Pressure gradients in the upper troposphere result from sloping isobaric surfaces.

Name: Pressure gradients in the upper troposphere result from sloping isobaric surfaces.
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The pressure gradient force is the force that drives air from areas of higher pressure to areas of lower pressure. In the upper troposphere, isobaric surfaces are not parallel to the Earth's surface, which results in sloping isobaric surfaces and pressure gradients.

Pressure Gradients in the Upper Troposphere Result from Sloping Isobaric