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Heat Accumulation in the Deeper Labrador Sea Causes Instabilities in Ice Sheet, Study Shows

Heinrich Events or, more accurately, Heinrich Layers, are recurrent conspicuous sediment layers, usually ten to 15 centimeters thick, with very coarse rock components that interrupt the otherwise fine-grained oceanic deposits in the North Atlantic. ....

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Excessive Heat Triggers Global Climate Change in North Atlantic Ocean

Excessive cooling events defined as Heinrich Events in the North Atlantic during the last glacial period are a perfect example of how local processes affect global climate. ....

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