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What (who) is RADIATIVE - definition
Radiative
·adj Capable of radiating; acting by radiation.
Passive daytime radiative cooling
![[[Desert climate]]s have the highest radiative cooling potential due to low humidity and cloud cover.<ref name=":21" />](https://commons.wikimedia.org/wiki/Special:FilePath/BW climate.png?width=200 "[[Desert climate]]s have the highest radiative cooling potential due to low humidity and cloud cover.<ref name=\":21\" />")
 oxide 2.jpg?width=200 "220x220px")
![A PDRC installed on a roof in [[Kolkata]] exhibited a nearly 4.9ᵒC decrease in surface ground temperatures (with an average reduction of 2.2ᵒC).<ref name=":13" />](https://commons.wikimedia.org/wiki/Special:FilePath/Buildings in Kolkata.jpg?width=200 "A PDRC installed on a roof in [[Kolkata]] exhibited a nearly 4.9ᵒC decrease in surface ground temperatures (with an average reduction of 2.2ᵒC).<ref name=\":13\" />")
![[[Temperate climate]]s have a moderate to high radiative cooling potential.<ref name=":21" />](https://commons.wikimedia.org/wiki/Special:FilePath/Koppen-Geiger Map C present.svg?width=200 "[[Temperate climate]]s have a moderate to high radiative cooling potential.<ref name=\":21\" />")
![[[Solar cell efficiency]] can be improved with PDRC application to reduce overheating and degradation of cells.<ref name="Heo 2022 Ju lee"/>](https://commons.wikimedia.org/wiki/Special:FilePath/Silicon heterojunction solar cell.jpg?width=200 "[[Solar cell efficiency]] can be improved with PDRC application to reduce overheating and degradation of cells.<ref name=\"Heo 2022 Ju lee\"/>")
![outgoing infrared radiation]] (shown in orange) and minimize the absorption of [[Solar Radiation]] (shown in yellow).](https://commons.wikimedia.org/wiki/Special:FilePath/The-NASA-Earth's-Energy-Budget-Poster-Radiant-Energy-System-satellite-infrared-radiation-fluxes.jpg?width=200 "outgoing infrared radiation]] (shown in orange) and minimize the absorption of [[Solar Radiation]] (shown in yellow).")
![Modifying PDRCs with [[vanadium dioxide]] (pictured) can achieve temperature-based 'switching' from cooling to heating to mitigate the "overcooling" effect.<ref name=":54" />](https://commons.wikimedia.org/wiki/Special:FilePath/VO2 crystal.jpg?width=200 "Modifying PDRCs with [[vanadium dioxide]] (pictured) can achieve temperature-based 'switching' from cooling to heating to mitigate the \"overcooling\" effect.<ref name=\":54\" />")
![Global map of average [[annual precipitation]]. The darker the color, the higher the precipitation.](https://commons.wikimedia.org/wiki/Special:FilePath/World precip annual.png?width=200 "Global map of average [[annual precipitation]]. The darker the color, the higher the precipitation.")
MANAGEMENT STRATEGY FOR GLOBAL WARMING
Passive radiative cooling; Daytime passive radiative cooling; Daytime radiative cooling
Passive daytime radiative cooling (PDRC), passive radiative cooling (PRC), or terrestrial radiative cooling is a solar radiation management strategy that has been proposed as a solution to global warming which involves the mass installation of sky-facing surfaces on Earth that reflect heat to outer space to reverse local and global temperature increases while requiring zero energy consumption or pollution. Because all materials in nature absorb more heat during the day than at night, PDRC surfaces are designed to maximize the efficiency of both solar reflectance (in 0.
Radiative forcing
![Planck curves]].](https://commons.wikimedia.org/wiki/Special:FilePath/ModtranRadiativeForcingDoubleCO2.png?width=200 "Planck curves]].")
![alt=Warming contributions of various GHGs, agents, factors [name the year that the contributions pertain to] [*correct reference given under the 'Talk' tab*]. Plus, the figure is inaccurate; at least wrt. to methane.](https://commons.wikimedia.org/wiki/Special:FilePath/Physical Drivers of climate change.svg?width=200 "alt=Warming contributions of various GHGs, agents, factors [name the year that the contributions pertain to] [*correct reference given under the 'Talk' tab*]. Plus, the figure is inaccurate; at least wrt. to methane.")
THE DIFFERENCE BETWEEN THE INCOMING RADIATION ENERGY AND THE OUTGOING RADIATION ENERGY IN A GIVEN CLIMATE SYSTEM
Solar forcing; Radiative efficiency; Radiative forcing (Calculation and Measurement); Radiative Forcing; Radiative forcings
Radiative forcing (or climate forcing) is the change in energy flux in the atmosphere caused by natural or anthropogenic factors of climate change as measured by watts / metre2. It is a scientific concept used to quantify and compare the external drivers of change to Earth's energy balance.
Examples of use of RADIATIVE
1. Most of the increase in radiative forcing measured since 1''0 is due to CO2, which now accounts for about 62 percent of the radiative forcing by all long–lived greenhouse gases.
2. Most of the increase in radiative forcing measured since 1''0 is due to carbon dioxide, which now accounts for about 62 percent of the radiative forcing by all long–lived greenhouse gases.
3. Positive radiative forcing tends to warm the surface of the Earth, and negative forcing tends to cool the surface.
4. Its focus is on the crucial role of clouds and their influence on radiative feedback processes in the atmosphere.
5. Radiative forcing is the change in the balance between solar radiation coming into the atmosphere and Earth‘s radiation going out.