1966
DOI: 10.1364/ao.5.000919
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Overcast Sky Luminances and Directional Luminous Reflectances of Objects and Backgrounds under Overcast Skies

Abstract: Two sky luminance distributions are given for overcast sky above snow-covered terrain, and directional luminous reflectance data are presented which were obtained under these skies. Luminous reflectances computed from Krinov spectral reflectance data for a variety of natural terrains measured under overcast are also included.

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Cited by 17 publications
(6 citation statements)
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“…1. The sky is assumed to be mostly cloudy or overcast and that the radiance from the sky varies smoothly with respect to the polar and azimuth angles of the hemisphere [8], [11], [20]. For more details, we refer the reader to [21].…”
Section: Attenuation and Airlightmentioning
confidence: 99%
“…1. The sky is assumed to be mostly cloudy or overcast and that the radiance from the sky varies smoothly with respect to the polar and azimuth angles of the hemisphere [8], [11], [20]. For more details, we refer the reader to [21].…”
Section: Attenuation and Airlightmentioning
confidence: 99%
“…Daylight spectrum has also been represented using a set of linear bases [25]. Works that model clouds and their effect on the ambient illumination also exist in literature [26,27]. In graphics, scenes have been rendered under different daylight [28] and night illuminations [29].…”
Section: Variation In Illuminationmentioning
confidence: 99%
“…Yet doubts persist about it, ranging from suggestions that thick overcasts have nearly uniform luminances [14], to observations that some overcasts' brightness maxima are in fact not at the zenith [15][16][17], to an empirical model that predicts some slight zenith asymmetry even for thick overcasts [18,19]. More recently, the CIE has incorporated some of the asymmetry from [18] to allow for brightness maxima around the Sun in optically thin overcasts [20], as do several other empirical models [21][22][23].…”
Section: Introductionmentioning
confidence: 99%