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Analysis of dendrochronological variability and associated natural climates in eurasia during the last 10,000 years

Exploitable results

Regional timeseries reconstructions of summer temperatures representing large areas of Western United States; western Canada, Eastern Canada, Western Europe, Western Siberia, Eastern Siberia. These reconstructions extend over four centuries or more and are provided as annual estimates with explicit confidence estimates. The data represent interannual to century timescales of variability.
Spatially detailed regression estimates of extended (April-Sept. mean) summer temperatures. Provides year by year indication of past temperature fields over much of the higher latitude regions of the Northern Hemisphere. Potential for many studies related to high-frequency (interannual) temperature variability: in North America, Europe, Fennoscandia, Siberia.

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