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Huge pool of Arctic fresh water could cool Europe

23 January 2012, by Tamera Jones

British scientists have discovered an enormous dome of fresh water in the western Arctic Ocean. They think it may result from strong Arctic winds accelerating a great clockwise ocean circulation called the Beaufort Gyre, causing the sea surface to bulge upwards.

Ocean circulation in the North Atlantic

The North Atlantic and Arctic Oceans are critical components of the ocean-climate system.

The researchers made their discovery using European Space Agency (ESA) satellites ERS-2 and Envisat. They measured sea-surface height over the western Arctic over a 15-year period, from 1995 to 2010.

Using these measurements, they calculate that since 2002 the sea surface in the western Arctic has risen by around 15cm, and the volume of fresh water has swollen by roughly 8000 cubic kilometres. This is around ten per cent of all the fresh water in the Arctic Ocean.

'Our findings suggest that a reversal of the wind could result in the release of this fresh water to the rest of the Arctic Ocean and even beyond.'
Dr Katharine Giles, CPOM, UCL

If the wind changes direction, as happened between the mid-1980s and mid-1990s, the water could spill out into the rest of the Arctic and then perhaps even the north Atlantic. This could cool Europe by slowing down a key ocean current derived from the Gulf Stream, which keeps the continent relatively mild compared with countries at similar latitudes.

The Gulf Stream forms part of a larger movement of water called the ocean conveyor belt, which is itself one component of the global system of ocean currents.

'Satellite data has shown us that a dome of fresh water has been building up in the western Arctic over the past 15 years, due to the wind. Our findings suggest that a reversal of the wind could result in the release of this fresh water to the rest of the Arctic Ocean and even beyond,' says Dr Katharine Giles from the Centre for Polar Observation and Modelling (CPOM) at University College London, lead author of the study, published in Nature Geoscience.

Earlier studies from ships, submarines, and instruments on moored buoys had pointed to increasing volumes of fresh water in the Arctic over the last few decades, especially in the western Arctic. Not only that, but other studies had found that less fresh water reached the Atlantic than expected over the same period of time. These findings suggest the water is concentrated in the Beaufort Gyre, and can't spill out into the Atlantic.

But all of these studies relied on limited observations, so scientists weren't sure exactly what was driving the changes.

Climate models had suggested that the action of the wind on the sea surface could cause a raised dome to form in the middle of the Beaufort Gyre. But until now, there had been no continuous observations of sea-surface height to demonstrate this categorically.

Now, using satellite data from 1995 to 2010, Giles and colleagues from the National Oceanography Centre (NOC) have found that the height of the sea surface in the middle of the Beaufort Gyre has increased substantially since 2002.

Ocean dynamic topography

The orange patch shows the Beaufort Gyre and the rise in sea surface height.

'We were surprised to find that our results also suggested that something else was going on,' says Giles. 'When we looked at our data on a year-to-year basis we noticed that the changes in the sea surface height did not always follow what the wind was doing so we thought about reasons why this might happen. One idea is that sea ice forms a barrier between the atmosphere and the ocean. So, as the sea-ice cover changes, the effect of the wind on the ocean might also change.'

'Our next step is to look into how changes in the sea-ice cover might affect the coupling between the atmosphere and the ocean in more detail to see if we can confirm this idea,' she adds.

'Satellites have been measuring how the ice is changing for many years but we now have the tools to monitor how the ocean underneath the ice is changing. These techniques can also be used with the recently launched CryoSat-2 satellite to measure changes over the whole basin,' says Dr Seymour Laxon, director of CPOM and co-author of the study.


Katharine A. Giles, Seymour W. Laxon, Andy L. Ridout, Duncan J. Wingham & Sheldon Bacon (2012), Western Arctic Ocean freshwater storage increased by wind-driven spin-up of the Beaufort Gyre, Nature Geoscience, doi: 10.1038/NGEO1379, published online on 22 January 2012


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Your comments

Oh dear yet more scaremongering by the lefty green lobby.

Steve, Somerset, england, UK
Monday, 23 January 2012 - 14:52

These cycles have been going on since the Atlantic opened up, so no need to worry it is just a part of the earths cycling of heat. Whatever happens to the climate mankind will just have to adapt or perish. With the effect the ever increasing World population is having on the environment and Governments inability to control it I think some control of the population by nature would benefit the Planet. So a little cooling would be ok! It is interesting though to follow these events even if we can do little or should do anything about them.

Malcolm Jones, Wales
Monday, 23 January 2012 - 20:33

Eight thousands cubic km sounds like a huge quantity. Let us remind that Lake Agassiz's discharge around 6000 BCE may have been a hundred times that amount. Moreover, current concentration of CO2 is sustaining such an increase in oceans' temperature that what we shall see is likely to be just one of the recurring disturbances in European weather. In a few summers, Arctic ice cap will lose its fastening links with Canadian ice shelves; then wind could truly destabilize it and displace some of that fresh water. Dynamics of the phenomenon will provide an excellent subject of study!

Massimo E. Roscio, Legnano, Italy
Saturday, 7 April 2012 - 08:19