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  • ...k|author=Frederick K. Lutgens, Edward T. Tarbuck and Dennis Tasa|title=The Atmosphere: An Introduction To Meteorology|edition=11th|publisher=Prentice Hall|year=2
    598 bytes (85 words) - 20:37, 27 March 2012
  • {{Dambigbox|Atmosphere (unit)|Atmosphere}} ...sp/en/ViewCGPMResolution.jsp?CGPM=10&RES=4 BIPM Definition of the standard atmosphere]</ref> For practical purposes, it is often replaced by the [[Bar (unit)|bar
    5 KB (837 words) - 10:47, 9 September 2023
  • ...cessful isolation of [[argon]], a [[noble]] gas appearing in the [[Earth's atmosphere]]. ...gases. After noting that the density of the nitrogen gas isolated from the atmosphere was somewhat higher than the density of nitrogen obtained by chemical means
    2 KB (306 words) - 15:17, 18 August 2009
  • {{r|Earth's atmosphere}}
    734 bytes (97 words) - 13:39, 4 December 2022
  • {{r|Earth's atmosphere}}
    810 bytes (101 words) - 18:43, 28 May 2011
  • '''Greenhouse gases''' are gases in an atmosphere that absorb and emit [[infrared radiation]]. By doing so they produce the [
    805 bytes (117 words) - 14:06, 26 January 2009
  • {{r|Atmosphere}}
    927 bytes (118 words) - 09:07, 28 April 2024
  • '''Aether''' (᾿Αιθήρ) is the ancient-Greek god of the high atmosphere, containing the air breathed by the gods, in contrast to the ordinary, lowe
    771 bytes (113 words) - 04:22, 29 October 2008
  • {{r|Atmosphere (unit)}}
    828 bytes (110 words) - 13:36, 8 July 2011
  • {{r|Atmosphere}}
    890 bytes (115 words) - 20:39, 11 January 2010
  • ...f incident light, the [[dissipation]] of light in the [[Earth's atmosphere|atmosphere]] is greater when it falls at a shallow angle.]]
    2 KB (404 words) - 10:27, 26 September 2007
  • ...66-6}}</ref><ref>{{cite book|author=F.K. Lutgens and E.J.Tarbuck|title=The Atmosphere: A Introduction to Meteorology|edition=5th Edition|publisher=Prentice Hall| ...meteorology. Those events are bound by the variables existing in [[Earth's atmosphere]] (such as [[temperature]], [[pressure]] and [[water]] [[Gas|vapor]]) and t
    9 KB (1,226 words) - 15:00, 4 March 2021
  • *{{cite book|author=Kshudiram Saha|title=The Earth's Atmosphere: Its Physics and Dynamics|edition=1st Edition|publisher=Springer|year=2008|
    790 bytes (114 words) - 16:13, 20 October 2009
  • *{{cite book|author=F.K. Lutgens and E.J.Tarbuck|title=The Atmosphere: A Introduction to Meteorology|edition=5th Edition|publisher=Prentice Hall|
    885 bytes (130 words) - 16:13, 17 November 2008
  • {{r|Atmosphere}}
    912 bytes (145 words) - 14:21, 3 November 2008
  • ...]], [[animal]]s, [[microorganisms]], [[soil]], [[Rock (geology)|rocks]], [[atmosphere]] and [[natural phenomenon|natural phenomena]] that occur within their boun
    1 KB (139 words) - 15:03, 1 May 2011
  • {{r|Atmosphere}}
    1 KB (145 words) - 09:18, 6 March 2024
  • '''[[Air]]''' is that part of Earth's atmosphere that humans and all other mammals breathe. It is a colorless, odorless and
    950 bytes (152 words) - 14:34, 11 March 2010
  • ...n|<sup>14</sup>C]]) it contains. Cosmic radiation creates carbon-14 in the atmosphere which is absorbed by plants through [[photosynthesis]]. When animals eat pl The amount of carbon-14 in the atmosphere (and therefore plants and animals) varies over time, so dates need to be ca
    2 KB (367 words) - 15:47, 24 September 2012
  • ...isbn = 0890541728}}</ref>. Under high pressure (2,000 [[Atmosphere (unit)|atmosphere]]s) water will supercool to as low as &minus;70°C (&minus;94°F, 233 K) be ...31&nbsp;K) before freezing. Under high pressure (2,000 [[Atmosphere (unit)|atmosphere]]s) water will super cool to as low as &minus;70°C (&minus;94°F, 203 K) b
    6 KB (821 words) - 15:24, 14 August 2009
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