1981
DOI: 10.1016/0038-092x(81)90209-7
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Effect of atmospheric humidity on radiation cooling

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Cited by 43 publications
(19 citation statements)
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“…Brought to you by | MIT Libraries Authenticated Download Date | 5/9/18 9:30 AM transparency of the sky is quite sensitive to precipitable water vapor concentration, which is correlated with relative humidity (RH) and ground temperature [39,40], and thus varies geographically. Its influence is illustrated in Figure 2: higher precipitable water vapor concentration leads to stronger absorption within the atmospheric window.…”
Section: Tropospheric Temperature and Atmospheric Transmittancementioning
confidence: 99%
“…Brought to you by | MIT Libraries Authenticated Download Date | 5/9/18 9:30 AM transparency of the sky is quite sensitive to precipitable water vapor concentration, which is correlated with relative humidity (RH) and ground temperature [39,40], and thus varies geographically. Its influence is illustrated in Figure 2: higher precipitable water vapor concentration leads to stronger absorption within the atmospheric window.…”
Section: Tropospheric Temperature and Atmospheric Transmittancementioning
confidence: 99%
“…[36][37][38] For atmospheric radiation, the atmospheric constituents like H 2 O, CO 2 , O 3 , CH 4 , and N 2 O contribute; however, for transmission within the atmospheric window, the major role is played by the H 2 O content within the atmosphere. [ 38,39 ] The amount of the water vapor content in the atmosphere can be associated to ground surface temperature and relative humidity (RH) or dew point. [37][38][39] Here, we will briefl y discuss the variation of the atmospheric transmittance for different locations and estimate the cooling potential for variable RH, assuming cloud-free sky conditions.…”
Section: Effects Of Atmospheric Conditionsmentioning
confidence: 99%
“…[ 38,39 ] The amount of the water vapor content in the atmosphere can be associated to ground surface temperature and relative humidity (RH) or dew point. [37][38][39] Here, we will briefl y discuss the variation of the atmospheric transmittance for different locations and estimate the cooling potential for variable RH, assuming cloud-free sky conditions. Figure 4 a shows the modeled atmospheric transmittance [ 28 ] for the ambient temperatures and mean RH during the peak daytime (3 pm) at summer (January, 2015) in two mid-latitude locations in Australia.…”
Section: Effects Of Atmospheric Conditionsmentioning
confidence: 99%
“…This has already been discussed in various earlier reports. [49][50][51][52] To minimize the effects of incoming solar radiation, an IR transparent reflector needs to be integrated on the top side of the surface. Alternatively, a cooling device itself can be designed that possesses the capability to serve as both solar reflector and IR radiator simultaneously.…”
Section: Design Principle Of Passive Radiative Coolermentioning
confidence: 99%