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