Surface winds in the Northern Hemisphere flow across isobars towards low pressure due to friction, which reduces the Coriolis force and causes the wind to spiral inward toward the low-pressure center.
Explanation:
The Arctic Oscillation (AO) is a large-scale climate pattern of sea level pressure differences between the Arctic and the mid-latitudes of the Northern Hemisphere. It affects weather patterns across the entire Northern Hemisphere.
No comments yet. Be the first to start the discussion!