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stratosphere
atmospheric region
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External Websites
- Nature - Communications Earth and Environment - Stratospheric drivers of extreme events at the Earth’s surface
- PNAS - Earth, Atmospheric, and Planetary Sciences - Why the lower stratosphere cools when the troposphere warms
- UCAR Center for Science Education - The Stratosphere
- University of Cambridge - Faculty of Mathematics - Into the stratosphere
- Key People:
- Jean-Felix Piccard
- Auguste Piccard
- Léon Teisserenc de Bort
- Related Topics:
- atmosphere
- jet stream
- quasi-biennial oscillation
stratosphere, layer of Earth’s atmosphere lying between the troposphere and the mesosphere. The lower portion of the stratosphere is nearly isothermal (a layer of constant temperature), whereas temperatures in its upper levels increase with altitude. The stratosphere extends from the tropopause at about 10 to 17 km (about 6 to 11 miles) altitude to its upper boundary (the stratopause) at about 50 km (30 miles), and it also contains the ozone layer. See atmosphere.