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stratosphere (n.)

1908, from French stratosphère, literally "sphere of layers," coined by French meteorologist Léon-Philippe Teisserenc de Bort (1855-1913) from Latin stratus "a spreading out" (from past-participle stem of sternere "to spread out," from PIE root *stere- "to spread") + French -sphère, as in atmosphère (see sphere).

The region where the temperature increases or remains steady as altitude increases. An earlier stratosphere, attested in English 1908 and coined in German 1901, was a geological term for part of the Earth's crust. It is now obsolete in this sense. Related: Stratospheric.

also from 1908
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Trends of stratosphere

updated on September 28, 2017

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