 Atlantic Equatorial mode

The Atlantic Equatorial Mode (AEM) is a climate phenomenon that refers to the variability in sea surface temperatures and atmospheric conditions over the equatorial Atlantic Ocean. It plays a significant role in influencing weather patterns and climate variability in the surrounding regions, including North America, South America, and Africa. The AEM is characterized by fluctuations in sea surface temperatures along the equatorial Atlantic, which can affect the strength and position of the trade winds, precipitation patterns, and storm activity in the tropics.