The fast-flowing, narrow air currents known as jet streams, in the tropopause, where the troposphere, whose temperature decreases with altitude, gives way to the stratosphere, whose temperature increases with altitude, reach their peak strength.
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A
The fast-flowing, narrow air currents known as jet streams, in the tropopause, where the troposphere, whose temperature decreases with altitude, gives way to the stratosphere, whose temperature increases with altitude,
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B
In the tropopause, where the troposphere gives way to the stratosphere, respectively decreasing and increasing with altitude, the fast-flowing, narrow air currents known as jet streams
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C
In the tropopause, where the troposphere, whose temperature decreases with altitude, gives way to the stratosphere, whose temperature increases with altitude, the fast-flowing, narrow air currents known as jet streams
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D
Increasing in temperature with altitude, the fast-flowing, narrow air currents known as jet streams, where the troposphere, whose temperature decreases with altitude, gives way in the tropopause to the stratosphere,
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E
The fast-flowing, narrow air currents known as jet streams, in the tropopause, where the troposphere whose temperature decreases with altitude gives way to the stratosphere, increases in temperature with altitude and
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