Search results
Jump to navigation
Jump to search
- ...k|author=Frederick K. Lutgens, Edward T. Tarbuck and Dennis Tasa|title=The Atmosphere: An Introduction To Meteorology|edition=11th|publisher=Prentice Hall|year=2598 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)|bar5 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 means2 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, lowe771 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 t9 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 boun1 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 and950 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 ca2 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 −70°C (−94°F, 233 K) be ...31 K) before freezing. Under high pressure (2,000 [[Atmosphere (unit)|atmosphere]]s) water will super cool to as low as −70°C (−94°F, 203 K) b6 KB (821 words) - 15:24, 14 August 2009