H. Malberg et G. Bokens, WINTER AND SUMMER TEMPERATURES IN BERLIN SINCE 1929 AND THEIR RELATIONSHIP WITH THE NORTH-ATLANTIC OSCILLATION (NAG), Meteorologische Zeitschrift, 6(5), 1997, pp. 230-234
As the investigation shows there exists a direct relationship between
the mean winter temperatures in Berlin and the intensity of the circul
ation over the North Atlantic Ocean. The correlation coefficient betwe
en winter temperatures (Dec.-Feb.) and NAO amounts to 0.65 and 0.71 fo
r the winter half-year (Oct.-Mar.). Both values are significant on the
99.9 %-level. The correlation coefficient between summer temperatures
(June-Aug.) and NAO is much weaker. The values are only 0.13 and 0.24
for the summer half-pear (Apr.-Sep.), respectively. Furthermore a rem
arkable increase of the NAO occurs for winter and spring since several
decades, but no increase is observed for summer and fall. The number
of storms over the Northern Atlantic is also significantly correlated
to the NAG.