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P2C2: Investigations on How Polar Climates Communicate with Each Other at the Millennial Timescale

P2C2: Investigations on How Polar Climates Communicate with Each Other at the Millennial Timescale
P2C2:研究极地气候如何在千年时间尺度上相互交流
批准号:
1600784
负责人:
Drew Coleman
金额:
$29.87万
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2016
资助国家:
美国
项目状态:
已结题
起止时间:
2016-07-15 至 2020-06-30

项目摘要

项目成果

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中文摘要
翻译
本项目建立在研究者先前关于千年时间尺度的极地气候与海因里希事件的双极起源之间耦合的研究基础上(即极地同步假说)。研究人员将追求一些研究问题,其中最重要的是:(1)极地同步是如何和何时开始的,以及它是如何演变的?(2)由于耦合意味着信息的通信或交换,被交换的信息的性质是什么?这些科学问题目前还没有答案。主要的更广泛的影响包括对极地气候和半球间气候强迫交流有更深入的科学认识。该项目还包括本科生发现和理解古气候动力学。
英文摘要
This project builds upon previous research by the investigator regarding the coupling between polar climate at millennial time scales and the bi-polar origin of Heinrich events (i.e., the polar synchronization hypothesis). The researcher will pursue a number of research questions, among the most important being: (1) How and when did polar synchronization start, and how did it evolve? and (2) What is the nature of the information being exchanged since coupling implies communication or exchange of information? These scientific questions are currently unanswered.The primary Broader Impacts involve greater scientific understanding of polar climate and inter-hemispheric communication of climate forcing. The project also involves undergraduate students in the discovery and understanding of paleoclimate dynamics.
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会议论文
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A Quantitative Method for Measuring Temperature-time Histories in Hydrothermal Magmatic Ore Systems
Collaborative Research: Caldera Magmatism from the Inside Out: A geochronologic and Geochemical Investigation of Plutonic and Volcanic Rocks in Three Contrasting Calderas
Collaborative Research: Study of the Peruvian flat slab and its effects on the continental lithosphere
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