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Millennial Cycles in Equatorial Atlantic Sediments: A Presumed Solar-Forced, Wind-Controlled Phenomenon Important in Modeling Ocean/Climate Dynamics

Millennial Cycles in Equatorial Atlantic Sediments: A Presumed Solar-Forced, Wind-Controlled Phenomenon Important in Modeling Ocean/Climate Dynamics
赤道大西洋沉积物的千年周期：推测的太阳驱动、风控现象对于海洋/气候动力学建模非常重要
批准号：
9313821
负责人：
Andrew McIntyre
金额：
$31.16万
依托单位：
Columbia University
依托单位国家：
美国
项目类别：
Continuing Grant
财政年份：
1994
资助国家：
美国
项目状态：
已结题
起止时间：
1994-02-15 至 1998-01-31
来源：
https://www.nsf.gov/awardsearch/showAward?AWD_ID=9313821&HistoricalAwards=false
关键词：
MillennialCyclesEquatorialAtlanticSediments

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英文摘要
9313821 McIntyre The goal of this study is to determine if solar forcing alters climate at the millennial time scales with the help of calcareous planktonic and isotopic proxies. This will be done in three steps. First, the response of surface waters of equatorial Atlantic to climate controlled wind variations will be documented. Second, these signals will be compared with time series from other regions to determine if these short period signals are global. Third, a sine wave signal of millennial response of ocean/climate will need constructed which can be used bother for comparison with other records and as a predictive template.
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Atlantic Interhemispheric Heat Transport Workshop, Palisades, New York, September 11-12, 1995
  • 批准号：
    9526835
  • 项目类别：
    Standard Grant
  • 资助金额：
    $0.6万
  • 财政年份：
    1995
  • 负责人：
    Andrew McIntyre
  • 依托单位：
    Columbia University
Heat Cycles of the Tropical Ocean Reservoir at Orbital Frequencies in the Pleistocene: Paleoestimation Part II
  • 批准号：
    9114955
  • 项目类别：
    Standard Grant
  • 资助金额：
    $7.0万
  • 财政年份：
    1991
  • 负责人：
    Andrew McIntyre
  • 依托单位：
    Columbia University
A Unique Paleomeasure of Turbulent Boundary Layer Heat Content: Florisphaera Profunda
  • 批准号：
    8911841
  • 项目类别：
    Continuing Grant
  • 资助金额：
    $20.16万
  • 财政年份：
    1989
  • 负责人：
    Andrew McIntyre
  • 依托单位：
    Columbia University
Documenting Atlantic South Equatorial Current Variations, O-140Ka, to Determine Causality
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