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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Conference proceedings 1996levance to the next century and that for which there is the most evidence. High-resolution proxy records for this period are available from a variety of sources. Five sections consider dendroclimatology, ice cores, corals, historical records, lake varves, and other indicators. The final two sections

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1431-7125 of most relevance to the next century and that for which there is the most evidence. High-resolution proxy records for this period are available from a variety of sources. Five sections consider dendroclimatology, ice cores, corals, historical records, lake varves, and other indicators. The final tw

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nutrition

Christian M?bius,Catherine Pallenbergtion on how or if certain climatic features of the past millennium (the Medieval Warm Epoch and Little Ice Age) were manifested in the northern Americas; Canada and the U. S. state of Alaska. These data are also valuable for determining how such natural fluctuations compare to recent, possibly anthropogenic climatic change.

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Introductionuctuations and cycles have occurred on longer timescales. We live in an interglacial climate, a warm phase on the 10,000 year timescale, in a period known as the Quaternary, dominated for the most part by Ice Age Climates.

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