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The Atlantic Multidecadal Oscillation (AMO) is a global-scale mode of multidecadal climate variability (that is, it is an example of a cyclical or semicyclical pattern of climate change that repeats on a timescale on the order of several decades). The AMO is based on sea surface temperatures in the North Atlantic Ocean between the equator and 70° north latitude. Generally, the AMO is computed as a detrended ten-year running mean of these sea surface temperatures and represents variability... więcej
Salem Press Encyclopedia of Science, 2023. 3p.
