An Introduction to Solar Radiation 1983
DOI: 10.1016/b978-0-12-373750-2.50009-4
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Extraterrestrial Solar Irradiation

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Cited by 186 publications
(192 citation statements)
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“…Based on the month and day of the year, the number of days n elapsed until the day and time of measurement made by the pyranometer was determined, using the formulas provided in Table 2. First, the given declination in degrees equation ( 1) was calculated (Duffie & Beckman, 1991;Iqbal, 1983) Here the number of days n for each type of month day of the year was determined from Table 2.…”
Section: Clear Index Determination Proceduresmentioning
confidence: 99%
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“…Based on the month and day of the year, the number of days n elapsed until the day and time of measurement made by the pyranometer was determined, using the formulas provided in Table 2. First, the given declination in degrees equation ( 1) was calculated (Duffie & Beckman, 1991;Iqbal, 1983) Here the number of days n for each type of month day of the year was determined from Table 2.…”
Section: Clear Index Determination Proceduresmentioning
confidence: 99%
“…Knowing the solar constant G sc and the latitude ϕ for the location of each station, the hour angle ω s was determined by the equation ( 2) (Belúcio, et al, 2014;Duffie & Beckman, 1991;Iqbal, 1983;Kumar, 2016) For Vianello and Alves, 1991, considering the chronological time variable H, which varies from 0 to 24 hours (in degrees), the hour angle w s , in the morning and ws<0; at noon w s =0 and in the afternoon ws>0, such that, after calculating the hour angle, taking into account the time (local time converted to solar). Having first, treating the measurement hour with a time interval of 1 (one) and 10 (ten) minutes, that is, minute by minute, then transforming the hour angle into degrees, a worse result was obtained equation ( 3).…”
Section: Clear Index Determination Proceduresmentioning
confidence: 99%
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“…where Eb = direct radiation intensity (measured perpendicular to the sun) Ed = diffuse radiation intensity value (measured on a horizontal surface) E0 = Extraterrestrial Orthogonal Intensity [6] m = air mass [7] , b d τ τ = Beam and diffuse optical depths, which depend on the terrain of the area and vary during the year and an average can be obtained from ASHRAE RP-1453 [8].…”
Section: Clear-sky Solar Radiationmentioning
confidence: 99%
“…When the measurement of solar radiation is unavailable, the theoretical radiations can be assumed according to the location and configurations of the bridge following the clear-sky model presented by the American Society of Heating, Refrigerating and Air-Conditioning Engineers (ASHRAE, 2021) or similar variants (Chow et al, 2005;Iqbal, 2012;Sousa Tomé et al, 2018).…”
mentioning
confidence: 99%