Replies to Msg. #731422
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 Msg. #  Subject Posted by    Board    Date   
63479 Re: Winger Global Cooling
   ktc [b]Another theory proposed by Ewing and Donn in 1956 hypothesized...
ribit   POPE   04 Jul 2012
8:41 PM
63447 Re: Winger Global Cooling
   "What is clear from the record going back over nearly four decades is...
DGpeddler   POPE   04 Jul 2012
1:18 AM

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Re: Winger Global Cooling

By: killthecat in POPE
Wed, 04 Jul 12 12:33 AM
Msg. 63438 of 65535
(This msg. is a reply to 63436 by DGpeddler)
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Here's some real, potential Winger Global Cooling (North Atlantic mostly) for you to ponder. (Do wingers ponder?)

Another theory proposed by Ewing and Donn in 1956 hypothesized that an ice-free Arctic Ocean leads to increased snowfall at high latitudes. When low-temperature ice covers the Arctic Ocean there is little evaporation or sublimation and the polar regions are quite dry in terms of precipitation, comparable to the amount found in mid-latitude deserts. This low precipitation allows high-latitude snowfalls to melt during the summer. An ice-free Arctic Ocean absorbs solar radiation during the long summer days, and evaporates more water into the Arctic atmosphere. With higher precipitation, portions of this snow may not melt during the summer and so glacial ice can form at lower altitudes and more southerly latitudes, reducing the temperatures over land by increased albedo. Furthermore, under this hypothesis the lack of oceanic pack ice allows increased exchange of waters between the Arctic and the North Atlantic Oceans, warming the Arctic and cooling the North Atlantic. (Current projected consequences of global warming include a largely ice-free Arctic Ocean within 5–20 years). Additional fresh water flowing into the North Atlantic during a warming cycle may also reduce the global ocean water circulation. Such a reduction, by reducing the effects of the Gulf Stream, would have a cooling effect on northern Europe, which in turn would lead to increased low-latitude snow retention during the summer. It has also been suggested that during an extensive glacial period, glaciers may move through the Gulf of Saint Lawrence, extending into the North Atlantic ocean far enough to block the Gulf Stream.