Monday, May 07, 2007

Melting of Greenland Likely to Impact Atlantic Currents



According to a revision article published in Science, ocean circulation during the last ice age was very different to present day circulation. The formation of deep water currents in the North Atlantic was much weaker and the flow of warm water from the Gulf Stream decreased. This led to a cooling of the northern hemisphere and contributed to the formation of the great ice caps which covered North America, Scandinavia and Europe.

In a similar study, the marine sediments of the North Atlantic were observed in order to document the sequence of events that led to that disturbance. The melting caused a significant decrease in the Gulf Stream, which transports warm water from the Gulf of Mexico to the North. This submerged the region of the North Atlantic into a period of glacial cold which lasted at least 1,200 years.

Nevertheless, the slowing down of the ocean circulation in the North Atlantic began about 700 to 1,200 years before this great melting of the ice caps and the subsequent flow of fresh water into the ocean took place. The very first stage of this change coincided with brief and isolated periods of melting of the small British Ice Sheet (BIS). The authors of the study have come to this conclusion from an observation of the fine layers of sediment (formed by grains of quartz) coming from successive waves of icebergs which, when they melted dumped their load of sediments onto the sea bed. These icebergs came from the edges of the ice which surround and stabilised the BIS.

These results show that the disturbances caused by melting may in turn cause substantial changes in ocean circulation without the need for a catastrophic dumping of fresh water. This seems to indicate that an acceleration in the melting of the Greenland ice cap, could, in fact, play a key role in the future stability of ocean circulation and climate change in the whole North Atlantic region.


Some of this was already known. That the British Icecap had this effect is interesting. It might suggest postponing buying lots in Greenland. It might get mighty cold in the North Atlantic for a while while the rest of the world roasts.

Ah, the chaotic climate! Never a more fickle mistress!

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