2004
DOI: 10.1016/j.rse.2004.03.002
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Simplified atmospheric radiative transfer modelling for estimating incident PAR using MODIS atmosphere products

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Cited by 89 publications
(43 citation statements)
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“…While the extraterrestrial radiation budget and its wavelength distribution are well known and relatively constant, the terrestrial reception of PAR is altered by a dynamically changing atmosphere (Van Laake and Sanchez-Azofeifa, 2004). Atmospheric radiative transfer is driven by absorption, molecular (Raleigh) and particle (Mie) scattering effects attenuating the amount of solar radiation received by the earth surface (Szeicz, 1974;B C A Rao, 1984;Baker and Frouin, 1987).…”
Section: Photosynthetically Active Radiationmentioning
confidence: 99%
See 1 more Smart Citation
“…While the extraterrestrial radiation budget and its wavelength distribution are well known and relatively constant, the terrestrial reception of PAR is altered by a dynamically changing atmosphere (Van Laake and Sanchez-Azofeifa, 2004). Atmospheric radiative transfer is driven by absorption, molecular (Raleigh) and particle (Mie) scattering effects attenuating the amount of solar radiation received by the earth surface (Szeicz, 1974;B C A Rao, 1984;Baker and Frouin, 1987).…”
Section: Photosynthetically Active Radiationmentioning
confidence: 99%
“…The MODIS Atmospheric Profile products (MOD04-MOD07) consist of total-ozone burden, atmospheric stability, temperature and moisture profiles, and atmospheric water vapour, measured on a daily basis. Even though the atmospheric interactions of solar irradiance are well understood, a standardized product providing regular observations of global PAR is currently not available (Liang et al, 2006), however, techniques to derive accurate estimates of global PAR using MODIS have been developed (Van Laake and Sanchez-Azofeifa, 2004;Liang et al 2006).…”
Section: Photosynthetically Active Radiationmentioning
confidence: 99%
“…In order for the methodology to be used on an operational basis, these parameters have to be available from satellite at the same resolution as the VIs and FAPAR. Sanchez-Azofeifa (2004, 2005) presented a method which gives incident PAR by implementation of a simple radiative transfer model where the amount of PAR is a function of the solar constant, solar zenith angle and the atmospheric transmittance, which in turn is cal- culated using daily atmospheric data from the MODIS sensor onboard the NASA platforms Terra and Aqua. implemented the method for Scandinavian conditions and found that five day averages of PAR could be operationally obtained with an r 2 of 83% at Norunda and 74% at Asa.…”
Section: Operational Remote Sensing Of Apar and Atmentioning
confidence: 99%
“…Therefore, they are important variables in vegetation dynamics and climate change modelling [1,2], as well as key indicators of drought [3]. The solar radiation budget, also called net solar radiation, is defined as the difference between incident and reflected shortwave radiative fluxes at the Earth's surface [4].…”
Section: Introductionmentioning
confidence: 99%