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  2. Greenhouse effect - Wikipedia

    en.wikipedia.org/wiki/Greenhouse_effect

    Most gases whose molecules have two different atoms (such as carbon monoxide, CO), and all gases with three or more atoms (including H 2 O and CO 2), are infrared active and act as greenhouse gases. (Technically, this is because when these molecules vibrate , those vibrations modify the molecular dipole moment , or asymmetry in the distribution ...

  3. Greenhouse gas - Wikipedia

    en.wikipedia.org/wiki/Greenhouse_gas

    Greenhouse gases are infrared active, meaning that they absorb and emit infrared radiation in the same long wavelength range as what is emitted by the Earth's surface, clouds and atmosphere. [19]: 2233 99% of the Earth's dry atmosphere (excluding water vapor) is made up of nitrogen (N 2) (78%) and oxygen (O 2) (21%).

  4. Illustrative model of greenhouse effect on climate change

    en.wikipedia.org/wiki/Illustrative_model_of...

    An exact calculation using the MODTRAN model, over all wavelengths and including methane and ozone greenhouse gasses, as shown in the plot above, gives, for tropical latitudes, an outgoing flux = 298.645 W/m 2 for current CO 2 levels and = 295.286 W/m 2 after CO 2 doubling, i.e. a radiative forcing of 1.1%, under clear sky conditions, as well ...

  5. Water vapor windows - Wikipedia

    en.wikipedia.org/wiki/Water_vapor_windows

    Water vapor is a gas that absorbs many wavelengths of Infrared (IR) energy in the Earth's atmosphere, and these wavelength ranges that can partially reach the surface are coming through what is called 'water vapor windows'.

  6. Atmospheric window - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_window

    The individual absorption spectra of major greenhouse gases plus Rayleigh scattering are shown in the lower panel. [1] An atmospheric window is a region of the electromagnetic spectrum that can pass through the atmosphere of Earth. The optical, infrared and radio windows comprise the three main atmospheric windows. [2]

  7. Carbon dioxide - Wikipedia

    en.wikipedia.org/wiki/Carbon_dioxide

    Carbon dioxide is a greenhouse gas. It absorbs and emits infrared radiation at its two infrared-active vibrational frequencies. The two wavelengths are 4.26 μm (2,347 cm −1) (asymmetric stretching vibrational mode) and 14.99 μm (667 cm −1) (bending vibrational mode).

  8. Trace gas - Wikipedia

    en.wikipedia.org/wiki/Trace_gas

    A few examples of the major greenhouse gases are water, carbon dioxide, methane, nitrous oxide, ozone, and CFCs. These gases can absorb infrared radiation from the Earth's surface as it passes through the atmosphere. The most influential greenhouse gas is water vapor. It frequently occurs in high concentrations, may transition to and from an ...

  9. Infrared window - Wikipedia

    en.wikipedia.org/wiki/Infrared_window

    The infrared atmospheric window is an atmospheric window in the infrared spectrum where there is relatively little absorption of terrestrial thermal radiation by atmospheric gases. [1] The window plays an important role in the atmospheric greenhouse effect by maintaining the balance between incoming solar radiation and outgoing IR to space.