全新世
古气候学
气候变化
气候学
在现在之前
热带气候
地质学
干旱
全球降温
气候模式
冰期
自然地理学
海洋学
地理
古生物学
考古
作者
Paul A. Mayewski,Eelco J. Rohling,J. Curt Stager,Wibjörn Karlén,Kirk A. Maasch,L. David Meeker,E. A. Meyerson,Françoise Gasse,Shirley van Kreveld,Karin Holmgren,Julia A. Lee‐Thorp,Gunhild Rosqvist,Frank R. Rack,Michael Staubwasser,Ralph R Schneider,Eric J. Steig
出处
期刊:Quaternary Research
[Cambridge University Press]
日期:2004-10-21
卷期号:62 (3): 243-255
被引量:2475
标识
DOI:10.1016/j.yqres.2004.07.001
摘要
Although the dramatic climate disruptions of the last glacial period have received considerable attention, relatively little has been directed toward climate variability in the Holocene (11,500 cal yr B.P. to the present). Examination of ?50 globally distributed paleoclimate records reveals as many as six periods of significant rapid climate change during the time periods 9000"8000, 6000"5000, 4200"3800, 3500"2500, 1200"1000, and 600"150 cal yr B.P. Most of the climate change events in these globally distributed records are characterized by polar cooling, tropical aridity, and major atmospheric circulation changes, although in the most recent interval (600"150 cal yr B.P.), polar cooling was accompanied by increased moisture in some parts of the tropics. Several intervals coincide with major disruptions of civilization, illustrating the human significance of Holocene climate variability.
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