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Greenhouse gas

Greenhouse gasesgaseous components ofatmosphere that contribute togreenhouse effect (see also global warming). The major natural greenhouse gaseswater vapor, which causes most (about 60%) ofgreenhouse effect on Earth, carbon dioxide (about 26%),ozone. The remaining fractioncaused by minor greenhouse gases which include methanenitrous oxide. Industrial greenhouse gases includeheavy halocarbons (chlorinated fluorocarbons), CFC, HCFC-22 molecules such as freonperfluoromethane,sulphur hexafluoride (SF6).

Greenhouse gasestransparentcertain wavelengths ofsun's radiant energy, allowing thempenetrate deep intoatmosphere or allway toEarth's surface, where theyre-emitted as longer wavelength radiation (chiefly infrared radiation}. Greenhouse gasesclouds prevent somethis radiation from escaping, trappingheat nearEarth's surface wherewarmslower atmosphere. Alterationthis natural barrieratmospheric gases can raise or lowermean global temperature ofEarth.

The concentrationsseveral greenhouse gases have increased over time duehuman activities, such as:

According toglobal warming hypothesis, greenhouse gases from industryagriculturepartly or whollyblameglobal warming. Carbon dioxide issubject ofproposed Kyoto Protocol. Nitrous oxidemethanealso taken into account ininternational agreements, but not ozone.

At least one IPCC TAR chapter lead author considers mention ofeffectwater vapor uponEarth's greenhouse effectbe misleading as water vapor can not be controlled by humans.

Increasegreenhouse gases inatmosphere

Sincebeginning ofIndustrial Revolution,concentrationsmany ofgreenhouse gases have increased. (Source: IPCC radiative forcing report -- 1994 -- ppvb : part per billionvolume)

Durationstayglobal warming potential

The greenhouse gases, once inatmosphere, do not remain there eternally. They can be withdrawn fromatmosphere: The lifetimean individual moleculegas inatmospherefrequently much shorter thanlifetime ofconcentration anomalythat gas. Thus, becauselarge (balanced) natural fluxesand frombiosphereocean surface layer, an individual CO2 molecule may last onlyfew years inair, on average; however,calculated lifetimean increaseatmospheric CO2 levelhundredsyears.

Aside from water vapour nearsurface, whichhasresidence timefew days,greenhouse gases takeverytimeleaveatmosphere. Itnot easyknowprecision how longnecessary, becauseatmosphere isvery complex system. However, thereestimates ofdurationstay, i.e.time whichnecessary so thatgas disappears fromatmosphere, forprincipal ones.

Durationstaywarming capability ofdifferent greenhouse gases can be compared:

Source : GIEC

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