As altitude increases, the remote PIC should expect:

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Multiple Choice

As altitude increases, the remote PIC should expect:

Explanation:
Winds aloft tend to increase with altitude because surface friction that slows winds near the ground fades away, allowing the pressure gradient to drive faster air higher up. In the upper atmosphere, especially around jet-stream levels, winds are stronger, so as you climb you generally encounter higher wind speeds. For a remote PIC, this means planning for greater wind impact on airspeed versus groundspeed and recognizing that wind-related effects can change with altitude. The idea that winds would decrease or stay the same doesn’t match how wind strength typically changes with height, and while turbulence can occur in some layers, the question is about the overall wind speed trend with altitude.

Winds aloft tend to increase with altitude because surface friction that slows winds near the ground fades away, allowing the pressure gradient to drive faster air higher up. In the upper atmosphere, especially around jet-stream levels, winds are stronger, so as you climb you generally encounter higher wind speeds. For a remote PIC, this means planning for greater wind impact on airspeed versus groundspeed and recognizing that wind-related effects can change with altitude. The idea that winds would decrease or stay the same doesn’t match how wind strength typically changes with height, and while turbulence can occur in some layers, the question is about the overall wind speed trend with altitude.

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