Continuation of Physical Properties of the Siple Dome Deep Ice Core

单穹顶深冰芯物理特性的延续

• 批准号: 0087160
• 负责人: Richard Alley
• 金额: $ 27.62万
• 依托单位: Pennsylvania State Univ University Park
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2001
• 资助国家: 美国
• 起止时间: 2001-06-01 至 2004-05-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0087160&HistoricalAwards=false
• 关键词: Continuation; Physical; Properties; Siple; Dome

0087160 AlleyThis award provides support to continue paleoclimate and ice dynamical studies of the Siple Dome deep ice core and associated shallow cores from West Antarctica, to help understand the history of climate and ice-sheet stability. Visible examination of the ice cores contributes to the required dating of the paleoclimatic records. Because ice-flow corrections for accumulation rates are difficult in deep ice, a new physically based paleoclimatic indicator of temperature or snow accumulation will be developed, based on bubble-size histories and on the physics of firn densification and grain growth. The paleoclimatic reconstruction of summer temperatures will be accomplished through observation and analysis of the rare melt layers in the ice core. Studies of the distribution of climate change in space and time will be continued, focusing on the possibility that a climate oscillation of ~ 1500 years has combined with "noise" from changes in freshwater fluxes to force rapid, large, nearly synchronous, widespread to global changes in the mode of operation of the climate system. Visual and c-axis studies of ice grains in the core will help detect flow disturbances, such as the ones which were seen in the GISP2 ice cores, if they are present in the Siple Dome core. The results of this study should lead to a better understanding of rapid climate change in Antarctica and, through comparison, to other records worldwide. The study should also contribute to knowledge of the flow and stability of the West Antarctic ice sheet.

0087160 Alley 该奖项为继续对西南极洲 Siple Dome 深冰芯和相关浅层冰芯进行古气候和冰动力学研究提供支持，以帮助了解气候和冰盖稳定性的历史。 对冰芯的肉眼检查有助于确定古气候记录所需的年代。 由于在深冰中对积雪速率进行冰流修正很困难，因此将根据气泡尺寸历史以及冰晶致密化和晶粒生长的物理学，开发一种新的基于物理的温度或积雪古气候指标。 夏季气温的古气候重建将通过对冰芯中稀有融化层的观察和分析来完成。 将继续研究气候变化在空间和时间上的分布，重点关注约1500年的气候振荡与淡水通量变化的“噪音”相结合，迫使全球气候系统运行模式发生快速、大规模、近乎同步、广泛的变化的可能性。 对核心中冰粒的视觉和 c 轴研究将有助于检测流动扰动，例如在 GISP2 冰芯中看到的流动扰动（如果它们存在于 Siple Dome 核心中）。 这项研究的结果应该有助于更好地了解南极洲的快速气候变化，并通过与世界各地的其他记录进行比较。 这项研究还有助于了解南极西部冰盖的流动和稳定性。