The stratosphere is the second layer of our planet’s atmosphere, wedged between the troposphere (1st layer) and mesosphere (3rd layer). Â It reaches roughly from altitudes of 10km to 50km. Â These boundaries are set by reversals in the temperature grade. Â In the troposphere, as altitude increases temperature decreases, however, in the stratosphere the reverse is true. Â This is because ozone builds up at the outer extent of the stratosphere capturing UV radiation from the sun, and thus warming up. Â . Â Then in the mesosphere temperature starts decreasing again with altitude gain. Â Commercial airliners and military planes often operate at altitudes around 9-12km because of the unique turbulence free nature of the stratosphere. Â The stratosphere supports bacterial life, so it is considered part of the biosphere. Â There have even been reports of birds flying in the stratosphere and over mount Everest, whose peak is around 9km.
The stratosphere is also considered near-space, not actual space. Â It is also possible to send a camera payload up to the stratosphere using a a large helium balloon for relatively low cost like these MIT kids did…
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