1986
DOI: 10.1175/1520-0450(1986)025<0087:sssmfd>2.0.co;2
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Simple Solar Spectral Model for Direct and Diffuse Irradiance on Horizontal and Tilted Planes at the Earth's Surface for Cloudless Atmospheres

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Cited by 706 publications
(327 citation statements)
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“…The transmission model SPCTRAL2 [43] was used to simulate the solar spectra in different seasons, namely the summer (21 June), autumn (18 October) and winter (21 December) at noon of the given days. The incident surface was defined by coordinates of 52.00°N 4.37°E (Delft, The Netherlands), tilt angle of 37.0°, and azimuth angle of 180° (South).…”
Section: Variations In Photocurrent Generationmentioning
confidence: 99%
“…The transmission model SPCTRAL2 [43] was used to simulate the solar spectra in different seasons, namely the summer (21 June), autumn (18 October) and winter (21 December) at noon of the given days. The incident surface was defined by coordinates of 52.00°N 4.37°E (Delft, The Netherlands), tilt angle of 37.0°, and azimuth angle of 180° (South).…”
Section: Variations In Photocurrent Generationmentioning
confidence: 99%
“…The position and irradiation of the sun are modeled 1.0 with SOLPOS [55] and SPTRL2 [56,57]. Several threshold angles and energies, tracking modes as well as solar absorber thicknesses are considered.…”
Section: Annual Yield For Directionally Selective Solar Absorbersmentioning
confidence: 99%
“…The basic equation describing the amount of direct solar ultraviolet radiation propagating through the atmosphere and reaching the ground, is given in Bird and Riordan (1986) Z(dh) = H(oh) * D * 7(rh) * 7(d) * 7(Wh) * 7(0/i) * 7(Uh) )…”
Section: Directnormal Irradiancementioning
confidence: 99%
“…Values for the extra-terrestrial solar radiation are for the spectral region from 280 to 400 nm. These values were derived following Bird and Riordan (1986) calculations and the formulation from Green (1983).…”
Section: Directnormal Irradiancementioning
confidence: 99%
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