Abstract
Boreal winter 2009–2010 made headlines for cold anomalies in many countries of the northern mid-latitudes. Northern Europe
was severely hit by this harsh winter in line with a record persistence of the negative phase of the North Atlantic Oscillation
(NAO). In the present study, we first provide a wider perspective on how unusual this winter was by using the recent 20th
Century Reanalysis. A weather regime analysis shows that the frequency of the negative NAO was unprecedented since winter
1939–1940, which is then used as a dynamical analog of winter 2009–2010 to demonstrate that the latter might have been much
colder without the background global warming observed during the twentieth century. We then use an original nudging technique
in ensembles of global atmospheric simulations driven by observed sea surface temperature (SST) and radiative forcings to
highlight the relevance of the stratosphere for understanding if not predicting such anomalous winter seasons. Our results
demonstrate that an improved representation of the lower stratosphere is necessary to reproduce not only the seasonal mean
negative NAO signal, but also its intraseasonal distribution and the corresponding increased probability of cold waves over
northern Europe.
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