Wednesday, April 02, 2014

Warm North Atlantic Ocean Promotes Extreme Winters in US and Europe

Time series and complimentary modes of the Pacific Decadal Oscillation (PDO) and Atlantic Multidecadal Oscillation (AMO). Shaded areas indicate combinations of positive (+) and negative (-) PDO and AMO periods. Note -PDO, +AMO modes in the 1950s and 1999-2003, when severe drought gripped much of the western U.S. (Credit: US Geological Survey) Click to enlarge.
The extreme cold weather observed across Europe and the east coast of the US in recent winters could be partly down to natural, long-term variations in sea surface temperatures, according to a new study published today.

Researchers from the University of California Irvine have shown that a phenomenon known as the Atlantic Multidecadal Oscillation (AMO) -- a natural pattern of variation in North Atlantic sea surface temperatures that switches between a positive and negative phase every 60-70 years -- can affect an atmospheric circulation pattern, known as the North Atlantic Oscillation (NAO), that influences the temperature and precipitation over the Northern Hemisphere in winter.

When the AMO is in its positive phase and the sea surface temperatures are warmer, the study has shown that the main effect in winter is to promote the negative phase of the NAO which leads to "blocking" episodes over the North Atlantic sector, allowing cold weather systems to exist over the eastern US and Europe.

The results have been published today, Wednesday 2 April, in IOP Publishing's journal Environmental Research Letters.

Warm North Atlantic Ocean Promotes Extreme Winters in US and Europe

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