The flow of water from the eastern Mediterranean to the Atlantic Ocean increased significantly during the Younger Dryas compared to today.
Around 13,000 years ago, parts of the planet experienced a period of intense climate change known as the Younger Dryas. This was when parts of Europe and North America returned toThis marked the last period of intense cold in the northern hemisphere before the current, warmer Holocene epoch. The cold conditions had an effect on water circulation in the Mediterranean and Atlantic at the time. A new study led by the University of Barcelona looks into this specifically.
"Mediterranean water masses are one of the primary sources of salt in the North Atlantic. Water salinity is an important factor in oceanography, as it determines the density of water masses.
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