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Geophysical Institute of the ASCR

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Geomagnetic forcing on regional and global temperatures<br />

We show that inter-annual variations <strong>of</strong> temperature in Europe, North America and over <strong>the</strong> globe at<br />

a time <strong>of</strong> faster warming <strong>of</strong> <strong>the</strong> earth’s surface over <strong>the</strong> past thirty years are influenced by<br />

geomagnetic activity indicating <strong>the</strong> solar wind (Bucha, 2004, 2005). The obtained results help to<br />

distinguish between <strong>the</strong> response to geomagnetic and anthropogenic forcing and contribute to useful<br />

climate forecasts in Europe and North America up to six months in advance.<br />

High correlation coefficients that were found between geomagnetic activity and meteorological<br />

parameters are important for <strong>the</strong> detection <strong>of</strong> causes influencing inter-annual and intra-seasonal<br />

variations <strong>of</strong> regional and global temperatures in <strong>the</strong> past several decades (Bucha and Bucha, 1998,<br />

2002). The positive phase <strong>of</strong> NAO (North Atlantic Oscillation) prevailed from 1973 to 1994. At that<br />

time also geomagnetic activity was highest over <strong>the</strong> past 135 years. We found that <strong>the</strong> NAO as well as<br />

winter temperatures in Europe and in <strong>the</strong> U.S.A. are positively correlated with geomagnetic activity.<br />

Summer temperatures in Europe are also positively correlated (correlation coefficient equals 0.78)<br />

while temperatures in <strong>the</strong> USA are negatively correlated (-0.77) with geomagnetic activity (Bucha,<br />

2005).<br />

aa<br />

50<br />

30<br />

10 64<br />

T(°C)<br />

60<br />

56<br />

a<br />

b<br />

aa<br />

T(°C)<br />

120<br />

100<br />

80<br />

60 65<br />

40<br />

108<br />

104<br />

100 0.4<br />

∆T(°C)<br />

60<br />

T(°C)<br />

55<br />

0.2<br />

0.0<br />

-0.2<br />

c<br />

d<br />

e<br />

f<br />

1970 1980 1990 2000<br />

years<br />

Fig. 38. Time series <strong>of</strong> (a) geomagnetic activity (aa index) for February, (b) surface air temperature in Europe<br />

for <strong>the</strong> sum <strong>of</strong> June-August, (c) geomagnetic activity for <strong>the</strong> sum <strong>of</strong> December – February, (d) surface air<br />

temperature in <strong>the</strong> U.S.A. for <strong>the</strong> sum <strong>of</strong> May – July and (e) for <strong>the</strong> sum <strong>of</strong> May – September, (f) annual<br />

anomalies <strong>of</strong> global temperature.<br />

Successful seasonal forecasts up to six months in advance for Europe and <strong>the</strong> USA could become<br />

a good evidence <strong>of</strong> <strong>the</strong> validity <strong>of</strong> evolutionary processes in <strong>the</strong> atmosphere influenced by<br />

geomagnetic forcing. Preliminary predictions based on <strong>the</strong> positive correlation between geomagnetic<br />

activity (Fig. 38, curve a) and summer temperature in Europe indicate that low geomagnetic activity<br />

in February 2005 influenced <strong>the</strong> temperature in central Europe which was below normal in summer<br />

2005 with probability <strong>of</strong> 70 – 80% (curve b). Vice versa, negative correlation between geomagnetic<br />

activity in winter (curve c) and summer temperature in <strong>the</strong> USA (curve d) shows that <strong>the</strong> US<br />

temperature in summer 2005 probably was higher than was in 2004.<br />

57

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