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En cambio, en la estratosfera (hasta la estratopausa, a una altitud de cerca de 50 km), la temperatura aumenta gradualmente con la altitud debido a la absorción de radiación ultravioleta por el ozono.
In contrast, in the stratosphere (up to the stratopause, at a height of nearly 50 km), temperature gradually increases with height because of the absorption of ultraviolet radiation by ozone.
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