Arctic Oscillation signature in a Red Sea coral


Contact
lohmann [ at ] awi-bremerhaven.de

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.



Item Type
Article
Authors
Divisions
Programs
Publication Status
Published
Eprint ID
11039
Cite as
Rimbu, N. , Lohmann, G. , Felis, T. and Pätzold, J. (2001): Arctic Oscillation signature in a Red Sea coral , Geophysical Research Letters, 28 (15), pp. 2959-2962 .


Download
[thumbnail of Fulltext]
Preview
PDF (Fulltext)
Rim2001a.pdf

Download (296kB) | Preview
Cite this document as:

Share
Add to AnyAdd to TwitterAdd to FacebookAdd to LinkedinAdd to PinterestAdd to Email

Research Platforms
N/A

Campaigns
N/A


Actions
Edit Item Edit Item