New Study Indicates North Atlantic Is Close To A Tipping Point
A long-standing theory contends that the period’s initial cooling was maintained by “sea-ice to ocean feedbacks”; as the sea ice expanded, ocean currents slowed, which in turn decreased the flow of warm water from the south. The University of Exeter conducted a new study that examined how the ocean has changed and responded to external changes over the last few centuries using the shells of quahog clams, which can survive for several hundred years....