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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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发表于 2025-3-21 16:28:14 | 显示全部楼层 |阅读模式
书目名称Climatic Variations and Forcing Mechanisms of the Last 2000 Years
编辑Philip D. Jones,Raymond S. Bradley,Jean Jouzel
视频video
丛书名称Nato ASI Subseries I:
图书封面Titlebook: Climatic Variations and Forcing Mechanisms of the Last 2000 Years;  Philip D. Jones,Raymond S. Bradley,Jean Jouzel Conference proceedings 1
描述A profound knowledge of the past climate is vital for our understanding of global warming. The past 2000 years are both the period which is 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 two sections cover the histories of various forcing factors and attempt to bring together records from a variety of sources and provide explanations.
出版日期Conference proceedings 1996
关键词Climatology; Eisbohrkerne; Global change; Globale Veränderung; Jahresringe; Klimatologie; Meteorologie; cor
版次1
doihttps://doi.org/10.1007/978-3-642-61113-1
isbn_softcover978-3-642-64700-0
isbn_ebook978-3-642-61113-1Series ISSN 1431-7125
issn_series 1431-7125
copyrightSpringer-Verlag Berlin Heidelberg 1996
The information of publication is updating

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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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Christian Möbius,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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