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  2. Heat is produced in the process of the formation of ozone, and this heat is responsible for temperature increases, from an average -60°F (-51°C) at tropopause to a maximum of about 5°F (-15°C) at the top of the stratosphere. This increase in temperature with height means warmer air is located above cooler air.
    www.noaa.gov/jetstream/atmosphere/layers-of-atm…
    Instead, the heat absorbed and trapped by our atmosphere keeps our planet's average surface temperature at a balmy 15°C (59°F). Some of the atmosphere's gases, like carbon dioxide, are particularly good at absorbing and trapping radiation.
    scied.ucar.edu/learning-zone/atmosphere/what-is-a…
     
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