1982
DOI: 10.1016/0038-092x(82)90245-6
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The thermal radiance of clear skies

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Cited by 257 publications
(124 citation statements)
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“…Emissivity formula was obtained by an approximate integration of the Schwartzschild's transfer equation for a standard atmosphere. 4) Berdahl and Martin (1984) (B&M) introduced some modifications to the formula developed by Berdahl and Fromberg (1982), based on the use of a more extensive dataset. Their final parameterisation was function of the dewpoint temperature, T d (°C).…”
Section: Clear Skiesmentioning
confidence: 99%
“…Emissivity formula was obtained by an approximate integration of the Schwartzschild's transfer equation for a standard atmosphere. 4) Berdahl and Martin (1984) (B&M) introduced some modifications to the formula developed by Berdahl and Fromberg (1982), based on the use of a more extensive dataset. Their final parameterisation was function of the dewpoint temperature, T d (°C).…”
Section: Clear Skiesmentioning
confidence: 99%
“…Whereas historically radiative cooling was largely developed for night-time applications (1)(2)(3)(4)(5)(6)(9)(10)(11)(12)(13), recent works have achieved daytime radiative cooling (7,14). In particular, it was shown that the radiative cooling to below ambient air temperature can be achieved (7), with a photonic structure that reflects almost all incident sunlight and simultaneously emits significant thermal radiation in the midinfrared.…”
mentioning
confidence: 99%
“…This limitation excludes pitched roofs and walls. The existing models (Berdahl and Fromberg, 1982;Idso and Jackson, 1969;Roach, 1955;Swinbank, 1963; Unsworth and Monteith, 1971) was empirically verified mostly for clear sky conditions, rather than for cloudy skies and different levels of air pollution. Cole (1976) proposed a simple empirical model for calculation cf longwave radiation incident on surfaces at all angles, from horizontal to vertical.…”
Section: Introductionmentioning
confidence: 91%