Editing Humidity (section)

=== Global climate ===
{{See also|Greenhouse effect}}
Humidity affects the [[energy budget]] and thereby influences temperatures in two major ways. First, water vapor in the atmosphere contains "latent" energy. During transpiration or evaporation, this [[latent heat]] is removed from surface liquid, cooling the Earth's surface. This is the biggest non-radiative cooling effect at the surface. It compensates for roughly 70% of the average net radiative warming at the surface.

Second, water vapor is the most abundant of all [[greenhouse gases]]. Water vapor, like a green lens that allows green light to pass through it but absorbs red light, is a "selective absorber". Like the other greenhouse gasses, water vapor is transparent to most solar energy. However, it absorbs the infrared energy emitted (radiated) upward by the Earth's surface, which is the reason that humid areas experience very little nocturnal cooling but dry desert regions cool considerably at night. This selective absorption causes the greenhouse effect. It raises the surface temperature substantially above its theoretical radiative equilibrium temperature with the sun, and water vapor is the cause of more of this warming than any other greenhouse gas.

Unlike most other greenhouse gases, however, water is not merely below its boiling point in all regions of the Earth, but below its freezing point at many altitudes.  As a condensible greenhouse gas, it [[Precipitation|precipitates]], with a much lower [[scale height]] and shorter atmospheric lifetime — weeks instead of decades.  Without other greenhouse gases, Earth's [[blackbody temperature]], below the freezing point of water, would cause water vapor to be removed from the atmosphere.<ref>{{cite web |url=http://www.saga.iao.ru/glossary/?catalog=9&sowa=All&term=@1621 |title=Blackbody Radiation |access-date=2015-01-11 |archive-date=2020-08-14 |archive-url=https://web.archive.org/web/20200814131004/http://www.saga.iao.ru/glossary/?catalog=9&sowa=All&term=@1621 |url-status=live }}</ref><ref>{{cite web |url=http://www.physics.rutgers.edu/~abragg/109/L14.html |title=Lecture notes |access-date=2015-01-11 |archive-date=2017-10-23 |archive-url=https://web.archive.org/web/20171023010911/http://www.physics.rutgers.edu/~abragg/109/L14.html |url-status=dead }}</ref><ref>{{cite web |url=http://storm.colorado.edu//~toohey/lecture8.html |title=Radiative Balance, Earth's Temperature, and Greenhouse Gases (lecture notes) |access-date=2015-01-11 |archive-date=2016-03-04 |archive-url=https://web.archive.org/web/20160304085052/http://storm.colorado.edu//~toohey/lecture8.html |url-status=live }}</ref>  Water vapor is thus a "slave" to the non-condensible greenhouse gases.<ref>{{cite web | url=https://www.e-education.psu.edu/geosc10/l12_p7.html | title=GEOSC 10 Optional Enrichment Article 1 | author=Alley, R. | date=2014 | access-date=2015-01-11 | archive-date=2018-09-08 | archive-url=https://web.archive.org/web/20180908115943/https://www.e-education.psu.edu/geosc10/l12_p7.html | url-status=dead }}</ref><ref>{{cite web|url=http://www.soest.hawaii.edu/MET/Faculty/businger/courses/notes101/28ModelingClimate.pdf |title=Lecture 28: Future Global Warming Modeling Climate Change |author=Businger, S. |url-status=dead |archive-url=https://web.archive.org/web/20150130212102/http://www.soest.hawaii.edu/MET/Faculty/businger/courses/notes101/28ModelingClimate.pdf |archive-date=2015-01-30 }}</ref><ref>{{cite web | url=http://www.astro.washington.edu/users/eschwiet/essays/greenhouse_ASTR555.pdf | title=Comparing the Greenhouse Effect on Earth, Mars, Venus, and Titan: Present Day and through Time | author=Schwieterman, E. | access-date=2015-01-11 | archive-date=2015-09-23 | archive-url=https://web.archive.org/web/20150923175539/http://www.astro.washington.edu/users/eschwiet/essays/greenhouse_ASTR555.pdf | url-status=dead }}</ref>