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...].<ref>The [[density]] of air-free water at a [[pressure]] of 1 [[Pressure|atmosphere]] and 3.98 °C is 999.974 kg per cubic metre. &nbsp; September 2001, The [[

...d]] slowed the craft as it plunged through the [[celestial body atmosphere|atmosphere]]. During this time, entry science experiments were performed. At 6 km alti

{{r|Pakistan Space and Upper Atmosphere Research Commission|SUPARCO (Pakistani Space Agency)}}

Where the [[atmosphere]] and [[ocean]] are in contact, energy is passed from moving air to the wat

...uction in earlier organisms before oxygen was at high concentration in the atmosphere and thus would represent a more ancient form of energy production in cells. ...ked out, and in alcohol production the carbon dioxide is released into the atmosphere.

* Stabilize greenhouse gas concentration in the atmosphere to a level that would prevent dangerous interference with the world climate

* {{cite book | author = Ramsay, William | title = The Gases of the Atmosphere | year = 1905 | publisher = Macmillan | location = London }}

...an average specific density of 0.69. This is a mean value; Saturn's upper atmosphere is less dense and its core is considerably more dense than water. Saturn's [[celestial body atmosphere|atmosphere]] exhibits a banded pattern similar to Jupiter's (in fact, the nomenclature

...to trigger a change in Sputnik's radio signal. It re-entered the [[Earth's atmosphere]] in January 1958.

*{{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|

*{{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 &rarr; 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