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GEOPHYSICAL RESEARCH LETTERS,
VOL. 28, NO. 15,
PAGES 2959–2962,
2001
Arctic Oscillation signature in a Red Sea coral
Norel Rimbu
Bremen University, Department of Geosciences, Bremen, Germany
Gerrit Lohmann
Bremen University, Department of Geosciences, Bremen, Germany
Thomas Felis
Bremen University, Department of Geosciences, Bremen, Germany
Jürgen Pätzold
Bremen University, Department of Geosciences, Bremen, Germany
Abstract
We show that the winter time series of the Ras Umm Sidd coral oxygen isotope record from the northern Red Sea (approximately
28°N) is linked to the Arctic Oscillation phenomenon, the Northern Hemisphere’s dominant mode of atmospheric variability.
Until now, the detection of this mode, which is most prominent in winter, in proxy climate records was difficult due to the
lack of a clear seasonality in most paleoclimatic archives. The results suggest that northern Red Sea corals can provide information
about the low-frequency variability of the Northern Hemisphere winter circulation during the pre-instrumental period.
Received 26
February
2001;
accepted 24
April
2001.
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Citation: Rimbu, N., G. Lohmann, T. Felis, and J. Pätzold
(2001),
Arctic Oscillation signature in a Red Sea coral,
Geophys. Res. Lett.,
28(15),
2959–2962.
Copyright 2001 by the American Geophysical Union.
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