Temperature response in the Altai region lags solar forcing
Article first published online: 15 JAN 2009
Copyright 2009 by the American Geophysical Union.
Geophysical Research Letters
Volume 36, Issue 1, January 2009
How to Cite
2009), Temperature response in the Altai region lags solar forcing, Geophys. Res. Lett., 36, L01808, doi:10.1029/2008GL035930., , , , , , , and (
- Issue published online: 15 JAN 2009
- Article first published online: 15 JAN 2009
- Manuscript Accepted: 5 DEC 2008
- Manuscript Revised: 1 DEC 2008
- Manuscript Received: 6 SEP 2008
Auxiliary material for this article contains a text file, five figures, and one table.
Auxiliary material files may require downloading to a local drive depending on platform, browser, configuration, and size. To open auxiliary materials in a browser, click on the label. To download, Right-click and select “Save Target As…” (PC) or CTRL-click and select “Download Link to Disk” (Mac).
See Plugins for a list of applications and supported file formats.
Additional file information is provided in the readme.txt.
|grl25285-sup-0001-readme.txt||plain text document||9K||readme.txt|
|grl25285-sup-0002-txts01.txt||plain text document||6K||Text S1. Sample preparation, dating, δ18O analyses, and calibration.|
|grl25285-sup-0003-fs01.eps||PS document||5911K||Figure S1. Location of the study site in the Siberian Altai and spatial variation of δ18O responses in central and southeast Asia.|
|grl25285-sup-0004-fs02.eps||PS document||188K||Figure S2. Signature of the Tambora eruption in the ice core.|
|grl25285-sup-0005-fs03.eps||PS document||129K||Figure S3. Annual record of Belukha δ18O and March–November Barnaul temperature and correlation between 10-year δ18O and March–November temperature means.|
|grl25285-sup-0006-fs04.eps||PS document||221K||Figure S4. Temperature reconstructions for the Altai, different regions in central Asia, and the Northern Hemisphere together with the reconstructed solar activity based on 10Be.|
|grl25285-sup-0007-fs05.eps||PS document||297K||Figure S5. Cross correlation between Altai temperature reconstruction and 14C based solar activity.|
|grl25285-sup-0008-ts01.txt||plain text document||0K||Table S1. Correlation coefficient between the 10Be and 14C based solar modulation and the respective temperature reconstruction for the periods 1250–2000 and 1250–1850.|
Please note: Wiley Blackwell is not responsible for the content or functionality of any supporting information supplied by the authors. Any queries (other than missing content) should be directed to the corresponding author for the article.