Why Europe's climate faces a stormy future
Release Date 02 April 2012
Europe is likely to be hit by more violent winter storms in the future. Now a new study into the effects of climate change has found out why.
A weakening of the warm North Atlantic ocean current, the Meridional Overturning Circulation, during the next century has already been predicted by climate scientists, with suggestions it could lead to colder sea temperatures and reduced warming in Britain.
But new research by scientists at the University of Reading's Walker Institute and the University of Cologne suggests that the weakening of the warm current could also partially shut down Europe's protection against violent storms blowing in from the ocean.
The research, published on April 1 in the journal Nature Geoscience, suggests that without such strong warm ocean currents, the regional temperature variations in the North Atlantic will increase.
Such temperature variations, or gradients, help to power storms as they brew up over the ocean. The increase in regional gradients in the Atlantic suggests that the number of storms following a more southerly track, therefore hitting land in Europe, will also increase as greenhouse gas levels rise in the atmosphere.
This is contrary to predictions about changes to storm tracks in other parts of the globe, where increasing temperatures are expected to cause storms to reach higher latitudes than is currently the norm.
The findings are likely to be useful for planners, policy makers and businesses that will need to prepare for the impending changes to our climate in the years ahead.
Dr Tim Woollings, from the University of Reading's Department of Meteorology, said: "From the climate models studied, we expect more storms will hit Europe as the 21st century progresses. We found that changes in ocean currents, in response to increasing levels of greenhouse gases, are crucial in shaping the North Atlantic storm track changes.
"Predictions showed obvious changes to expected weather patterns by the end of the century, but it is not yet clear exactly when this signal may first emerge.
"Predicting future changes to storm patterns can be difficult, and we have shown that in order to improve confidence in these predictions we need to improve our observations and models of ocean currents."
The researchers studied and compared a number of climate models, including those used to help compile the influential fourth assessment report of the Intergovernmental Panel on Climate Change.
For more details, or to organise interviews, please contact Pete Castle at the University of Reading on 0118 378 7391 or email@example.com.
For questions relating only to this paper, please contact co-author Professor Jonathan Gregory, on 01392 884542, on Friday or Saturday only.
Notes to editors
The full paper, ‘Response of the North Atlantic storm track to climate change shaped by ocean-atmosphere coupling', by Woollings, T, JM Gregory, JG Pinto, M Reyers and DJ Brayshaw, is published online by Nature Geoscience at 6pm on 1 April, 2012.
The University of Reading is ranked in the top 1% of universities in the world (THE World University Rankings 2011-12) and is among the top 20 universities in the UK for research funding.
The Walker Institute for Climate System Research at the University of Reading brings together research from across a range of academic disciplines to enhance understanding and improve prediction of the risks and opportunities from our changing climate.