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A newly designed optical system enabled oblique irradiation of high irradiance from any direction of incidence.
The isotropic sky model assumes a uniform distribution of diffuse irradiance from the sky.
Figure 11 shows the simulation results under varying irradiance from 100%to50%0%.
Traditional adaptations of tropical/sub tropical buildings to high ambient irradiance from high elevations are outlined.
The SOLSPEC instrument measures the absolute solar spectral irradiance from 200 to 2500 nm.
Figure 1 Annual average daily global horizontal irradiance from year 1955 to 2004, London International Airport, in W/m 2, data courtesy of Environment Canada CWEEDS.
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The DIRINDEX model was designed to estimate hourly solar beam irradiances from hourly global horizontal irradiances.
Significant differences in ETR values were obtained among leaves grown under different grown irradiances from PPFD of 605 to 1585 µmol m−2 s−1 (p < 0.05).
Different radiation sources and measurement devices were tested to illustrate the problem of incomparability of measured irradiances from different laboratories around Europe.
The large Earth-Sun-Mars angle during the extended mission (∼130°, in contrast to ∼40° during the primary mission) and the consequent errors in adjusting solar irradiances from Earth to Mars may be responsible.
The good agreement of the EUVAC and SEE derived photoelectron fluxes with the FAST measured fluxes at solar maximum lends support to an earlier finding that the previous reference solar EUV irradiances from the Atmosphere Explorer measurements need to be adjusted upward by a factor of 2 3 below 25 nm wavelength.
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