Collaborative Research: P2C2--Speleothem Constraints on Seasonal Hydroclimate Variability in Mainland Southeast Asia since the Late Pleistocene

合作研究：P2C2--晚更新世以来东南亚大陆洞穴水文季节变化的制约

• 批准号: 2102976
• 负责人: William McGee
• 金额: $ 16.41万
• 依托单位: Massachusetts Institute of Technology
• 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: 2021-07-01 至 2024-06-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2102976&HistoricalAwards=false
• 关键词: Collaborative; Research; P2C2; Speleothem; Constraints

This project aims to characterize the Asian summer and winter monsoon circulation and local hydroclimate across Mainland Southeast Asia (MESA) during the last ~45 thousand years using a suite of speleothem records from caves that extend across a critical geographical divide between Laos and Vietnam, two countries with very distinct seasonal rainfall climatologies. The overarching goal of this work is to explore the dynamic response of summer and winter Asian monsoon variability to changing external drivers, such as insolation, and internal climate variability which will contribute to improved understanding of large-scale hydrological variability in a vulnerable region. Specifically, the researchers will develop a new set of past climate records utilizing multiple environmental tracers (Carbon and Oxygen isotopes, trace elements such as Magnesium/Calcium, radiocarbon) in precisely dated speleothems spanning at least the last ~45 thousand years. Additionally, a detailed cave monitoring program will aid the interpretation of data obtained from the speleothems. The results will be integrated with other regional and global records of past climate variability and state-of-the-art climate model simulations to diagnose the dominant mechanisms driving hydroclimate variability on sub-decadal to millennial timescales in the MESA region. The research will address the following specific objectives: (1) Determine the summer and fall/winter response of MSEA hydroclimate to orbital and millennial-scale forcing, (2) Determine the response of MSEA hydroclimate to decadal to multidecadal scale sea surface temperature variability, and (3) Synthesize data with other available records to elucidate the spatiotemporal patterns of MSEA hydroclimate, which, combined with paleoclimate model analyses, will allow us investigation of the dynamical mechanisms underlying summer and fall/winter monsoon variability. Speleothem oxygen isotope records from three study sites will serve as a proxy for summer monsoon intensity, dominated by the degree of upstream rainout over the Indian Ocean and trace element measurements will provide robust evidence for past variations in local water balance at each cave site, with Laos sites recording summer rainfall and Vietnam sites recording fall/winter rainfall.The potential Broader Impacts include a better understanding of the monsoon dynamics and related hydroclimate in a vulnerable region by generating quantitative and well-dated multi-millennial climate records from speleothems. The project will provide scientific training, mentorship and professional development for several undergraduate (including summer research experience) and one graduate (Ph.D.) students, as well as one postdoctoral researcher at three universities including two minority serving institutions. Additionally, the project will support an early career scientist. The results of the project will be part of ongoing and newly developed public outreach activities both in The US and the study region (Laos/Vietnam) involving students and postdocs. The project will also foster international and transdisciplinary collaborations including with local 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.

这个项目的目的是利用一套洞穴洞穴记录来描述过去约45000年来东南亚大陆(MESA)的亚洲夏季和冬季季风环流和当地水文气候，这些洞穴横跨老挝和越南之间的关键地理分水岭，这两个国家具有非常不同的季节性降雨气候。这项工作的主要目标是探讨夏季和冬季亚洲季风变化对不断变化的外部驱动因素的动态响应，例如日照和内部气候变化，这将有助于更好地了解脆弱区域的大尺度水文变化。具体地说，研究人员将利用多种环境示踪剂(碳和氧同位素、镁/钙等痕量元素、放射性碳)开发一套新的过去气候记录，这些记录的年代准确，跨越至少过去约45000年。此外，一个详细的洞穴监测计划将有助于解释从洞穴中获得的数据。研究结果将与过去气候变化的其他区域和全球记录以及最先进的气候模型模拟相结合，以诊断驱动台地地区在亚十年至千年时间尺度上水文气候变化的主要机制。这项研究将针对以下具体目标：(1)确定夏季和秋季/冬季MSEA水文气候对轨道和千年尺度强迫的响应，(2)确定MSEA水文气候对年代际至数十年尺度海面温度变率的响应，以及(3)与其他现有记录相结合，阐明MSEA水文气候的时空模式，结合古气候模式分析，使我们能够研究夏季和秋季/冬季季风变率的动力机制。来自三个研究地点的洞穴氧同位素记录将作为夏季风强度的替代指标，以印度洋上游降雨程度为主，微量元素测量将为每个洞穴地点过去当地水平衡的变化提供强有力的证据，老挝地点记录夏季降雨量，越南地点记录秋季/冬季降雨。潜在的更广泛的影响包括通过从洞穴中生成定量和准确的数千年气候记录，更好地了解脆弱地区的季风动态和相关的水文气候。该项目将为几名本科生(包括暑期研究经验)和一名研究生(博士)提供科学培训、指导和专业发展。一名学生以及三所大学的一名博士后研究员，其中包括两个少数民族服务机构。此外，该项目将支持一名早期职业科学家。该项目的成果将是在美国和研究地区(老挝/越南)正在进行的和新开发的公共宣传活动的一部分，涉及学生和博士后。该项目还将促进国际和跨学科合作，包括与当地社区的合作。该奖项反映了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。