The Last deglaciation in Greenland: demystifying the mystery interval

格陵兰岛最后一次冰消期：揭开神秘间隔的神秘面纱

• 批准号: 2102944
• 负责人: Christo Buizert
• 金额: $ 48.92万
• 依托单位: Oregon State University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2021
• 资助国家: 美国
• 起止时间: 2021-09-01 至 2024-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2102944&HistoricalAwards=false
• 关键词: Last; deglaciation; Greenland; demystifying; mystery

The ‘last deglaciation’ is the transition from the last Ice Age to our current climate state; a transition that took from approximately 18,000 to 11,000 years ago. The last deglaciation is the most recent natural example of large-scale global warming, which can help scientists better understand scientifically and societally important problems such as the sensitivity of climate to atmospheric carbon dioxide and the sensitivity of the Greenland ice sheet to climate change. The award supports new and improved reconstructions of Greenland temperature and snowfall rates for the last 23,000 years. The work will enhance scientific understanding of Greenland climate history, can improve Greenland ice sheet model simulations of past and future ice loss, and provides a benchmark for climate model simulations. The award supports a graduate student at Oregon State University and a summer undergraduate internship at University of Washington, contributing to the STEM (Science, Technology, Engineering and Mathematics) workforce. The researchers will visit regional middle and high schools annually for a day of polar research. The award supports the further development and professional design of a Climate Feedback boardgame – an active-learning classroom activity for teaching climate feedbacks and their role in global climate change. The researchers will use a new climate reconstruction strategy that combines four independent sources of Greenland climate information from ice cores: borehole temperatures, water stable isotope ratios of ice, isotopic fractionation in atmospheric nitrogen, and methane-based empirical constraints on the ice core gas age-ice age difference; previous reconstructions have only considered two or fewer of such constraints at a time. Targeted high-precision measurements of methane and nitrogen isotopic fractionation (∂15N-N2) will be performed on the Greenland NEEM, NGRIP and GISP2 ice cores to aid these reconstructions, and to replicate recently discovered glacial ∂15N-N2 signals in the GISP2 core. The award supports new model development to incorporate these new sources of climatic information into a single reconstruction. The work further includes a series of hypothesis-driven modeling experiments using a state-of-the-art isotope-enabled climate model that seek to answer the paradoxical observation of an extremely weak near-field Heinrich Event response in Greenland, and a strong far-field response in the global monsoon and tropical hydrology.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

“最后一次冰消期”是从最后一个冰河时代到我们目前的气候状态的转变；这一转变发生在大约 18,000 年前到 11,000 年前，这是大规模全球变暖的最新自然例子，这可能会有所帮助。科学家们更好地了解科学和社会上的重要问题，例如气候对大气二氧化碳的敏感性以及格陵兰冰盖对气候变化的敏感性。该奖项支持对格陵兰岛温度和降雪率进行新的和改进的重建。这项工作将增强对格陵兰岛气候历史的科学理解，可以改进格陵兰岛冰盖模型对过去和未来冰损失的模拟，并为气候模型模拟提供基准。该奖项支持俄勒冈州立大学的一名研究生和一名研究人员。华盛顿大学的暑期本科生实习，为 STEM（科学、技术、工程和数学）劳动力做出贡献。研究人员每年将访问地区初中和高中，进行一天的极地研究。该奖项支持项目的进一步发展和专业设计。气候反馈棋盘游戏——一项主动学习的课堂活动，用于教授气候反馈及其在全球气候变化中的作用。研究人员将使用一种新的气候重建策略，该策略结合了来自冰芯的格陵兰气候信息的四个独立来源：钻孔温度、水稳定同位素比率。冰、大气氮中的同位素分馏以及对冰芯气体年龄-冰年龄差异的基于甲烷的经验约束；以前的重建一次仅考虑了两个或更少的此类约束的有针对性的高精度测量。甲烷和氮同位素分馏 (∂15N-N2) 将在格陵兰 NEEM、NGRIP 和 GISP2 冰芯上进行，以帮助这些重建，并在 GISP2 冰芯中复制最近发现的冰川 ∂15N-N2 信号。该奖项支持新模型。这项工作还包括使用最先进的技术进行一系列假设驱动的建模实验。同位素支持的气候模型，旨在回答格陵兰岛极弱的近场海因里希事件响应和全球季风和热带水文学中强烈的远场响应的矛盾观察。该奖项反映了 NSF 的法定使命，并被视为值得通过使用基金会的智力优点和更广泛的影响审查标准进行评估来支持。

项目成果

Atmospheric methane variability through the Last Glacial Maximum and deglaciation mainly controlled by tropical sources

末次盛冰期和冰消期期间的大气甲烷变化主要由热带源控制

• DOI: 10.1038/s41561-023-01332-x
• 发表时间: 2023-11-27
• 期刊: Nature Geoscience
• 影响因子: 18.3
• 作者: Ben Riddell;J. Rosen;Edward Brook;C. Buizert;Kaden Martin;James E. Lee;J. Edwards;Michae
• 通讯作者: Michae

Bipolar impact and phasing of Heinrich-type climate variability

海因里希型气候变率的两极影响和阶段

• DOI: 10.1038/s41586-023-05875-2
• 发表时间: 2023-05
• 期刊: Nature
• 影响因子: 64.8
• 作者: Martin, Kaden C.;Buizert, Christo;Edwards, Jon S.;Kalk, Michael L.;Riddell;Brook, Edward J.;Beaudette, Ross;Severinghaus, Jeffrey P.;Sowers, Todd A.
• 通讯作者: Sowers, Todd A.

The Ice Core Gas Age‐Ice Age Difference as a Proxy for Surface Temperature

冰芯气体时代——冰河时代差异作为表面温度的代表

• DOI: 10.1029/2021gl094241
• 发表时间: 2021-10
• 期刊: Geophysical Research Letters
• 影响因子: 5.2
• 作者: Buizert; Christo
• 通讯作者: Christo