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Temperature response in the Altai region lags solar forcing
Author(s) -
Eichler Anja,
Olivier Susanne,
Henderson Keith,
Laube Andreas,
Beer Jürg,
Papina Tatyana,
Gäggeler Heinz W.,
Schwikowski Margit
Publication year - 2009
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2008gl035930
Subject(s) - forcing (mathematics) , solar variation , climatology , environmental science , atmospheric sciences , meteorology , geology , geography
The role of the sun on Earth's climate variability is still much debated. Here we present an ice core oxygen isotope record from the continental Siberian Altai, serving as a high‐resolution temperature proxy for the last 750 years. The strong correlation between reconstructed temperature and solar activity suggests solar forcing as a main driver for temperature variations during the period 1250–1850 in this region. The precisely dated record allowed for the identification of a 10–30 year lag between solar forcing and temperature response, underlining the importance of indirect sun‐climate mechanisms involving ocean‐induced changes in atmospheric circulation. Solar contribution to temperature change became less important during industrial period 1850–2000 in the Altai region.