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EAGER: Improving Ice Core Observations of Large Volcanic Eruptions, and Their Effect on Global Climate Change, with a Novel Sulfur Isotope Method

EAGER: Improving Ice Core Observations of Large Volcanic Eruptions, and Their Effect on Global Climate Change, with a Novel Sulfur Isotope Method
EAGER:利用新型硫同位素方法改进大型火山喷发的冰芯观测及其对全球气候变化的影响
批准号:
1340174
负责人:
Jess Adkins
金额:
$14.78万
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2013
资助国家:
美国
项目状态:
已结题
起止时间:
2013-06-01 至 2015-05-31

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中文摘要
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英文摘要
The attribution of modern planetary scale warming between forcings associated with solar output, greenhouse gases, and both natural (volcanic) and anthropogenic aerosols is a challenging and important problem. To date the cooling effect of large volcanic eruptions has been determined by measuring sulfate concentrations in ice cores. However, only volcanoes that inject sulfur dioxide into the stratosphere can cause sustained global cooling as the rain out of new aerosols in the troposphere is very efficient. We need a way to distinguish volcanoes with large amounts of sulfate in the ice core record, but no stratospheric impact (like the Mount St. Helens eruption), from those that reached the stratosphere, so that they can be taken out of the volcanic forcing function in climate attribution studies.Fortunately, injection of SO2 into the stratosphere leaves a mass independent isotopic signal on the sulfur of the resulting sulfate aerosols. This research, led by a professor at the California Institute of Technology, builds on a new technique for measuring sulfur isotopes on small samples that lowers the detection limit the relevant isotopic systems by over three orders of magnitude. This new method will be used to generate a time series of sulfur isotope variability in ice cores of the top 100 volcanic events of the last 1,000 years. The researchers will identify which volcanic eruptions actually entered the stratosphere and therefore caused a global climate cooling. These are the events that must be accounted for in climate warming attribution studies. The research will focus on an ice core from South Greenland. Certain events will be cross-checked in ice cores from Antarctic to confirm the global distribution of sulfate aerosol. The results of this work could be potentially transformative in changing our understanding of the sensitivity of climate to CO2 increases. Outcomes will inform educational outreach efforts. Funding also supports an early career scientist.
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Calcium Carbonate Dissolution Mechanisms in the Ocean
  • 批准号:
    2242211
  • 项目类别:
    Standard Grant
  • 资助金额:
    $63.64万
  • 财政年份:
    2023
  • 负责人:
    Jess Adkins
  • 依托单位:
Collaborative Research: Particle Scavenging Controls on Trace Element Distributions
  • 批准号:
    2124317
  • 项目类别:
    Standard Grant
  • 资助金额:
    $13.96万
  • 财政年份:
    2021
  • 负责人:
    Jess Adkins
  • 依托单位:
Collaborative Research: New approaches to study calcium carbonate dissolution on the sea floor and its impact on paleo-proxy interpretations
  • 批准号:
    1834492
  • 项目类别:
    Standard Grant
  • 资助金额:
    $54.88万
  • 财政年份:
    2018
  • 负责人:
    Jess Adkins
  • 依托单位:
Biomineralization in Deep-sea Corals: Empirical Tracer Calibration Coupled to a Mechanistic Model of Skeletal Growth
  • 批准号:
    1737404
  • 项目类别:
    Standard Grant
  • 资助金额:
    $43.67万
  • 财政年份:
    2017
  • 负责人:
    Jess Adkins
  • 依托单位:
国内基金
海外基金
Improving modelling of compact binary evolution.
  • 批准号:
    10903001
  • 项目类别:
    青年科学基金项目
  • 资助金额:
    20.0万元
  • 批准年份:
    2009
  • 负责人:
    史蒂芬
  • 依托单位: