Titlebook: Climatic Variations and Forcing Mechanisms of the Last 2000 Years; Philip D. Jones,Raymond S. Bradley,Jean Jouzel Conference proceedings 1

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arousal

D. Pietrowski,J. Ennker,P. Kleinehe major periods of drought and wetness appear contemporaneous, suggesting a teleconnection for higher-frequency climatic events such as the El Niño-Southern Oscillation (ENSO). Now, for the first time, a longer temporal perspective is available from ice core records and it suggests that lower-frequ

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Femish

Tree-ring variables as proxy-climate indicators: Problems with low-frequency signalsnce of long-term climate change. Other forcings may also be ‘corrupting’ the climate signal in the recent period (that used for calibrating the climate signal). Differences in the origin of the samples or changes in site ecology may also impart an inhomogeneity in the response of tree growth through

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Reconciling the glacial and dendrochronological records for the last millennium in the Canadian Rock and 3 . sites) that routinely cover the last 3–400 years but include millennial chronologies in all 3 species. These records show strong regional suppression in ring-width series corresponding to the early 18th century, mid-19th and late 20th century glacial events plus periods in the mid 14th, mid

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Large-Scale Climatic Influences on Baldcypress Tree Growth Across the Southeastern United Statesvector amplitude series derived from the first three significant principal components of tree growth with northern hemisphere 700 mb heights for spring (March-June) from 1948 to 1980. The strongest relationship discovered was between the first principal component of baldcypress growth (PC1) and spri

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