Collaborative Research: P2C2--Western United States Hydroclimate during the Last Interglacial: Developing Proxy Records and Using Model Intercomparison to Glimpse the Future

合作研究：P2C2——末次间冰期美国西部水文气候：开发代理记录并利用模型比对展望未来

• 批准号: 2102885
• 负责人: Warren Sharp
• 金额: $ 22.81万
• 依托单位: Berkeley Geochronology Center
• 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=2102885&HistoricalAwards=false
• 关键词: Collaborative; Research; P2C2; Western; United

Freshwater availability is critical to agricultural, energy and urban systems in the arid to semi-arid western U.S. Quantifying hydroclimate change during past warm periods, such as the Last Interglacial (LIG; ~129,000-116,000 years before present), is essential for evaluating climate model simulations of Earth’s past. This project aims to reconstruct variations in the spatial and seasonal distribution of precipitation in the western U.S. during the LIG during which global temperature are comparable to low-end 21st century projections. The project will include the application of novel methods (calcium and triple oxygen isotopes) on stalagmites from Lake Shasta Caverns (northern California) and Titan Cave (northern Wyoming), and will provide new chronological data and novel measurements (carbonate clumped and triple oxygen isotopes) at four lake sites in the northeast Great Basin (Bear Lake, Utah/Idaho and Bonneville Basin, Utah/Nevada), and southwest Great Basin/Mojave Desert (Lake Manix and Owens Lake, California). The anticipated results of this project are past records of changes in temperature, rainfall amount and moisture source and seasonality. These new past climate records will be integrated into a regional proxy-data network used to benchmark climate model simulations of the Last Interglacial period (127 ka).The paleoclimate modeling intercomparison (PMIP4) and coupled model intercomparison project (CMIP6) efforts of the climate modeling community include Tier 1 LIG (127ka) simulations as a benchmarking target for models with similar CO2 levels, different orbital configuration, unchanged topography and higher sea level. The validation of hydroclimate-relevant variables at a regional scale using climate models requires robustly dated and spatially distributed paleoclimate observations in order to place the LIG water cycle in the western U.S. in the context of geologic and future climate change. Yet, few quantitative estimates of paleoclimate exist for this interval, which offers geochronologic challenges too as it is beyond the limit of radiocarbon age control. This project seeks to improve our understanding of LIG climate in the western U.S. by providing: 1) new observations from speleothem records, 2) new U-Th dating of existing lake cores, and 3) the application of novel semi-quantitative proxies for temperature, precipitation and humidity to speleothems and lake sediments. Through the development of new high-resolution proxy time-series from speleothems and lake sediments, we will provide new insight into the behavior of the North American Monsoon during a past warm period and reconstruct hydroclimatic response to abrupt climatic events during the penultimate deglaciation (Termination II) and Marine Isotope Stage 5 (MIS5). The research uses existing lake cores recovered and archived by previous NSF- and USGS-funded continental drilling projects, and recently collected speleothems known to span much of MIS5 and the LIG.The potential Broader Impacts include quantifying regional hydroclimate changes during past warm periods and benchmarking of climate model simulations for the last interglacial. Other Broader Impacts include translating the project research outcomes via a workshop (paleo to policy) convening water resource managers, government agencies (e.g., USGS), climate and weather risk assessment and projection companies and early career paleoclimate researchers from across the U.S. This workshop will emphasize on the information that terrestrial past climate records (lake sediments, tree rings, speleothems) can provide in terms of hydroclimate data beyond the instrumental records needed by policy makers to assess climate variability and extreme events such as drought and floods. The researchers will produce a white paper, policy briefs for water resource managers and a presentation at an education and outreach session at a scientific meeting (American Geophysical Union). The project will provide scientific training, mentorship and professional development for two graduate students and one postdoctoral researcher. Through joint field trips and collaborations, these students and postdoc will have opportunities to develop interdisciplinary expertise in climate archives, novel proxy systems, geochronology and model-proxy comparison. In addition, the researchers will recruit undergraduate students to complete summer internships related to the project. The undergraduate students will be recruited through (1) the Earth Horizons program and partnership between Vanderbilt University and Tennessee State University, a Historically Black University (HBCU); (2) the Leadership Alliance program at Brown University funded through NSF-REU-EPSCOR. The undergraduate students will be encouraged to develop their research into presentations at regional, national and international scientific meetings (e.g., AGU, GSA).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.

淡水供应对于美国干旱至半干旱西部地区的农业、能源和城市系统至关重要。量化过去温暖时期（例如末次间冰期（LIG；距今约 129,000-116,000 年））期间的水文气候变化对于评估气候至关重要该项目旨在重建 LIG 期间美国西部降水空间和季节分布的变化，在此期间全球温度与该项目将包括对沙斯塔湖洞穴（加利福尼亚州北部）和泰坦洞穴（怀俄明州北部）的石笋应用新方法（钙和三氧同位素），并将提供新的年代数据和新的测量结果。 （碳酸盐团块和三氧同位素）位于大盆地东北部的四个湖点（熊湖、犹他州/爱达荷州和邦纳维尔盆地，该项目的预期结果是过去的温度、降雨量和水分来源和季节的变化记录。被整合到一个区域代理数据网络中，用于对末次间冰期（127ka）的气候模型模拟进行基准测试。古气候模型比对（PMIP4）和耦合模型比对项目（CMIP6）气候建模界的努力包括将 Tier 1 LIG (127ka) 模拟作为具有相似二氧化碳水平、不同轨道配置、未改变地形和较高海平面的模型的基准目标，使用气候模型在区域范围内验证与水文气候相关的变量。需要可靠的日期和空间分布的古气候观测，以便将美国西部的 LIG 水循环置于地质和未来气候变化的背景下，然而，对此古气候的定量估计很少。间隔，这也带来了地质年代学的挑战，因为它超出了放射性碳年龄控制的限制。该项目旨在通过提供：1）来自洞穴记录的新观察结果，2）新的 U-Th 测年来提高我们对美国西部 LIG 气候的了解。现有湖泊核心的数据，以及3）通过开发新的高分辨率代理时间序列，将温度、降水和湿度的新型半定量代理应用于洞穴沉积物和湖泊沉积物。通过洞穴沉积物和湖泊沉积物，我们将为过去温暖时期的北美季风行为提供新的见解，并重建对倒数第二次冰消期（终止 II）和海洋同位素阶段 5（MIS5）期间突然气候事件的水文气候响应。使用由先前 NSF 和 USGS 资助的大陆钻探项目回收和存档的现有湖芯，以及最近收集的已知跨越 MIS5 和 MIS5 大部分地区的洞穴岩LIG。潜在的更广泛的影响包括量化过去温暖时期的区域水文气候变化以及对最后一次间冰期的气候模型模拟进行基准测试。其他更广泛的影响包括通过召集水资源管理者、政府机构的研讨会（古到政策）转化项目研究成果。 （例如，美国地质调查局）、气候和天气风险评估和预测公司以及来自美国各地的早期职业古气候研究人员。本研讨会将强调陆地过去气候记录（湖泊）的信息沉积物、树木年轮、洞穴沉积物）可以提供超出政策制定者评估气候变化和干旱和洪水等极端事件所需的工具记录的水文气候数据。在科学会议（美国地球物理联盟）的教育和推广会议上的演讲 该项目将为两名研究生和一名博士后研究员提供科学培训、指导和专业发展，这些学生和博士后将通过联合实地考察和合作。有机会发展气候档案、新型代理系统、地质年代学和模型代理比较方面的跨学科专业知识。此外，研究人员将招募本科生来完成与该项目相关的暑期实习。本科生将通过（1）地球地平线计划招募。范德比尔特大学和田纳西州立大学（HBCU）之间的合作；（2）由 NSF-REU-EPSCOR 资助的布朗大学领导力联盟项目将鼓励本科生将他们的研究发展到地区演讲中。 ,国家和国际科学会议（例如，AGU、GSA）。该奖项反映了 NSF 的法定使命，并通过使用基金会的智力价值和更广泛的影响审查标准进行评估，被认为值得支持。