flymango, on 25 July 2012 - 01:43 , said:
Don't know my facts at all but seem to remember reading that the ice melting has a significant impact on the Gulfstream by changing the temperature flows of the ocean up and down the Atlantic with severe climatic impacts and on fisheries and agriculture in both Europe and North America.
This is the thermohaline circulation system, which depends on the temperature of water at the poles and equator and is affected by the mix of fresh (glacier) and salt (ocean) water...
Large ice shelfs cracking up and adding to it will disrupt this system.
No doubt there are arguments against that too. Like we like all a good rainy English summer and forgetting the extensive and repeated wild fires and droughts in N America which decrease food production and increase prices.
This from Wikipedia:
http://en.m.wikipedi...ation#section_2
In April 2004, the hypothesis that the Gulf Stream is switching off received a boost when a retrospective analysis of U.S. satellite data seemed to show a slowing of the North Atlantic Gyre, the northern swirl of the Gulf Stream.[7]
In May 2005, Peter Wadhams reported to The Times of London about the results of investigations in a submarine under the Arctic ice sheet measuring the giant chimneys of cold dense water, in which the cold dense water normally sinks down to the sea bed and is replaced by warm water, forming one of the engines of the North Atlantic Drift. He and his team found the chimneys to have virtually disappeared. Normally there are seven to twelve giant columns, but Wadhams found only two giant columns, both extremely weak.[8][9]
In 2008, Vage et al. reported "the return of deep convection to the subpolar gyre in both the Labrador and Irminger seas in the winter of 2007–2008," employing "profiling float data from the Argo program to document deep mixing," and "a variety of in situ, satellite and reanalysis data" to set the context for the phenomenon. This might have a lot to do with the observations of variations in cold water chimney behaviour.[10]
In January 2010, the Gulf Stream briefly connected with the West Greenland Current after fluctuating for a few weeks due to an extreme negative phase of the Arctic oscillation, temporarily diverting it west of Greenland.[11][12]