全新世气候系统的突变及周期性

鲜锋; 周卫健; 余华贵

全新世气候系统的突变及周期性

鲜锋^1,2,
周卫健¹,
余华贵^1,2

1 中国科学院地球环境研究所黄土与第四纪地质国家重点实验室, 西安 710075;
2 中国科学院研究生院, 北京 100049

基金项目:

黄土与第四纪地质国家重点实验室基金(SKLLQG0322)

国家自然科学基金项目(40531003,40121303)

国家重点基础研究发展规划项目(NBRPC 2004 CB720200)

详细信息

作者简介:
鲜锋(1979-),男,博士生,从事地质数据分析及全新世气候演化研究,E-mail:xianf@ieecas.cn

中图分类号: P532
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出版历程
- 收稿日期: 2006-03-05
- 修回日期: 2006-06-21

THE ABRUPT CHANGES AND PERIODICITIES OF CLIMATE DURING HOLOCENE

1 SKLLQG, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China;
2 Graduate School of the Chinese Academy of Sciences, Beijing 100049, China

摘要

摘要: 高纬冰心、海洋沉积物及陆相古气候沉积记录揭示了全新世冰后期(最近1万年以来)存在系列气候突变事件及百年-千年尺度的气候周期韵律,证实了在冰期-间冰期旋回大尺度气候背景下全球气候存在较大不稳定特征这一基本事实。全新世作为与人类文明衔接的最新地质时段,各国科学家针对全新世气候系统变化特征及驱动机制的研究不断取得新的进展,这些成果将为未来气候演化趋势预测提供重要的历史相似性。总结了近年来关于全新世气候系统的突变及周期性研究的一些成果,并进行了概略的评述和展望。
- 气候突变 /
- 百年—千年尺度 /
- 历史相似性 /
- 全新世冰后期
Abstract: Paleoclimatic sequences from the ice core, marine sediments and terrestrial records indicate the serial abrupt climatic changes on centennial-millennial scales during the Holocene, which further confirms the instabilities of climatic system in the background of glacial-interglacial cycles. Holocene is a latest stage that is related to the human being, and great progress has been made in the researches of its climatic evolution history and climatic forcing mechanism. These researches can provide a historical analog for future climatic change and the climatic trend predictions. In this paper, the latest progress in abrupt changes and climatic periodicities during the Holocene are reviewed and some comments are given for the further work in the future.
- abrupt climatic changes /
- centennial-millennial scales /
- historical analog /
- Holocene

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