Winds occurring as a result of upper-level flow are generally faster than the surface winds directly below.

Name: Winds occurring as a result of upper-level flow are generally faster than the surface winds directly below.
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This is because there is less friction at higher altitudes, allowing the winds to flow more freely and reach higher speeds. Surface winds are slowed down by friction from the terrain and other objects on the ground, resulting in slower speeds.

Winds Occurring as a Result of Upper-Level Flow Are Generally