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Effects of the slowdown of the thermohaline circulation during Heinrich Event 1 and the Younder Dryas Period on the climate of tropical south-western Africa and tropical eastern South America

Effects of the slowdown of the thermohaline circulation during Heinrich Event 1 and the Younder Dryas Period on the climate of tropical south-western Africa and tropical eastern South America
海因里希事件1和雅德尔仙女木期期间温盐环流减慢对热带西南非洲和热带南美洲东部气候的影响
批准号:
5411100
负责人:
Professor Dr. Gerold Wefer
金额:
$0.0万
依托单位国家:
德国
项目类别:
Infrastructure Priority Programmes
财政年份:
2003
资助国家:
德国
项目状态:
已结题
起止时间:
2002-12-31 至 2006-12-31

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中文摘要
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英文摘要
Slow-down of the thermohaline circulation during the Younger Dryas period and Heinrich Event 1 increased the sea surface temperatures of the tropical Atlantic Ocean. This tropical warming would have strong implications for terrestrial climates. It is proposed to investigate the terrestrial climatic change in tropical southwestern Africa and tropical eastern South America during these periods. The effects of slow-down of the thermohaline circulation will be studied in decadal resolution by means of palynology of sediments of ODP Site 1078 and lake sediments from South America. Of special interest are (1) variations in the African south east trade wind system, (2) timing and response of the vegetation to sea surface temperatures fluctuations of the tropical Atlantic, (3) constrains to the migration and average position of the Intertropical Convergence Zone.
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Last glacial maximum/last deglacial South Pacific interannual to decadal climate variability - Sub-seasonal reconstructions from Tahiti reef corals
  • 批准号:
    28791619
  • 项目类别:
    Infrastructure Priority Programmes
  • 资助金额:
    $0.0万
  • 财政年份:
    2006
  • 负责人:
    Professor Dr. Gerold Wefer
  • 依托单位:
Millennial scale deep circulation changes in the North Atlantic during the Plio-Pleistocene inferred from high resolution records of chemical- and physical sediment properties
Millennial-scale changes in position and intensity of the Deep Western Boundary Current (DWBC) during the last glacial period
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