Temperatures of the sea surface in a vast region south of Greenland are near to, or below their lowest recorded levels
Saturday 26 September 2015
A boat is seen seen among the icebergs that broke off from the Jakobshavn Glacier as the sun reaches its lowest point of the day on July 23, 2013 in Ilulissat, Greenland Getty
A giant “blob” of cold water has appeared in the North Atlantic over the summer months, bucking the global trend of warmer-than-normal sea surface temperatures around the world, scientists said.
Temperatures of the sea surface in a vast region south of Greenland are near to, or below their lowest recorded levels, leading some scientists to speculate that it may be a sign that the vast oceans currents of the North Atlantic are slowing down due to large volumes of glacial melt-water running into the sea.
Since the beginning of the year, scientists at the US National Oceanic and Atmospheric Administration (NOAA) have recorded much lower sea-surface temperatures than usual in the region south of Greenland and Iceland, with some area recording the lowest eight-month period on record.
This contrasts with the noticeably higher-than-average temperatures seen in almost every other part of the world, which has coincided with a strong “El Nino” event in the Pacific Ocean – the warm sea current associated with a disturbance in normal weather patterns.
A spokeswoman for the UK’s Met Office said: “North Atlantic sea surface temperatures are well below average and they have been all summer.”
One suggestion is that the freshwater run-off from the melting Greenland glaciers are disturbing the ocean “engine” that drives the North Atlantic meridional overturning circulation – the giant “conveyor belt” of sea currents that include the Gulf Stream.
The engine that drives ocean currents is powered by the sinking of cold, salty water from the sea surface to the seabed in a part of the North Atlantic south of Iceland. But some scientists fear that it is being disturbed by a layer of cold freshwater, which tends to remain on the sea surface, because the less-dense freshwater floats on the denser, salty water.
The 'blob', highlighted in blue, just south of the coast of Greenland
Earlier this year, scientists published a study suggesting that the North Atlantic circulation – the northward flow of warm, surface water and the southward flow of deep, cold water – had slowed down by between 15 and 20 per cent during the 20th Century.
“The current ‘blob’ was caused partly by strong winds over the Atlantic during the winter 2013-14 taking a lot of heat out of the ocean, but I think there are longer-term changes going on in the Atlantic that would give a similar temperature pattern,” said Leon Hermanson, a senior scientist at the Met Office Hadley Centre in Exeter.
“The magnitude of the changes on time scales of decades is larger than the effects we expect from Greenland land-ice melt or other factors slowing down the Atlantic conveyor belt,” Dr Hermanson said.
“The measurements we have of the conveyor belt are only ten years long and not at the ideal latitude to study the northern North Atlantic, but I think, based on my own and other people’s research, that the conveyor belt is currently decreasing, mainly due to climate variability and only a little due to climate change,” he said.