State of the Science Fact Sheet: Atlantic Meridional Overturning Circulation (AMOC)
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2024
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Alternative Title:Atlantic Meridional Overturning Circulation (AMOC)
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Description:The AMOC is the Atlantic Ocean component of the global Meridional Overturning Circulation, which is sometimes also referred to as the global ocean conveyor belt (Fig. 1). The AMOC carries relatively warm and salty upper ocean waters to the highlatitude North Atlantic and then to the Arctic, releasing heat into the atmosphere over the high-latitudes. As such, the warm and salty water cools along its path northward becoming denser, and sinking to form cooler deep water in the high-latitude North Atlantic. The newly formed deep water then moves southward and is slowly (over hundreds to thousands of years) transformed into upper ocean waters through mixing and upwelling in the Indo-Pacific and Southern Ocean. The AMOC transports heat, salt, carbon, nutrients, and other properties across the basin, meaning that variations in the AMOC’s strength (commonly measured by the volume of upper ocean water transported northward in unit time) impacts sea level, marine ecosystems, shift temperature and precipitation patterns, and extreme weather. Thus, changes in the AMOC can significantly impact society.
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Rights Information:CC0 Public Domain
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Compliance:Library
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