fuagf -- it's the increased Greenland ice melt -- the much fresher and thus lighter/less-dense meltwater floats at the surface, keeping the warmer but still heavier/denser saltwater brought to the area by the thermohaline circulation, specifically by the Gulf Stream, from remaining at the surface in contact with the air to be chilled enough to become dense enough to then sink as part of/to continue the thermohaline circulation (and accordingly add the heat to the air that helps keep the UK and Europe so relatively mild) -- the fresher water at the surface just turns to ice if sufficiently chilled, without ever becoming dense enough to then sink into/through the denser saltwater below it as part of/to continue the thermohaline circulation -- covering that, and more (together just one snippet from the ongoing climate research I have stashed):
the study: Competition between global warming and an abrupt collapse of the AMOC in Earth’s energy imbalance Published online:06 October 2015 Abstract A collapse of the Atlantic Meridional Overturning Circulation (AMOC) leads to global cooling through fast feedbacks that selectively amplify the response in the Northern Hemisphere (NH). How such cooling competes with global warming has long been a topic for speculation, but was never addressed using a climate model. Here it is shown that global cooling due to a collapsing AMOC obliterates global warming for a period of 15–20 years. Thereafter, the global mean temperature trend is reversed and becomes similar to a simulation without an AMOC collapse. The resulting surface warming hiatus lasts for 40–50 years. Global warming and AMOC-induced NH cooling are governed by similar feedbacks, giving rise to a global net radiative imbalance of similar sign, although the former is associated with surface warming, the latter with cooling. Their footprints in outgoing longwave and absorbed shortwave radiation are very distinct, making attribution possible. http://www.nature.com/articles/srep14877
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