The Pacific Meridional Mode (PMM) is a climate pattern that involves variations in ocean temperature and atmospheric conditions in the central and eastern Pacific Ocean. It is characterized by changes in sea surface temperatures (SSTs) that typically occur along a north-south gradient, affecting both the equator and higher latitudes. The PMM can influence weather patterns across the Pacific region and can affect global climate systems, including precipitation patterns, droughts, and temperature variations in various parts of the world.
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