Intro to Climate Science
The North Atlantic Oscillation (NAO) is a climate phenomenon characterized by fluctuations in the difference of atmospheric pressure at sea level between the Icelandic low and the Azores high. These fluctuations influence weather patterns in the North Atlantic region, impacting precipitation, temperature, and storm tracks in Europe and North America. The NAO is an essential aspect of internal climate variability and interacts with other oscillations, affecting global weather systems.
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