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Gulf stream slowdown shows need to end climate change & capitalism

The Gulf stream’s warmth stretches from the tip of Florida northwards along the US East Coast. It is one of many currents in the thermohaline, or Atlantic meridional overturning circulation (AMOC), an essential system credited for the hospitality of the Northern hemisphere. It carries warm water from the Tropics to the North Atlantic “like a conveyor belt,” as climate scientists have aptly described, amidst serious concerns of AMOC weakening and possibly eventually stalling altogether.