Parametric calibration of the Hargreaves–Samani equation for use at new locations

Detalhes bibliográficos
Autor(a) principal: Shahidian, Shakib
Data de Publicação: 2013
Outros Autores: Serralheiro, Ricardo, Serrano, João Manuel, Teixeira, José Luís
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10174/9231
https://doi.org/10.1002/hyp.9277
Resumo: The Hargreaves–Samani (HS) evapotranspiration equation is very useful for the on-site irrigation management in data-short situations such as small and midsize farms and landscaped areas. Although much work has been performed to improve the precision of the evapotranspiration (ETo) estimates for use at new locations, the results have not been consistent and many have not been confirmed by other works. The purpose of this study was to review and to evaluate the seven most promising parameters used for the calibration of the HS evapotranspiration equation, using two different regions: California and Bolivia. The results of this study show that annual correlations between HS and Penman–Monteith can be misleading because the correlation is poor in the humid months and improves progressively along the dry season until the first rains. The average monthly wind speed can be used for both spatial and seasonal calibration of the HS equation, especially during the irrigation season. Elevation and precipitation can be used to calibrate the HS equation when no reference ETo values are available at nearby stations. The monthly value of KT calculated from solar radiation follows a parabolic function along the year and should not be used for improving the estimates of the HS equation because the clearness index produces better results than actual solar radiation measurements. The results also indicate that the use of distance to coast, temperature range and temperature parameter does not improve the precision of the HS equation
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spelling Parametric calibration of the Hargreaves–Samani equation for use at new locationshargreaves SamaniEvapotranspirationcalibrationThe Hargreaves–Samani (HS) evapotranspiration equation is very useful for the on-site irrigation management in data-short situations such as small and midsize farms and landscaped areas. Although much work has been performed to improve the precision of the evapotranspiration (ETo) estimates for use at new locations, the results have not been consistent and many have not been confirmed by other works. The purpose of this study was to review and to evaluate the seven most promising parameters used for the calibration of the HS evapotranspiration equation, using two different regions: California and Bolivia. The results of this study show that annual correlations between HS and Penman–Monteith can be misleading because the correlation is poor in the humid months and improves progressively along the dry season until the first rains. The average monthly wind speed can be used for both spatial and seasonal calibration of the HS equation, especially during the irrigation season. Elevation and precipitation can be used to calibrate the HS equation when no reference ETo values are available at nearby stations. The monthly value of KT calculated from solar radiation follows a parabolic function along the year and should not be used for improving the estimates of the HS equation because the clearness index produces better results than actual solar radiation measurements. The results also indicate that the use of distance to coast, temperature range and temperature parameter does not improve the precision of the HS equationHydrological Processes2014-01-06T13:03:12Z2014-01-062013-02-15T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://hdl.handle.net/10174/9231http://hdl.handle.net/10174/9231https://doi.org/10.1002/hyp.9277engShahidian, S., Serralheiro, R. P., Serrano, J., & Teixeira, J. L. (2012). Parametric calibration of the Hargreaves–Samani equation for use at new locations. Hydrological Processes.ERUshakib@uevora.ptricardo@uevora.ptjmrs@uevora.ptjlteixeira@isa.utl.pt580Shahidian, ShakibSerralheiro, RicardoSerrano, João ManuelTeixeira, José Luísinfo:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2024-01-03T18:51:04Zoai:dspace.uevora.pt:10174/9231Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-20T01:03:22.598470Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse
dc.title.none.fl_str_mv Parametric calibration of the Hargreaves–Samani equation for use at new locations
title Parametric calibration of the Hargreaves–Samani equation for use at new locations
spellingShingle Parametric calibration of the Hargreaves–Samani equation for use at new locations
Shahidian, Shakib
hargreaves Samani
Evapotranspiration
calibration
title_short Parametric calibration of the Hargreaves–Samani equation for use at new locations
title_full Parametric calibration of the Hargreaves–Samani equation for use at new locations
title_fullStr Parametric calibration of the Hargreaves–Samani equation for use at new locations
title_full_unstemmed Parametric calibration of the Hargreaves–Samani equation for use at new locations
title_sort Parametric calibration of the Hargreaves–Samani equation for use at new locations
author Shahidian, Shakib
author_facet Shahidian, Shakib
Serralheiro, Ricardo
Serrano, João Manuel
Teixeira, José Luís
author_role author
author2 Serralheiro, Ricardo
Serrano, João Manuel
Teixeira, José Luís
author2_role author
author
author
dc.contributor.author.fl_str_mv Shahidian, Shakib
Serralheiro, Ricardo
Serrano, João Manuel
Teixeira, José Luís
dc.subject.por.fl_str_mv hargreaves Samani
Evapotranspiration
calibration
topic hargreaves Samani
Evapotranspiration
calibration
description The Hargreaves–Samani (HS) evapotranspiration equation is very useful for the on-site irrigation management in data-short situations such as small and midsize farms and landscaped areas. Although much work has been performed to improve the precision of the evapotranspiration (ETo) estimates for use at new locations, the results have not been consistent and many have not been confirmed by other works. The purpose of this study was to review and to evaluate the seven most promising parameters used for the calibration of the HS evapotranspiration equation, using two different regions: California and Bolivia. The results of this study show that annual correlations between HS and Penman–Monteith can be misleading because the correlation is poor in the humid months and improves progressively along the dry season until the first rains. The average monthly wind speed can be used for both spatial and seasonal calibration of the HS equation, especially during the irrigation season. Elevation and precipitation can be used to calibrate the HS equation when no reference ETo values are available at nearby stations. The monthly value of KT calculated from solar radiation follows a parabolic function along the year and should not be used for improving the estimates of the HS equation because the clearness index produces better results than actual solar radiation measurements. The results also indicate that the use of distance to coast, temperature range and temperature parameter does not improve the precision of the HS equation
publishDate 2013
dc.date.none.fl_str_mv 2013-02-15T00:00:00Z
2014-01-06T13:03:12Z
2014-01-06
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://hdl.handle.net/10174/9231
http://hdl.handle.net/10174/9231
https://doi.org/10.1002/hyp.9277
url http://hdl.handle.net/10174/9231
https://doi.org/10.1002/hyp.9277
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv Shahidian, S., Serralheiro, R. P., Serrano, J., & Teixeira, J. L. (2012). Parametric calibration of the Hargreaves–Samani equation for use at new locations. Hydrological Processes.
ERU
shakib@uevora.pt
ricardo@uevora.pt
jmrs@uevora.pt
jlteixeira@isa.utl.pt
580
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv Hydrological Processes
publisher.none.fl_str_mv Hydrological Processes
dc.source.none.fl_str_mv reponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação
instacron:RCAAP
instname_str Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação
instacron_str RCAAP
institution RCAAP
reponame_str Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
collection Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
repository.name.fl_str_mv Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação
repository.mail.fl_str_mv
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