Collaborative Research: Ice Core Studies Reconstructing Greenland Climate During the Eemian and Beyond

合作研究：冰芯研究重建峨眉纪及以后的格陵兰气候

• 批准号: 1107343
• 负责人: Michael Bender
• 金额: $ 29.56万
• 依托单位: Princeton University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2012
• 资助国家: 美国
• 起止时间: 2012-01-01 至 2015-12-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1107343&HistoricalAwards=false
• 关键词: Collaborative; Research; Ice; Core; Studies

The primary goal of this collaborative project between three institutions is to understand the extent and evolution of the Greenland Ice Sheet (GIS) during the Eemian period (roughly 130,000 to 115,000 years ago, the last major interglacial period in Earth's history) and the deglaciation immediately preceding it ("Termination 2"). The GIS is an important agent influencing sea level, and Arctic and global climate, on multiple timescales. Its dynamics need to be understood in the context of past climate changes, but there is little information available about the footprint, volume, and elevation of the GIS prior to the last ice age due to the absence of continuous ice core records prior to 123,000 years ago. During the Eemian, the GIS was perhaps half its present size, contributing on the order of 3 m to "excess" sea level rise. Characterizing the evolution of the GIS during glacial termination 2 and the Eemian would improve our understanding of its dynamics, and enhance our ability to make projections of sea level rise during the coming centuries. Older ice does exist at the bottoms of previously drilled ice cores, but the extraction of age and climate information from this older ice is hampered by the fact that it is stratigraphically disturbed and, in many cases, contaminated with soil or bedrock material. These investigators propose several novel methods to date this disturbed and/or "dirty" ice and to extract information on climate and ice sheet extent. The investigators will combine their new measurements and other available data to develop a more complete history of the GIS during termination 2 and the Eemian. They will work with ice sheet modelers to investigate the constraints that the Eemian data provide for the models and improve their predictive capability. These efforts have the potential to improve our ability to predict the contribution of the GIS to sea-level rise in the coming decades to centuries. Educational and outreach activities include the training of two graduate students, inclusion of this research in summer teacher enrichment programs, a lecture series for graduate students and postdocs, and communication of the results through the news media.

这个三个机构之间的合作项目的主要目标是了解埃米安时期（大约 130,000 至 115,000 年前，地球历史上最后一个主要间冰期）格陵兰冰盖 (GIS) 的范围和演变，以及在此之前的冰消期（“终止 2”）。 GIS 是在多个时间尺度上影响海平面、北极和全球气候的重要因素。需要在过去的气候变化背景下了解其动态，但由于缺乏 123,000 年前的连续冰芯记录，因此关于最后一个冰河时代之前 GIS 的足迹、体积和海拔的信息很少。在峨眉纪期间，GIS 的大小可能只有现在的一半，导致海平面“过度”上升约 3 m。描述冰川终止期间 2 和峨眉期 GIS 的演化特征将提高我们对其动态的理解，并增强我们预测未来几个世纪海平面上升的能力。较老的冰确实存在于先前钻取的冰芯的底部，但从这些较老的冰中提取年龄和气候信息受到了地层扰动的阻碍，并且在许多情况下受到土壤或基岩材料的污染。这些研究人员提出了几种新方法来测定这种受干扰和/或“脏”冰的年代，并提取有关气候和冰盖范围的信息。研究人员将结合他们的新测量结果和其他可用数据，以开发 GIS 在终止 2 和 Eemian 期间更完整的历史。他们将与冰盖建模者合作，研究埃米亚数据为模型提供的约束，并提高其预测能力。这些努力有可能提高我们预测 GIS 对未来几十年到几个世纪海平面上升的影响的能力。教育和推广活动包括培训两名研究生、将这项研究纳入暑期教师充实计划、为研究生和博士后举办的系列讲座以及通过新闻媒体传播结果。