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JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 106, NO. D3,
PAGES 2929–2941,
2001
Low-frequency temperature variations from a northern tree ring density network
Keith R. Briffa
Timothy J. Osborn
Fritz H. Schweingruber
Ian C. Harris
Philip D. Jones
Stepan G. Shiyatov
Eugene A. Vaganov
Abstract
We describe new reconstructions of northern extratropical summer temperatures for nine subcontinental-scale regions and a
composite series representing quasi “Northern Hemisphere” temperature change over the last 600 years. These series are based
on tree ring density data that have been processed using a novel statistical technique (age band decomposition) designed to
preserve greater long-timescale variability than in previous analyses. We provide time-dependent and timescale-dependent uncertainty
estimates for all of the reconstructions. The new regional estimates are generally cooler in almost all precalibration periods,
compared to estimates obtained using earlier processing methods, particularly during the 17th century. One exception is the
reconstruction for northern Siberia, where 15th century summers are now estimated to be warmer than those observed in the
20th century. In producing a new Northern Hemisphere series we demonstrate the sensitivity of the results to the methodology
used once the number of regions with data, and the reliability of each regional series, begins to decrease. We compare our
new hemisphere series to other published large-regional temperature histories, most of which lie within the 1σ confidence
band of our estimates over most of the last 600 years. The 20th century is clearly shown by all of the palaeoseries composites
to be the warmest during this period.
Received 10
July
2000;
accepted 13
September
2000.
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Citation: Briffa, K. R., T. J. Osborn, F. H. Schweingruber, I. C. Harris, P. D. Jones, S. G. Shiyatov, and E. A. Vaganov
(2001),
Low-frequency temperature variations from a northern tree ring density network,
J. Geophys. Res.,
106(D3),
2929–2941.
Copyright 2001 by the American Geophysical Union.
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