VARIOUS WEATHER PHENOMENA ARE CONFINED TO THE TROPOSPHERE
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The air temperature begins to rise into the stratosphere. Such a temperature increasing prevents much air convection beyond the tropopause, and therefore most weather phenomena, including bearing clouds of thunderstorms, cumulonimbus, are confined to the troposphere.
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The air temperature begins to rise into the stratosphere. Such a temperature increasing prevents much air convection beyond the tropopause, and therefore most weather phenomena, including bearing clouds of thunderstorms, cumulonimbus, are confined to the troposphere.
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