Answer:
The troposphere extends from Earth’s surface to an average of 12 km (7 miles). As you move upward, air pressure decreases. The temperature generally decreases with increasing height up to the tropopause. The tropopause marks the transition into the stratosphere. Winds increase with height up the jet stream. The interaction of solar energy and wind cause the upper layer of the troposphere to have a low moisture content. Convection occurs in the troposphere due to the presence of water in the air as well as energy transfer from radiation and weather.
Step-by-step explanation:
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