Warming Arctic's global impacts outstrip predictions
Posted on 02 September 2009
Warming in the Arctic could lead to flooding affecting one quarter of the world’s population, substantial increases in greenhouse gas emissions from massive carbon pools, and extreme global weather changes, according to a new WWF report.Warming in the Arctic could lead to flooding affecting one quarter of the world’s population, substantial increases in greenhouse gas emissions from massive carbon pools, and extreme global weather changes, according to a new WWF report.
The Arctic Climate Feedbacks: Global Implications report, released today, outlines dire global consequences of a warming Arctic that are far worse than previous projections. The unprecedented peer-reviewed report brings together top climate scientists who have assessed the current science on arctic warming.
"What they found was a truly sobering picture,' said Dr Martin Sommerkorn, senior climate change advisor for WWF’s Arctic programme. 'What this report says is that a warming Arctic is much more than a local problem, it’s a global problem.
"Simply put, if we do not keep the Arctic cold enough, people across the world will suffer the effects."
The report shows that numerous arctic climate feedbacks – negative effects prompted by the impacts of warming -- will make global climate change more severe than indicated by other recent projections, including those of the Intergovernmental Panel on Climate Change’s 2007 assessment.
The dramatic loss of sea ice resulting from the Arctic warming at about twice the rate of the rest of the world will influence atmospheric circulation and weather in the Arctic and beyond. This is projected to change temperature and precipitation patterns in Europe and North America, affecting agriculture, forestry and water supplies.
In addition, the Arctic’s frozen soils and wetlands store twice as much carbon as is held in the atmosphere. As warming in the Arctic continues, soils will increasingly thaw and release carbon into the atmosphere as carbon dioxide and methane, at significantly increased rates. Levels of atmospheric methane, a particularly potent greenhouse gas, have been increasing for the past two years, and it is suggested that the increase comes from warming arctic tundra.
In a first-of-its kind assessment incorporating the fate of the ice sheets of Greenland and West Antarctica into global sea level projections, the WWF report concludes that sea- levels will very likely rise by more than one meter by 2100 -- more than twice the amount given in the Intergovernmental Panel on Climate Change’s 2007 assessment that had excluded the contribution of ice sheets from their projection. The associated flooding of coastal regions will affect more than a quarter of the world’s population.
"This report shows that it is urgently necessary to rein in greenhouse gas emissions while we still can," Sommerkorn said. "If we allow the Arctic to get too warm, it is doubtful whether we will be able to keep these feedbacks under control.
WWF has joined with other NGOs to produce a model climate treaty for Copenhagen that gives the world a blueprint for achieving the kind of emissions cuts needed to likely avoid arctic feedbacks.
"We need to listen now to these signals from the Arctic, and take the necessary action in Copenhagen this December to get a deal that quickly and effectively limits greenhouse gas emissions,” said James Leape, director general of WWF International.
In December 2009, the governments of 191 countries will meet in Copenhagen, Denmark, for the final round of negotiations for a new global agreement on climate change. The first period of the current agreement, called the 'Kyoto Protocol', will end in three years, in December 2012. The negotiations in Copenhagen are supposed to approve a new legal framework for global climate action from 2013 onwards.
According to WWF, this framework must guarantee much deeper and more rapid emission cuts from industrialized countries, and financing to developing countries to enable them also to take climate action.