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*{{cite book|author=F.K. Lutgens and E.J.Tarbuck|title=The Atmosphere: A Introduction to Meteorology|edition=5th Edition|publisher=Prentice Hall|

*{{cite book|author=F.K. Lutgens and E.J.Tarbuck|title=The Atmosphere: A Introduction to Meteorology|edition=5th Edition|publisher=Prentice Hall|

*{{cite book|author=F.K. Lutgens and E.J.Tarbuck|title=The Atmosphere: A Introduction to Meteorology|edition=5th Edition|publisher=Prentice Hall|

*{{cite book|author=F.K. Lutgens and E.J.Tarbuck|title=The Atmosphere: A Introduction to Meteorology|edition=5th Edition|publisher=Prentice Hall|

*{{cite book|author=F.K. Lutgens and E.J.Tarbuck|title=The Atmosphere: A Introduction to Meteorology|edition=5th Edition|publisher=Prentice Hall|

...r (H₂O) and accounts for 20.95% of the dry air in the [[Earth's atmosphere]]. Oxygen gas may be diatomic (O₂) or triatomic (O_3, ...ding to: 2O₃ → 3O₂ + 69 kcal/mol. In the outer atmosphere ([[stratosphere]]) ozone is formed under the influence of [[ultraviolet]] (

'''Vayu''': Yazad personifying the wind or atmosphere (Var. Gowad, Govad) (Indo-Iranian in origin)

...the quality of content, a related issue is the possible importation of the atmosphere on WP along with the content. Partially this is a question of what categori

...ture. Such impacts have happened before – in 1908, a meteoroid entered the atmosphere over Siberia in an event known as the Tunguska impact. When scientists firs

...ndon State College</ref> It assumes the airshed (i.e., a given volume of [[Atmosphere|atmospheric]] air in a geographical region) is in the shape of a box. It al ...llution plume parcels (also called particles) as the parcels move in the [[atmosphere]] and they model the motion of the parcels as a ''random walk'' process. T

...ndon State College</ref> It assumes the airshed (i.e., a given volume of [[Atmosphere|atmospheric]] air in a geographical region) is in the shape of a box. It al ...llution plume parcels (also called particles) as the parcels move in the [[atmosphere]] and they model the motion of the parcels as a ''random walk'' process. T

...to the [[atmosphere]]. These [[chemical compound]]s are transformed in the atmosphere, often traveling thousands of [[kilometer]]s from their original source, an ...broad term that includes both wet and dry deposition of material from the atmosphere which contain higher than normal amounts of acids (predominantly [[sulfuric

...to the [[atmosphere]]. These [[chemical compound]]s are transformed in the atmosphere, often traveling thousands of [[kilometer]]s from their original source, an ...broad term that includes both wet and dry deposition of material from the atmosphere which contain higher than normal amounts of acids (predominantly [[sulfuric

...0 [[Rankine (unit)|°R]]) and 14.696 [[U.S. customary units|psia]] (i.e., 1 atmosphere of absolute pressure) because it was almost universally used by the oil and * 101.325 kPa = 1 [[Atmosphere (unit)|atm]] = 1.01325 [[Bar (unit)|bar]] = 760 mm Hg = 29.92 in Hg ≈ 14.

[[File:Jan_Mayen_orthographic.png | thumb | 2002 EB5 entered the Earth's atmosphere near Iceland and Jan Mayen close to midnight on March 11, 2002.]]

...uter simulation|simulation]] of how air pollutants disperse in the ambient atmosphere. It is performed with computer programs, called [[Air pollution dispersion ...equation in 1947<ref>Sutton, O.G., "The problem of diffusion in the lower atmosphere", QJRMS, 73:257, 1947 and "The theoretical distribution of airborne polluti

...uter simulation|simulation]] of how air pollutants disperse in the ambient atmosphere. It is performed with computer programs, called [[Air pollution dispersion ...equation in 1947<ref>Sutton, O.G., "The problem of diffusion in the lower atmosphere", QJRMS, 73:257, 1947 and "The theoretical distribution of airborne polluti

*{{cite book|author=F.K. Lutgens and E.J.Tarbuck|title=The Atmosphere: A Introduction to Meteorology|edition=5th Edition|publisher=Prentice Hall|

...f fossil fuels and therefore emit large amounts of flue gas to the ambient atmosphere. The table below presents the total amounts of flue gas typically generated

...lements.</ref> At a [[pressure]] of 101.325 k[[Pascal (unit)|Pa]] (= 1.0 [[Atmosphere (unit)|atm]]), it has a [[boiling point]] of 4,265 °[[Celsius (unit)|C]] a