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  2. The troposphere is heated from below by latent heat, longwave radiation, and sensible heat. Surplus heating and vertical expansion of the troposphere occurs in the tropics. At middle latitudes, tropospheric temperatures decrease from an average of 15°C (59° F) at sea level to about −55°C (−67° F) at the tropopause.

    en.wikipedia.org/wiki/Troposphere

    Temperatures at the tropopause range from as low as −80 °C (−112 °F) in the tropics to −50 °C (−58 °F) in polar regions. The region above the planetary boundary layer is commonly known as the free atmosphere.

    www.britannica.com/science/atmosphere/Troposph…
     
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    Troposphere - Wikipedia

    The temperature of the troposphere decreases at high altitude by way of the inversion layers that occur in the tropopause, which is the atmospheric boundary that demarcates the troposphere from the stratosphere. See more

    The troposphere is the lowest layer of the atmosphere of Earth. It contains 80% of the total mass of the planetary atmosphere and 99% of the total mass of water vapor and aerosols, and is where most weather phenomena occur. … See more

    The general flow of the atmosphere is from west to east, which, however, can be interrupted by polar flows, either north-to-south flow or a south … See more

    "Layers of the Atmosphere". U.S. National Weather Service. Archived from the original on 2017-05-13.
    Chemical Reactions in the Atmosphere See more

    Composition
    The Earth's planetary atmosphere contains, besides other gases, water vapour and carbon dioxide, which produce carbonic acid in See more

     
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