup>, an estimation error lower than 4% and a R<sup>2</sup> higher than 0.69, proving to be the most accurate model for 8 (out of 14) locations. A modified Hargreaves–Samani method also performed acceptably for 4 locations, with a RMSE of 0.72–0.84 mm day<sup>−1</sup>, a slope varying from 0.95 to 1.01 and a R<sup>2</sup> higher than 0.78. One can conclude that, when weather data is missing, a calibrated HS equation is adequate to estimate ETo during the irrigation season.
topic reference evapotranspiration
FAO Penman Monteith
Hargreaves–Samani
temperature-based ET methods
irrigation scheduling
hot summer Mediterranean climate
url https://www.mdpi.com/2077-0472/11/2/124
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AT ricardopbraga estimationofreferenceevapotranspirationduringtheirrigationseasonusingninetemperaturebasedmethodsinahotsummermediterraneanclimate
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