1988
DOI: 10.1080/01431168808954888
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Determination of the effective emissivity and temperature under vertical observation of a citrus orchard. Application to frost nowcasting

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Cited by 26 publications
(5 citation statements)
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“…He introduced effective parameters of emissivity and temperature to simplify the mathematical development. Becker's model was validated by Caselles et al (1988) in an orange grove under vertical observation and a precision of 1% was obtained. Caselles and Sobrino (1989) give a more practical definition of the effective temperature than that proposed by Becker, which was used for determining orange tree temperatures from NOAA-AVHRR data.…”
Section: Geometrical Effectsmentioning
confidence: 99%
“…He introduced effective parameters of emissivity and temperature to simplify the mathematical development. Becker's model was validated by Caselles et al (1988) in an orange grove under vertical observation and a precision of 1% was obtained. Caselles and Sobrino (1989) give a more practical definition of the effective temperature than that proposed by Becker, which was used for determining orange tree temperatures from NOAA-AVHRR data.…”
Section: Geometrical Effectsmentioning
confidence: 99%
“…where £=(£1 +£2)/2 (2) Land surfaces are usually inhomogeneous (Becker and Raffy 1987) and a large range of LSTs can exist within a pixel, which makes the definition of effective surface temperatures and emissivities (Caselles et al 1988) difficult.…”
Section: ) Multi-angle Methodsmentioning
confidence: 99%
“…Essas temperaturas são estimadas segundo a Lei de Planck que estabelece que quanto maior a temperatura de um dado comprimento de onda, maior a quantidade de energia emitida por um corpo negro (blackbody) (BAPTISTA, 2003;DASH et al, 2002;WENG e YANG, 2004b;PRATA et al, 1995;BIAS et al, 2003). A temperatura quantificada pelo satélite é a temperatura radiante da superficie que é um valor superior à temperatura do ar A determinação da LST é um interesse que data de muito tempo e atinge diversas áreas de conhecimento como, por exemplo, processos termais que ocorrem no oceano (SCHLUESSEL et al, 1990;BARTON, 1995;OLIVEIRA, 2001), determinação de locais de pesca (ABDON, 1982), estimativa da umidade do solo (EPIPHANIO, 1982; , 1977;BECKER, 1981;MALARET et al, 1985;CASELLES et. al., 1988;SOBRINO e CASELLES, 1990).…”
Section: Infravermelho Termalunclassified