2016
DOI: 10.5935/1806-6690.20160054
|View full text |Cite
|
Sign up to set email alerts
|

Defining parameters for the Hargreaves-Samani equation for estimating reference evapotranspiration in the State of Ceará, Brazil

Abstract: RESUMO-O modelo de Hargreaves e Samani é utilizado na estimativa da evapotranspiração de referência, sendo muito útil para o manejo da irrigação, sendo o mesmo considerado de uso prático, pois utiliza elementos meteorológicos de fácil obtenção como a temperatura. Entretanto, o mesmo necessita de calibração regional para estimar adequadamente a evapotranspiração. Objetivou-se calibrar o modelo de Hargreaves e Samani para o estado do Ceará, utilizando dados meteorológicos de doze cidades. Os parâmetros empíricos… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1

Citation Types

0
2
0
1

Year Published

2017
2017
2021
2021

Publication Types

Select...
8

Relationship

1
7

Authors

Journals

citations
Cited by 12 publications
(3 citation statements)
references
References 13 publications
0
2
0
1
Order By: Relevance
“…If this calibration improves performance, an efficient and easy-to-use method is available. This calibration has been done by several researchers in many regions of Brazil: Goiás (Fernandes et al, 2012), Ceará (Lima Júnior et al, 2016), Pernambuco (Arraes et al, 2016) and Sete Lagoas -MG (Borges Júnior et al, 2017) and, of the world: Spain (Gavilán et al, 2006), Iran (Tabari & Zalaee, 2011), Bosnia and Herzegovina (Čadro et al, 2017) and Sichuan-China (Feng et al, 2017).…”
Section: Resultsmentioning
confidence: 99%
“…If this calibration improves performance, an efficient and easy-to-use method is available. This calibration has been done by several researchers in many regions of Brazil: Goiás (Fernandes et al, 2012), Ceará (Lima Júnior et al, 2016), Pernambuco (Arraes et al, 2016) and Sete Lagoas -MG (Borges Júnior et al, 2017) and, of the world: Spain (Gavilán et al, 2006), Iran (Tabari & Zalaee, 2011), Bosnia and Herzegovina (Čadro et al, 2017) and Sichuan-China (Feng et al, 2017).…”
Section: Resultsmentioning
confidence: 99%
“…After verification of the data homogeneity, the potential evapotranspiration (ETo) (mm d -1 ) for the 15 INMET stations was calculated using the equation proposed by [14], which considers the following variables: radiation at the top of the atmosphere, maximum, average and minimum daily temperature. This equation is an alternative for estimating potential evapotranspiration in sites with limited data availability, according to [15], and is expressed by the following equation: As the number of stations with precipitation data only (169) was much higher than the stations with data for the calculation of the potential evapotranspiration (15), the ANA rainfall series were grouped by INMET meteorological station. For this grouping, the Thiessen polygon method was used in order to obtain estimates of actual and maximum evapotranspiration for the 184 stations.…”
Section: Methodsmentioning
confidence: 99%
“…O modelo de Hargreaves e Samani (HS) apresentou bons resultados em vários locais em que foi utilizado, principalmente quando efetuado ajuste dos seus parâmetros (BORGES; MENDIONDO, 2007;TALAEE, 2011;JÚNIOR et al, 2012;RAZIEI;PEREIRA, 2013;TABARI et al, 2013;LIMA JUNIOR et al, 2016).…”
Section: Introductionunclassified