Cold European winters: interplay between the NAO and the East Atlantic mode

Western Europe has experienced a sequence of unusually cold winters culminating in December 2010, which was the coldest December in the United Kingdom for over 100 years. The North Atlantic Oscillation (NAO) is the most important indicator of the climate of the North Atlantic and Western Europe. How...

Full description

Saved in:
Bibliographic Details
Published inAtmospheric science letters Vol. 13; no. 1; pp. 1 - 8
Main Authors Moore, G. W. K., Renfrew, I. A.
Format Journal Article
LanguageEnglish
Published Chichester, UK John Wiley & Sons, Ltd 01.01.2012
John Wiley & Sons, Inc
Subjects
Atmospheric forcing
Central England Temperature
Climate science
Cold winters
Icelandic Low
North Atlantic Oscillation
Ocean-atmosphere system
Precipitation
Teleconnection patterns
Temperature
England
United Kingdom > UK
Northern Hemisphere
Ireland
Europe
Greenland
Online AccessGet full text

Cover

More Information
Summary:Western Europe has experienced a sequence of unusually cold winters culminating in December 2010, which was the coldest December in the United Kingdom for over 100 years. The North Atlantic Oscillation (NAO) is the most important indicator of the climate of the North Atlantic and Western Europe. However, in this article, we argue that the record cold temperatures in December 2010 cannot be explained by appeal to the NAO alone. Rather we show that the consideration of another atmospheric teleconnection pattern, the East Atlantic (EA) pattern, provides for a more robust explanation as to why December 2010 was so cold. Copyright © 2011 Royal Meteorological Society
ISSN:1530-261X
1530-261X
DOI:10.1002/asl.356