Melting Arctic sea ice could increase summer rainfall in northwest Europe

A new study offers an explanation for the extraordinary run of wet summers experienced by Britain and northwest Europe between 2007 and 2012. The study found that loss of Arctic sea ice shifts the jet stream further south than normal resulting in increased rain during the summer in northwest Europe.

Melting Arctic sea ice could increase summer rainfall in northwest Europe
This image shows the average location of the jet stream during wet summer months over northwest Europe. The arrows represent the winds at roughly 10 kilometers above the Earth's surface. The orange and red arrows show the strongest winds that make up the jet stream [Credit: James Screen, University of Exeter]
Dr James Screen from the University of Exeter used a computer model to investigate how the dramatic retreat of Arctic sea ice influences the European summer climate. He found that the pattern of rainfall predicted by the model closely resembles the rainfall pattern of recent summers. The study is published in the journal Environmental Research Letters.

Dr Screen said: "The results of the computer model suggest that melting Arctic sea ice causes a change in the position of the jet stream and this could help to explain the recent wet summers we have seen.

"The study suggests that loss of sea ice not only has an effect on the environment and wildlife of the Arctic region but has far reaching consequences for people living in Europe and beyond."