Collaborative Research: P2C2--Ice Core and Firn Aquifer Studies at Combatant Col, British Columbia, Canada
Collaborative Research: P2C2--Ice Core and Firn Aquifer Studies at Combatant Col, British Columbia, Canada
批准号:
2001961
负责人:
Eric Steig
金额:
$24.69万
依托单位:
依托单位国家:
美国
项目类别:
Continuing Grant
财政年份:
2020
资助国家:
美国
项目状态:
未结题
起止时间:
2020-07-15 至 2025-06-30
中文摘要
该项目旨在恢复加拿大不列颠哥伦比亚省康巴坦特科尔的冰芯,以重建过去500年来的水文气候变化。ComBatant Col以前的工作表明,保存了反映重要气候和环境变量的年度地层、水同位素和地球化学记录,包括大气环流、积雪、火灾活动和跨太平洋尘埃输送。现有的北太平洋冰芯仅位于阿拉斯加和育空地区。战斗科尔显著扩大了冰芯记录的空间覆盖范围,同时提供了不列颠哥伦比亚省西南部独特的水气候记录。该项目将进行详细的雷达调查和冰流模拟,以更好地了解冰川环境,并选择最佳钻探地点。将在不列颠哥伦比亚省北部大学的Hakai冰冻圈节点的支持下,取回从岩心到基岩的后勤。该项目包括对岩心的分析,包括水同位素比值和目视地层学。结合高分辨率雷达成像,来自ComBatant Col的岩芯将被用来确定该地点观测到的积雪含水层(液态水常年储存在冰雪过渡上方)是该地点的一个持久特征,还是最近形成的,并确定其对冰川能量平衡和动力学的影响。岩芯将被存档,供冰芯研究界进行进一步分析。潜在的更广泛的影响包括从战斗科尔冰芯开发出新的水文气候可变性记录,这将为影响不列颠哥伦比亚省和美国太平洋西北部广泛生态系统和人类社区的建模过程提供量化限制。其他潜在的更广泛的影响包括实地工作、培训和参与(冰钻),因为离实地很近,为不同的研究生群体提供便利。研究人员计划将外展活动作为“气候时间”系列研讨会的一部分,在研讨会上将突出战斗科尔遗址的古气候研究。这一奖项反映了NSF的法定使命,并通过使用基金会的智力优势和更广泛的影响审查标准进行评估,被认为值得支持。
英文摘要
This project aims to recover an ice core at Combatant Col, BC, Canada to reconstruct hydroclimate variability over the last 500 years. Previous work at Combatant Col demonstrates preservation of annual stratigraphy, water-isotope and geochemical records reflecting important climate and environmental variables including atmospheric circulation, snow accumulation, fire activity, and trans-Pacific dust transport. Existing North Pacific ice cores are located exclusively in Alaska and the Yukon. Combatant Col significantly expands the spatial coverage of ice core records, while simultaneously providing a unique record of hydroclimate in southwestern British Columbia. This project will conduct detailed radar surveys and ice-flow modeling to better understand the glaciological setting and to select the optimal site for drilling. A core to bedrock will be retrieved with logistics supported by the Hakai Cryosphere Node at the University of Northern British Columbia. Analysis of the core included in this project consists of water isotope ratios and visual stratigraphy. In combination with high-resolution radar imaging, the core from Combatant Col will be used to determine whether the observed firn-aquifer at this site (liquid water is stored perennially above the firn-ice transition) has been a persistent feature at the site, or whether it has formed recently, and to determine its impact on glacier energy balance and dynamics. The core will be archived and made available for additional analyses by the ice-core research community. The potential Broader Impacts include developing a new record of hydroclimate variability from the Combatant Col ice core which will provide quantitative constraints for modeling processes affecting a wide range of ecosystems and human communities in British Columbia and the Pacific Northwest of the United States. Other potential Broader Impacts include field work training and participation (Ice drilling) for a diverse cohort of graduate students facilitated by the proximity of the field site. The researchers plan outreach activities as part of “Climate Time” seminars series in which the paleoclimate research from Combatant Col site will be highlighted.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.
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