1968
DOI: 10.2172/12817537
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Directional Effects in Radiant Heat Transfer Between Pairs of Simply Arranged Surfaces

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Cited by 4 publications
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“…7, where h » R, then (12) where a = the earth albedo ~ 0.4 E s = the solar illuminance c^ 203.8 lightwatts/m 2 R = the radius of the earth h = the altitude above earth surface a = the phase angle Eclipsing Any computation of illumination in the near vicinity of the moon must account for the possibility that on occasion one or more sources may be behind the moon relative to the spacecraft. For this reason, special logic has been included in the program to account for the moon as an eclipsing body.…”
Section: Light Sourcesmentioning
confidence: 99%
“…7, where h » R, then (12) where a = the earth albedo ~ 0.4 E s = the solar illuminance c^ 203.8 lightwatts/m 2 R = the radius of the earth h = the altitude above earth surface a = the phase angle Eclipsing Any computation of illumination in the near vicinity of the moon must account for the possibility that on occasion one or more sources may be behind the moon relative to the spacecraft. For this reason, special logic has been included in the program to account for the moon as an eclipsing body.…”
Section: Light Sourcesmentioning
confidence: 99%