Arctic melt and summer temperature during past warm periods: a new ice core proxy

过去温暖时期的北极融化和夏季温度：新的冰芯代理

• 批准号: 2140500
• 负责人: Christo Buizert
• 金额: $ 52.98万
• 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: 2022
• 资助国家: 美国
• 起止时间: 2022-02-01 至 2025-01-31
• 项目状态: 未结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2140500&HistoricalAwards=false
• 关键词: Arctic; melt; summer; temperature; during

Glacier ice melt in the Arctic has profound impacts on local communities, ecosystems and infrastructure, and global sea level. Long-term records of past ice melt help scientists better understand the processes that contribute to ice melt, such as summer air temperatures and the concentration of soot and other particles in the ice that absorb sunlight. In particular, past warm periods are important to study because they provide potential analogs for our future climate. One method to reconstruct past surface melt is through visual detection of bubble-free layers. However, beyond approximately 5000 years, the melt layers are no longer visible because the ice layers get strongly thinned by ice flow and because the air bubbles dissolve into the ice crystals. This award supports the development of a new technique to reconstruct past melt in Arctic ice cores and the application of this technique to study past warm periods in Arctic ice cores from Greenland and Alaska. The award supports a graduate student at Oregon State University, contributing to the STEM (Science, Technology, Engineering and Mathematics) workforce. The researchers will develop lesson materials on ice cores and climate change for middle and high school students from underserved regions, host two STEM teacher workshops at OSU, and to support student clubs across Oregon rural communities.Glacier ice cores preserve a record of past surface melting that can be used for understanding past variability in melt intensity in response to climate forcing - either natural or anthropogenic. Researchers have traditionally reconstructed past surface melt in ice cores using visual detection of bubble-free layers. Unfortunately, this method does not work for old and/or deep ice, where melt layers can no longer be visually identified. The investigator will apply a new ice core proxy for surface melt intensity: the xenon/nitrogen ratio. In the absence of refrozen meltwater, the xenon/nitrogen ratio in ice samples reflects the atmospheric ratio. However, because of the high solubility of xenon, the xenon/nitrogen ratio becomes strongly enriched in the presence of surface melt. The investigator will use this proxy to address four important scientific questions: (1) what is the timing and magnitude of the Holocene Thermal Maximum in the Arctic; (2) what is the extent and magnitude of Greenland melt during the Last Interglacial period; (3) what are the drivers of Arctic melt on long time scales; and (4) how do current melt rates in the Arctic compare to the last 10,000 years. The investigator proposes measurements on the Renland and GISP2 ice cores (both from Greenland), and the Mt. Hunter ice core (from Alaska). The xenon/nitrogen melt proxy will be calibrated to reconstruct local summer temperature. The proposed work uses existing ice core samples and does not involve Arctic fieldwork. The award supports a graduate student at Oregon State University, contributing to the STEM (Science, Technology, Engineering and Mathematics) workforce. The researchers will develop lesson materials on ice cores and climate change for middle and high school students from underserved regions, host two STEM teacher workshops at OSU, and to support student clubs across Oregon rural communities.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.

北极冰川融化对当地社区、生态系统和基础设施以及全球海平面都有深远的影响。对过去冰川融化的长期记录有助于科学家更好地了解导致冰川融化的过程，例如夏季气温以及冰层中吸收阳光的煤烟和其他颗粒的浓度。特别是，过去的暖期对研究很重要，因为它们为我们未来的气候提供了潜在的相似之处。重建过去表面熔化的一种方法是通过视觉检测无气泡层。然而，在大约5000年后，融化的冰层不再可见，因为冰流使冰层变得非常薄，而且气泡溶解成冰晶。该奖项支持开发一种重建北极冰芯过去融化的新技术，并将这一技术应用于研究格陵兰和阿拉斯加北极冰芯过去的暖期。该奖项资助俄勒冈州立大学的一名研究生，为STEM(科学、技术、工程和数学)劳动力做出贡献。研究人员将为服务不足地区的初中生和高中生开发关于冰芯和气候变化的课程材料，在俄勒冈州州立大学举办两个STEM教师研讨会，并支持俄勒冈州农村社区的学生俱乐部。冰芯保存了过去表面融化的记录，可以用来了解过去在应对气候强迫(无论是自然的还是人为的)融化强度的变化。研究人员传统上通过目测无气泡层来重建冰芯过去的表面融化。不幸的是，这种方法不适用于旧冰和/或深冰，因为在那里，融化的冰层不再能被肉眼识别。研究人员将应用一种新的冰芯替代表面融化强度：氙气/氮的比率。在没有重新冻结的融化水的情况下，冰样中的氙氮比反映了大气比。然而，由于Xe的高溶解度，在表面熔体的存在下，Xe/N比变得非常丰富。调查人员将利用这一指标来解决四个重要的科学问题：(1)北极全新世最热的时间和级别；(2)上一次间冰期格陵兰融化的范围和规模；(3)在长时间尺度上，北极融化的驱动因素是什么；以及(4)北极目前的融化速度与过去10,000年相比如何。调查人员建议对Renland和GISP2冰芯(均来自格陵兰岛)和山顶进行测量。亨特冰芯(来自阿拉斯加)。将对氙气/氮熔体代理进行校准，以重建当地夏季温度。拟议中的工作使用现有的冰芯样本，不涉及北极实地考察。该奖项资助俄勒冈州立大学的一名研究生，为STEM(科学、技术、工程和数学)劳动力做出贡献。研究人员将为服务不足地区的初中生和高中生开发关于冰芯和气候变化的课程材料，在俄勒冈州州立大学主办两个STEM教师研讨会，并支持俄勒冈州农村社区的学生俱乐部。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。