The Atlantic Multidecadal Oscillation (AMO) is a long-term cycle of sea surface temperature fluctuations in the North Atlantic Ocean, typically lasting 60 to 80 years. This oscillation has significant effects on regional climates, influencing storm patterns and intensity, especially in North America and the Caribbean. The AMO alternates between warm and cool phases, affecting not only temperature but also precipitation patterns and atmospheric circulation, which in turn impacts the frequency and intensity of storms.
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