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- The troposphere is the lowest layer of the atmosphere, where most weather occurs12. It is heated from below by various sources of energy, such as latent heat, longwave radiation, and sensible heat1. The temperature of the troposphere decreases with altitude, from an average of 15°C (59° F) at sea level to about −55°C (−67° F) at the tropopause, the boundary between the troposphere and the stratosphere12. The tropopause temperature varies from −80 °C (−112 °F) in the tropics to −50 °C (−58 °F) in polar regions2.Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.
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/TroposphereTemperatures 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.
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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
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