Collaborative Research: Climatic instability in interior Alaska from the isotopic record of Late Quaternary ground ice.

合作研究：来自晚第四纪地冰同位素记录的阿拉斯加内陆气候不稳定。

• 批准号: 0714058
• 负责人: Matthew Lachniet
• 金额: $ 18.27万
• 依托单位: University of Nevada Las Vegas
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2007
• 资助国家: 美国
• 起止时间: 2007-09-15 至 2011-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0714058&HistoricalAwards=false
• 关键词: Collaborative; Research; Climatic; instability; interior

Intellectual Merit : Preliminary results of 14C-dated periglacial ice wedge growth intervals and d18O profiles suggest that the last glacial climate in Arctic Alaska was characterized by millennial-scale variability. These abrupt events are characterized by alternating ice wedge growth and at least seven thaw periods over the interval of 45,000 to 20,000 yrs BP. A decrease in ice wedge d18O values with decreasing ice age indicates gradual cooling during cold stadial climates. The hypothesis that these millennial-scale ice-wedge growth/thaw events are arctic manifestations of northern hemisphere stadials and the nine warm Dansgaard/Oeschger events (stadials 3-11) evident in Greenland Ice is evaluated. To test the hypothesis, ice wedges will be dated by 14C of entrapped organic material, and paleoclimate conditions estimated via the generation of d18O and dD time series, a proxy for winter air temperature. If the hypothesis is correct, it will indicate that the abrupt and severe millennial-scale climate changes strongly manifested in Greenland and the circum-North Atlantic have a hemispheric spatial fingerprint, and highlight the sensitivity of permafrost areas to global climate change on millennial time scales. This research will utilize the unique ground ice record in the Quaternary age permafrost in the Cold Regions Research CRREL Permafrost Tunnel near Fairbanks, Alaska, under controlled and Engineering Lab (CRREL) environmental conditions that allow precise sampling in subfreezing temperatures linked to a detailed and rigorous analysis of the sediments and ice and their sedimentary and thermal history.Broader Impacts: Due to a paucity of paleoclimatic data from Arctic and permafrost regions, this work will document the sensitivity of Arctic climate to global climate changes. Few data from the last glacial period are available from Arctic environments to calibrate global climate models, thus limiting scientists' ability to predict future climate change associated with anthropogenic global warming. Yet the effects of global warming are already documented in Arctic regions where native cultures, villages and ways of life will be severely affected by large or rapid changes in climate. The detailed stable isotopic analyses of ice wedges and ground ice will provide a high resolution proxy data source for unglaciated regions of the Arctic, filling an important data gap in our understanding of ice-ocean-atmosphere interactions in global climate. Research will be a collaborative effort, supporting undergraduate and graduate students at Dartmouth College and University of Nevada-Las Vegas.

智力优势：14 C测年冰缘冰楔生长间隔和d18 O剖面的初步结果表明，阿拉斯加北极地区末次冰期气候的特点是千年尺度的变化。这些突发事件的特征是交替的冰楔生长和至少7个解冻期在45,000至20,000年BP的时间间隔。冰楔d18 O值随冰期的减小而减小，表明在寒冷的气候条件下逐渐变冷。假设这些千年尺度的冰楔增长/融化事件是北极的表现北方半球stadials和9个温暖的Dansgaard/Oeschger事件（stadials 3-11）明显在格陵兰岛的冰进行了评估。 为了验证这一假设，冰楔将被14 C的截留有机物质，和古气候条件估计通过生成的d18 O和dD时间序列，冬季气温的代理。如果这一假设是正确的，它将表明格陵兰岛和环北大西洋地区强烈表现出的突然和严重的千年尺度气候变化具有半球空间指纹，并突出了永久冻土区对千年时间尺度上全球气候变化的敏感性。这项研究将利用阿拉斯加州费尔班克斯附近寒冷地区研究CRREL永久冻土隧道中第四纪永久冻土的独特地面冰记录，在受控和工程实验室（CRREL）环境条件下，允许在冰点以下温度进行精确采样，并对沉积物和冰及其沉积和热历史进行详细和严格的分析。 由于缺乏北极和永久冻土区的古气候数据，这项工作将记录北极气候对全球气候变化的敏感性。 从北极环境中获得的最后一次冰期的数据很少，无法校准全球气候模型，因此限制了科学家预测与人为全球变暖相关的未来气候变化的能力。然而，全球变暖的影响已经在北极地区记录在案，那里的土著文化，村庄和生活方式将受到气候大规模或快速变化的严重影响。冰楔和地冰的详细稳定同位素分析将为北极无冰川地区提供高分辨率的代用数据源，填补我们在了解全球气候中冰-海洋-大气相互作用方面的重要数据空白。 研究将是一个合作的努力，支持本科生和研究生在达特茅斯学院和内华达大学拉斯维加斯分校。