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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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 |
work_keys_str_mv |
AT goncalocrodrigues estimationofreferenceevapotranspirationduringtheirrigationseasonusingninetemperaturebasedmethodsinahotsummermediterraneanclimate AT ricardopbraga estimationofreferenceevapotranspirationduringtheirrigationseasonusingninetemperaturebasedmethodsinahotsummermediterraneanclimate |
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