Surface winds and upper-level winds blow in the same direction in a thermal circulation.

Name: Surface winds and upper-level winds blow in the same direction in a thermal circulation.
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In a thermal circulation, the surface winds blow from high pressure to low pressure, while the upper-level winds blow in the opposite direction (from west to east in the northern hemisphere). This creates a convection loop and is also known as a Hadley cell.

Surface Winds and Upper-Level Winds Blow in the Same Direction