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- ...tosphere (called the ''stratopause'') is around 50 km. The layer above the stratosphere is the [[mesosphere]]. [[Temperature]] increases with height in the stratosphere. This causes the stratosphere to be buoyantly stable, which suppresses vertical motions.580 bytes (84 words) - 12:57, 31 August 2009
- 220 bytes (30 words) - 00:38, 12 September 2009
- 12 bytes (1 word) - 17:20, 21 November 2007
- Auto-populated based on [[Special:WhatLinksHere/Stratosphere]]. Needs checking by a human.890 bytes (115 words) - 20:39, 11 January 2010
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- ...tosphere (called the ''stratopause'') is around 50 km. The layer above the stratosphere is the [[mesosphere]]. [[Temperature]] increases with height in the stratosphere. This causes the stratosphere to be buoyantly stable, which suppresses vertical motions.580 bytes (84 words) - 12:57, 31 August 2009
- Layer of the Earth's atmosphere that is directly above the stratosphere and directly below the thermosphere, located about 50 to 85 kilometers (30223 bytes (29 words) - 00:10, 12 September 2009
- ...ing and improving the nation's [[Air Quality Index|air quality]] and the [[Stratosphere|stratospheric ozone layer]].296 bytes (42 words) - 00:41, 28 June 2009
- The '''mesosphere''' is the layer of Earth's atmosphere above the [[stratosphere]]. The mesosphere lies at altitudes between about 50 km and 80 km. The top414 bytes (59 words) - 13:01, 31 August 2009
- {{r|Stratosphere}}532 bytes (66 words) - 21:01, 31 August 2009
- {{r|Stratosphere}}453 bytes (57 words) - 19:53, 11 January 2010
- {{r|Stratosphere}}669 bytes (81 words) - 21:49, 13 August 2009
- {{r|Stratosphere}}502 bytes (63 words) - 18:27, 11 January 2010
- {{r|Stratosphere}}481 bytes (60 words) - 17:15, 11 January 2010
- {{r|Stratosphere}}716 bytes (87 words) - 22:25, 3 September 2009
- {{r|Stratosphere}}634 bytes (80 words) - 21:06, 11 January 2010
- {{rpl|Stratosphere}}684 bytes (87 words) - 13:46, 21 November 2022
- ...e of about 80 km. The homosphere is composed of the [[troposphere]], the [[stratosphere]], and the [[mesosphere]]. Above the homosphere is the [[heterosphere]], wh696 bytes (104 words) - 15:28, 18 August 2009
- ...n]] that contains three oxygen [[atom]]s. It is produced in the Earth's [[stratosphere]] when [[ultraviolet radiation]] causes diatomic oxygen (O<sub>2</sub>) to878 bytes (122 words) - 22:17, 16 April 2009
- Auto-populated based on [[Special:WhatLinksHere/Stratosphere]]. Needs checking by a human.890 bytes (115 words) - 20:39, 11 January 2010
- ...nd the [[water]] produced a giant [[ash cloud]] that reached up into the [[stratosphere]]. The drastically increased concentration of small particles in the air po1 KB (183 words) - 08:45, 28 April 2010
- ...as do weather balloons. Above that is the [[mesosphere]]. The troposphere, stratosphere, and mesosphere together make up the [[homosphere]], in which the component3 KB (509 words) - 11:48, 2 February 2023
- ...p>) at the [[tropopause]] (boundary between the [[troposphere]] and the [[stratosphere]]). Radiative forcing is due to a change in an external driver of climate1 KB (206 words) - 12:06, 22 August 2008
- .... The '''''tropopause''''' is the boundary between the troposphere and the stratosphere. Together, the troposphere and the tropopause are known as the ''lower atmo ...and geographically. The '''''stratopause''''' is the boundary between the stratosphere and the mesosphere. The [[atmospheric pressure]] here is 1/1000th of the a7 KB (1,143 words) - 19:29, 31 August 2009
- ...the lowest to the highest layer, they are the '''[[Troposphere]]''', '''[[Stratosphere]]''', '''[[Mesosphere]]''', '''[[Thermosphere]]''' and the '''[[Exosphere] ::; ''Tropopause'': The boundary between the troposphere and the stratosphere. Together, the troposphere and the tropopause are known as the ''lower atmo22 KB (3,363 words) - 19:40, 9 January 2021
- ...The mushroom cloud climbed to 57,000 feet in only 90 seconds, entering the stratosphere. One minute later it reached 108,000 feet, eventually stabilizing at a ceil4 KB (670 words) - 10:29, 18 March 2024
- ...r, the [[troposphere]], the [[tropopause]], and the lower section of the [[stratosphere]]. The majority of Earth's observed weather is in the troposphere.<ref>{{ci9 KB (1,226 words) - 15:00, 4 March 2021
- ...ing and improving the nation's [[Air Quality Index|air quality]] and the [[Stratosphere|stratospheric ozone layer]]. The latest major amendments were enacted as th11 KB (1,664 words) - 19:22, 9 February 2010
- Large volcanic eruptions can inject [[aerosol]]s into the [[stratosphere]] which scatter solar radiation, decreasing surface air temperatures and lo13 KB (1,869 words) - 22:22, 6 January 2011
- ...ub>3</sub> → 3O<sub>2</sub> + 69 kcal/mol. In the outer atmosphere ([[stratosphere]]) ozone is formed under the influence of [[ultraviolet]] (UV) light.12 KB (1,791 words) - 05:43, 6 March 2024
- ...d contains about 80 percent of the mass of the overall atmosphere. The ''[[stratosphere]]'' is the next layer and extends from 18 km to about 50 km. The third laye ...the mixing layer capped by the inversion layer; the free troposphere; the stratosphere; the mesosphere and others. Many air pollution dispersion models are referr35 KB (5,287 words) - 21:27, 15 December 2013
- ...ut of the ether ... it was a magical vehicle collectively soaring into the stratosphere. And as more albums came out, the set got longer and longer.<ref>Liner note13 KB (1,938 words) - 02:43, 2 April 2024
- ...-bearing haloalkanes reach the upper atmosphere when they escape. In the [[stratosphere]], [[chlorofluorocarbon]]s (CFCs) break up due to [[UV]]-radiation, releasi18 KB (2,699 words) - 10:31, 28 June 2023