radiative$66418$ - ορισμός. Τι είναι το radiative$66418$
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Τι (ποιος) είναι radiative$66418$ - ορισμός

ENERGY TRANSFER THROUGH A MEDIUM THROUGH EMISSION AND ABSORPTION OF ELECTROMAGNETIC RADIATION
Equation of radiative transfer; Radiative Transfer; Radiative transfer equation; Radiative transport; Radiation transport

Passive daytime radiative cooling         
  • doi-access=free }}</ref>
  • Broadband PDRC emitters emit in both the solar spectrum and the infrared window (8 and 14 μm), while selective PDRC emitters only emit in the infrared window.<ref name=":54" />
  • [[Desert climate]]s have the highest radiative cooling potential due to low humidity and cloud cover.<ref name=":21" />
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  • 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" />
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  • Global map of cloud cover. Data taken from 2002 to 2015. The darker the color, the clearer the sky.
  • [[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"/>
  • outgoing infrared radiation]] (shown in orange) and minimize the absorption of [[Solar Radiation]] (shown in yellow).
  • 228x228px
  • 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.
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         
  • Measured global albedo anomaly from CERES (2000-2011).
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  • Planck curves]].
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  • 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.
  • alt=Line graph showing historical sunspot number count, Maunder and Dalton minima, and the Modern Maximum
  • CO<sub>2</sub>, temperature, and sunspot activity since 1850.
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.
Radiative transfer         
Radiative transfer is the physical phenomenon of energy transfer in the form of electromagnetic radiation. The propagation of radiation through a medium is affected by absorption, emission, and scattering processes.

Βικιπαίδεια

Radiative transfer

Radiative transfer (also called radiation transport) is the physical phenomenon of energy transfer in the form of electromagnetic radiation. The propagation of radiation through a medium is affected by absorption, emission, and scattering processes. The equation of radiative transfer describes these interactions mathematically. Equations of radiative transfer have application in a wide variety of subjects including optics, astrophysics, atmospheric science, and remote sensing. Analytic solutions to the radiative transfer equation (RTE) exist for simple cases but for more realistic media, with complex multiple scattering effects, numerical methods are required. The present article is largely focused on the condition of radiative equilibrium.