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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:
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

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中文摘要
翻译
9313821麦金太尔:这项研究的目标是借助钙质浮游生物和同位素替代物,确定太阳强迫是否在千年时间尺度上改变了气候。这将分三个步骤完成。首先,将记录赤道大西洋表层水对气候控制的风变化的响应。其次,将这些信号与其他地区的时间序列进行比较,以确定这些短周期信号是否为全球信号。第三,需要构建海洋/气候千年响应的正弦波信号,以便与其他记录进行比较,并作为预测模板。
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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会议论文
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:
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:
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:
Documenting Atlantic South Equatorial Current Variations, O-140Ka, to Determine Causality
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