different between tropopause vs stratosphere
tropopause
English
Etymology
tropo- (“troposphere”) +? -pause (“discontinuance”).
Noun
tropopause (plural tropopauses)
- The zone of transition between the troposphere and the stratosphere (approximately 13 kilometers). The tropopause normally occurs at an altitude of between 25,000 and 45,000 feet in polar and temperate zones. It occurs at 55,000 feet in the tropics.
Translations
French
Etymology
tropo- (“troposphere”) +? -pause (“discontinuance”).
Pronunciation
- IPA(key): /t??.p?.poz/
Noun
tropopause f (plural tropopauses)
- tropopause.
Further reading
- “tropopause” in Trésor de la langue française informatisé (The Digitized Treasury of the French Language).
tropopause From the web:
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stratosphere
English
Etymology
From French stratosphère, a word coined by its discoverer, meteorologist Léon Teisserenc de Bort. See strato- +? -sphere.
Pronunciation
Noun
stratosphere (plural stratospheres)
- (geology, obsolete) Collectively, those layers of the Earth’s crust which primarily comprise stratified deposits.
- 1908, Eduard Suess [aut.], Hertha Beatrice Coryn Sollas and William Johnson Sollas [trs.], The Face of the Earth (Oxford, at the Clarendon Press), volume 3, chapter 1, page 2
- So great is the part played by stratified deposits in the structure of the earth’s crust that we might be tempted to speak of the stratosphere of the earth in contradistinction to the scoriosphere of the moon.
- 1909, Eduard Suess [aut.], Hertha Beatrice Coryn Sollas and William Johnson Sollas [trs.], The Face of the Earth (Oxford, at the Clarendon Press), volume 4, chapter 15, page 546
- The stratosphere, or younger sedimentary envelope has been formed almost entirely at the expense of the Sal envelope.
- 1908, Eduard Suess [aut.], Hertha Beatrice Coryn Sollas and William Johnson Sollas [trs.], The Face of the Earth (Oxford, at the Clarendon Press), volume 3, chapter 1, page 2
- (meteorology) The region of the uppermost atmosphere where temperature increases along with the altitude due to the absorption of solar ultraviolet radiation by ozone. The stratosphere extends from the tropopause (10–15 kilometers) to approximately 50 kilometers, where it is succeeded by the mesosphere.
- 1909, Scientific Abstracts, A., volume 12, page 208 (heading)
- Variation in height of the stratosphere (isothermal layer).
- 1909, Scientific Abstracts, A., volume 12, page 208 (heading)
Translations
Further reading
- stratosphere on Wikipedia.Wikipedia
stratosphere From the web:
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