polar high pressure belt where they flow in which degrees a flow
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The polar highs are small in area and extend around the poles.
They lie around poles between 80 – 90° N and S latitudes.
Formation
The air from sub-polar low pressure belts after saturation becomes dry. This dry air becomes cold while moving towards poles through upper troposphere.
The cold air (heavy) on reaching poles subsides creating a high pressure belt at the surface of earth.
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