Arctic Oscillation signature in a Red Sea coral

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...

Full description

Saved in:
Bibliographic Details
Published in:Geophysical research letters Vol. 28; no. 15; pp. 2959 - 2962
Main Authors: Rimbu, Norel, Lohmann, Gerrit, Felis, Thomas, Pätzold, Jürgen
Format: Journal Article
Language:English
Published: Washington, DC Blackwell Publishing Ltd 01-08-2001
American Geophysical Union
Subjects:
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary: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.
Bibliography:ArticleID:2001GL013083
ark:/67375/WNG-6GTPHKBD-D
istex:91989AC0E022DBF02C26AEE4F53136C0B10DB905
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0094-8276
1944-8007
DOI:10.1029/2001GL013083