1977
DOI: 10.1590/s0006-87051977000100005
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Estimativa de graus-dia em função de altitude e latitude para o estado de São Paulo

Abstract: ( 1 ) Recebido para publicação em 21 de julho de 1976.(-) Com bolsa de suplementaçífo do C.N.Pq. SINOPSEO grau-dia é uma unidade térmica utilizada, principalmente, na determinação de épocas de plantio e colheita dos vegetais, contribuindo para uma agricultura racional. Pode ser estimado através de dados termométricos, ou seja, de médias mensais de temperaturas máximas e minimas, obtidas em abrigos meteorológicos padrões, para regiões climaticamente homogêneas.No presente trabalho foi utilizada a temperatura ba… Show more

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Cited by 11 publications
(6 citation statements)
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“…Climatic data for the locations and periods that the fruits were produced were obtained from automatic weather stations installed close to the harvest areas. Daily data of temperature and 225 MATURATION OF Eugenia pyriformis SEEDS rainfall (mm) were collected between flowering and harvest and were used to calculate respectively: the growing degree-day (GDD, °C day), according to the equations proposed by Villa Nova et al (1972), considering 10°C as base temperature (Pedro Junior et al 1977); and accumulated rainfall (mm). Sequential water balance was also calculated with rainfall data using the model proposed by Thornthwaite and Mather (1955), in descending scale level with available water capacity (AWC) of 125 mm (Leivas et al 2006, Rolim et al 2007.…”
Section: Methodsmentioning
confidence: 99%
“…Climatic data for the locations and periods that the fruits were produced were obtained from automatic weather stations installed close to the harvest areas. Daily data of temperature and 225 MATURATION OF Eugenia pyriformis SEEDS rainfall (mm) were collected between flowering and harvest and were used to calculate respectively: the growing degree-day (GDD, °C day), according to the equations proposed by Villa Nova et al (1972), considering 10°C as base temperature (Pedro Junior et al 1977); and accumulated rainfall (mm). Sequential water balance was also calculated with rainfall data using the model proposed by Thornthwaite and Mather (1955), in descending scale level with available water capacity (AWC) of 125 mm (Leivas et al 2006, Rolim et al 2007.…”
Section: Methodsmentioning
confidence: 99%
“…(*) = r significativo a 5% de probabilidade, ( NS ) = r não significativo. Table 2 Sensibilidade à dessecação de embriões de... (MARTINS et al, 2009;LAMARCA et al, 2013b), as características fotoblásticas e as exigências térmicas para a germinação (GUARDIA; LAMARCA, 2013) e os níveis de dormência e de tolerância à dessecação (DAWS et al, 2004(DAWS et al, , 2006PEREIRA et al, 2012).…”
Section: Discussionunclassified
“…O somatório de graus-dia (GD) foi realizado desde a floração até a colheita, segundo as equações propostas por Villa Nova et al (1972), considerando a temperatura base de 10 °C (PEDRO JUNIOR et al, 1977). Calculou-se, ainda, o balanço hídrico sequencial (mm), segundo o modelo proposto por Thornthwaite e Mather (1955), em nível de escala decendial, com capacidade de água disponível (CAD) de 125 mm (ROLIM et al, 2007).…”
Section: Methodsunclassified
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“…BURIOL & ESTEFANEL (1976) estimated the sum of monthly and annual GD at the state of Rio Grande do Sul as a function of the altitude, latitude, longitude, using T b of 0 ºC, 5 °C, 10 ºC, 15 ºC and 20 ºC, and obtained coefficients of determination ranging between 0.92 and 0.97, depending on the month and the T b applied. PEDRO JÚNIOR et al (1977) correlated GD with altitude and latitude by means of multiple linear regressions, and obtained coefficients of determination varying between 0.81 and 0.88, depending on the month analyzed. Despite the relevant contribution of these reports, GD modeling has been carried out considering the spatial and temporal variables separately, and using only monthly or annually scale.…”
Section: Introductionmentioning
confidence: 99%