scholarly journals RADIANT COOLING EFFECT OF CEILING SLIT CAPABLE OF BOTH DAYLIGHT HARVESTING AND SOLAR HEAT REMOVAL

2021 ◽  
Vol 86 (787) ◽  
pp. 788-796
Author(s):  
Kan SHINDO ◽  
Jun SHINODA ◽  
Ken IKAI ◽  
Takeshi TAKENAKA ◽  
Shuichi TAMURA ◽  
...  
Keyword(s):  
Heat Removal ◽  
Cooling Effect ◽  
Solar Heat ◽  
Radiant Cooling ◽  
Daylight Harvesting

A simplified model for the formation, movement, and dissipation of fair weather cumulus clouds

1965 ◽  
Vol 2 (1) ◽  
pp. 178-185
Author(s):  
Martin Fox
Keyword(s):  
Stochastic Model ◽  
Cloud Cover ◽  
Temporal Evolution ◽  
Cooling Effect ◽  
Simplified Model ◽  
Fair Weather ◽  
Cumulus Clouds ◽  
Solar Heat

Certain patches of ground are favorable to the formation of fair weather cumulus clouds. These are patches which reflect rather than absorb solar heat. As the air above these patches is warmed, it will rise and, if the humidity is sufficient, the cooling effect of higher elevation will cause formation of a cloud of the type known as the fair weather cumulus. This fact is used in the present paper to develop a stochastic model for the temporal evolution of the contribution to cloud cover by fair weather cumuli.

Synthesis of solar heat-reflective ZnTiO3 pigments with novel roof cooling effect

2019 ◽  
Vol 45 (12) ◽  
pp. 15768-15771 ◽  
Author(s):  
Jinpeng Lv ◽  
Mingzhang Tang ◽  
Ronghui Quan ◽  
Ziyi Chai
Keyword(s):  
Cooling Effect ◽  
Solar Heat

A simplified model for the formation, movement, and dissipation of fair weather cumulus clouds

1965 ◽  
Vol 2 (01) ◽  
pp. 178-185
Author(s):  
Martin Fox
Keyword(s):  
Stochastic Model ◽  
Cloud Cover ◽  
Temporal Evolution ◽  
Cooling Effect ◽  
Simplified Model ◽  
Fair Weather ◽  
Cumulus Clouds ◽  
Solar Heat

Certain patches of ground are favorable to the formation of fair weather cumulus clouds. These are patches which reflect rather than absorb solar heat. As the air above these patches is warmed, it will rise and, if the humidity is sufficient, the cooling effect of higher elevation will cause formation of a cloud of the type known as the fair weather cumulus. This fact is used in the present paper to develop a stochastic model for the temporal evolution of the contribution to cloud cover by fair weather cumuli.

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