• Thumbnail for Radiative forcing
    Radiative forcing (or climate forcing) is a concept used in climate science to quantify the change in energy balance in Earth's atmosphere. Various factors...
    69 KB (7,011 words) - 20:29, 5 October 2024
  • Thumbnail for Cloud feedback
    cloud-free conditions, is described as cloud forcing, cloud radiative forcing (CRF) or cloud radiative effect (CRE) At the top of the atmosphere, it...
    45 KB (4,868 words) - 14:16, 18 September 2024
  • Thumbnail for Climate sensitivity
    by smaller forcing values. Forcings from such investigations have also been analyzed and reported at decadal time scales. Radiative forcing leads to long-term...
    100 KB (10,694 words) - 20:45, 17 August 2024
  • Thumbnail for Global warming potential
    Global warming potential (category Climate forcing)
    greenhouse gas lifetimes, radiative efficiencies and metrics (PDF), IPCC, 2021, p. 7SM-24. National Research Council (2005). Radiative Forcing of Climate Change:...
    52 KB (4,684 words) - 20:24, 5 October 2024
  • Thumbnail for Atmospheric methane
    : 82  Methane's radiative forcing (RF) of climate is direct,: 2  and it is the second largest contributor to human-caused climate forcing in the historical...
    54 KB (5,808 words) - 20:33, 5 October 2024
  • Contrail (category Climate forcing)
    reflect incoming solar radiation, resulting in a net increase in radiative forcing. In 1992, this warming effect was estimated between 3.5 mW/m2 and...
    32 KB (3,197 words) - 17:05, 27 September 2024
  • Thumbnail for Greenhouse gas
    Greenhouse gas (category Climate forcing)
    radiation with the surface and limit radiative heat flow away from it, which reduces the overall rate of upward radiative heat transfer.: 139  The increased...
    75 KB (7,979 words) - 20:31, 5 October 2024
  • Thumbnail for Environmental impact of aviation
    understanding, nitrogen oxides, contrails and particulates. Their radiative forcing is estimated at 1.3–1.4 that of CO2 alone, excluding induced cirrus...
    119 KB (11,764 words) - 05:01, 2 October 2024
  • Thumbnail for Earth's energy budget
    multi-layered atmosphere is governed by radiative transfer equations such as Schwarzschild's equation for radiative transfer (or more complex equations if...
    57 KB (5,983 words) - 21:00, 12 August 2024
  • Thumbnail for Sulfate
    Winker, D.; Stevens, B. (1 November 2019). "Bounding Global Aerosol Radiative Forcing of Climate Change". Reviews of Geophysics. 58 (1): e2019RG000660....
    17 KB (4,498 words) - 17:55, 8 July 2024
  • increase in GHGs will slow down the rate of radiative cooling to space, i.e. produce a radiative forcing until a saturation point is reached. At steady...
    29 KB (3,902 words) - 04:16, 7 September 2024
  • Thumbnail for Black carbon
    Black carbon (category Climate forcing)
    averaged radiative forcing after carbon dioxide (CO2), and that the radiative forcing of black carbon is "as much as 55% of the CO2 forcing and is larger...
    100 KB (12,022 words) - 20:05, 4 October 2024
  • Thumbnail for Monte Carlo method
    on Monte Carlo methods in probability density function analysis of radiative forcing. Monte Carlo methods are used in various fields of computational biology...
    91 KB (10,518 words) - 18:18, 3 October 2024
  • season Radiative forcing, the difference between the incoming radiation energy and the outgoing radiation energy in a given climate system Forcing (magic)...
    1 KB (203 words) - 06:47, 19 August 2024
  • Thumbnail for IPCC Third Assessment Report
    short-lived and mostly produce negative radiative forcing; Natural factors have made small contributions to radiative forcing over the past century) Confidence...
    60 KB (5,740 words) - 13:23, 29 August 2024
  • Thumbnail for Ozone depletion
    have produced 0.34 ± 0.03 W/m2 of radiative forcing, corresponding to about 14 percent of the total radiative forcing from increases in the concentrations...
    137 KB (15,879 words) - 17:50, 2 October 2024
  • Earth's surface. Ozone depletion in the stratopshere has had a negative radiative forcing impact, however anthropogenic increases in the tropospheric abundance...
    40 KB (4,517 words) - 07:18, 2 October 2024
  • Thumbnail for 1,1-Difluoroethane
    1-Difluoroethane at Sigma-Aldrich "Changes in Atmospheric Constituents and in Radiative Forcing" (PDF). Cambridge University Press. 2007. p. 212. Retrieved 11 May...
    12 KB (1,030 words) - 09:42, 18 September 2024
  • Thumbnail for Representative Concentration Pathway
    RCP4.5, RCP6, and RCP8.5 – are labelled after a possible range of radiative forcing values in the year 2100 (2.6, 4.5, 6, and 8.5 W/m2, respectively)...
    22 KB (2,388 words) - 07:23, 15 August 2024
  • Thumbnail for Greenhouse effect
    Greenhouse effect (category Climate forcing)
    energy flows reduce radiative surface cooling (net upward radiative energy flow). Latent heat transport and thermals provide non-radiative surface cooling...
    84 KB (8,956 words) - 10:45, 25 September 2024
  • daytime radiative cooling (PDRC) (also passive radiative cooling, daytime passive radiative cooling, radiative sky cooling, photonic radiative cooling...
    22 KB (3,666 words) - 02:34, 20 August 2024
  • Thumbnail for Particulates
    Particulates (category Climate forcing)
    direct radiative forcing of atmospheric black carbon is +0.71 W/m2 with 90% uncertainty bounds of (+0.08, +1.27) W/m2" with "total direct forcing by all-black...
    197 KB (19,321 words) - 22:30, 5 October 2024
  • gases over the past several decades contributes more than 10% of the radiative forcing which drives global climate change as of year 2020. Moreover, the...
    11 KB (2,265 words) - 20:56, 14 January 2024
  • or decrease the warming that eventually results from a change in radiative forcing. climate change mitigation approaches to limit global warming, primarily...
    28 KB (3,224 words) - 05:24, 12 May 2024
  • Thumbnail for Causes of climate change
    activities can also impose forcings, for example, through changing the composition of Earth's atmosphere. Radiative forcing is a measure of how various...
    89 KB (7,973 words) - 20:13, 5 October 2024
  • Thumbnail for Ice–albedo feedback
    0.21 watts per square meter (W/m2) of radiative forcing, which is equivalent to a quarter of radiative forcing from CO2 increases over the same period...
    29 KB (3,514 words) - 03:24, 29 September 2024
  • Thumbnail for Natural gas
    period. Natural gas is thus a potent greenhouse gas due to the strong radiative forcing of methane in the short term, and the continuing effects of carbon...
    105 KB (11,480 words) - 20:26, 5 October 2024
  • Thumbnail for Climate change
    sunlight. Indirect effects of aerosols are the largest uncertainty in radiative forcing. While aerosols typically limit global warming by reflecting sunlight...
    315 KB (28,055 words) - 17:45, 3 October 2024
  • Thumbnail for Methane
    percentage caused by human activity. It accounted for 20% of the total radiative forcing from all of the long-lived and globally mixed greenhouse gases, according...
    90 KB (8,771 words) - 16:01, 30 September 2024
  • function, erf Exponential response formula Effective radiative forcing, a concept to compare radiative forcing in climate models ERF (gene), coding for ETS domain-containing...
    1 KB (161 words) - 17:26, 8 August 2024