“We do expect that this reduction in the volume of sinking water (in Greenland Sea) will lead to a reduction in the volume of warm water reaching Europe. That will cool down Europe or at least parts of Europe that are accessible to the ocean. … (England and coastal parts of Europe) will be getting more violent types of weather that are due to the higher temperature differences that are happening everywhere.”
– Ocean Physicist Peter Wadhams, Cambridge University, U. K.

May 11, 2005 Cambridge, England – Normally in the Atlantic Ocean, warm water moves from the Equator up to the British Isles, keeping England and parts of Europe warmer than Labrador which is at the same northern latitude. The warming is caused by a huge convection process called the Atlantic Thermohaline Circulation, or North Atlantic Drift. Equatorial warm water is circulated to the Labrador Sea and Greenland Sea, cools off, and then sea ice forms. The ice does not take up the sea salt which is left behind in the ocean and makes the water denser and it sinks. For more than a century, at least a dozen cylinder-shaped columns of cold water have been sinking into the deep ocean and heading back south toward the Equator which has kept the big conveyor belt of warm-to-cold-to-warm water going in the Atlantic Ocean.Click for report.














