Tropical Atlantic Hydrologic Change during the Paleocene-Eocene Thermal Maximum

古新世-始新世热最大值期间热带大西洋水文变化

• 批准号: 2202983
• 负责人: Donald Penman
• 金额: $ 17.28万
• 依托单位: Utah 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: 2022-09-01 至 2024-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2202983&HistoricalAwards=false
• 关键词: Tropical; Atlantic; Hydrologic; Change; during

Climate models predict how global patterns of evaporation and precipitation (the hydrologic cycle) may behave differently in a warmer world. Predicted changes to the global hydrologic cycle have regional implications for the frequency and severity of drought, fire, extreme weather events, and flooding. This project seeks to use the sedimentary record to study how the hydrologic cycle changed during a past warm interval in Earth’s history. The project targets a well-studied ancient global warming event: the Paleocene-Eocene Thermal Maximum, 56 million years ago. By analyzing the chemistry of microfossils preserved in deep-sea sediments from this time period, the researchers can constrain how the balance of evaporation and precipitation changed in regions thought to be particularly sensitive to hydrologic change. The results will be compared to simulations of climatic warming carried out by the latest generation of global climate models. This data-model comparison will improve predictions for future hydrologic variations under ongoing climate change. This project will also provide training and experience for graduate students, and summer internship programs for undergraduate students from under-served communities.Future changes to global patterns of evaporation and precipitation are one of the most pressing areas of concern highlighted by numerical simulations of anthropogenic climate change. Studying past warm events in Earth’s geological past provides an opportunity to test climate model skill in predicting regional hydrologic change. Specifically, recent climate model simulations of the anomalously warm conditions during the Paleocene-Eocene Thermal Maximum (PETM, ~56 million years ago) suggest that the tropical Atlantic Ocean was particularly susceptible to a pronounced shift towards a more arid (more evaporation, less precipitation) state under warmer conditions. This project will test that model prediction by geochemically constraining regional hydrologic change across the PETM using deep-sea sediment cores from the Tropical Atlantic. Regional hydrologic change across the PETM will be constrained by analyzing oxygen isotopes in surface-dwelling planktonic foraminifera at Ocean Drilling Project Site 1258 (Demerara Rise, Tropical North Atlantic Ocean). Since oxygen isotopes in foraminifera reflect a combination of temperature and seawater composition, the magnesium to calcium ratio (Mg/Ca) of the same foraminifers will also be measured to correct for temperature effects, producing a record of changing oxygen isotopic composition of surface seawater across the PETM. The sense and magnitude of this change will be compared to recent simulations of Eocene warming using NCAR’s isotope-enabled Community Earth System Model (iCESM). The methods developed in the proposed work will also be applied to several other sites with published foraminiferal oxygen isotope and Mg/Ca records, producing a global data-model synthesis for hydrologic change across the PETM. This comparison will either bolster confidence in model predictions for regional hydrologic change under warmer conditions, or else identify areas for improvement. The project will support a PhD student and provide training and experience in analytical geochemistry and climate model interpretation.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.

气候模型预测了全球蒸发和降水模式（水文循环）在变暖的世界中的表现可能会有所不同。对全球水文循环的预测变化对干旱、火灾、极端天气事件和洪水的频率和严重程度具有区域性影响。该项目旨在利用沉积记录来研究在地球历史上过去的温暖期，水文循环是如何变化的。该项目的目标是一个经过充分研究的古代全球变暖事件：5600万年前的古新世-始新世热最大值。通过分析这一时期深海沉积物中保存的微化石的化学成分，研究人员可以限制被认为对水文变化特别敏感的地区的蒸发和降水平衡是如何变化的。这些结果将与最新一代全球气候模式对气候变暖的模拟进行比较。这种数据模型比较将改进对持续气候变化下未来水文变化的预测。该项目还将为研究生提供培训和经验，并为来自服务不足社区的本科生提供暑期实习项目。全球蒸发和降水格局的未来变化是人为气候变化数值模拟所强调的最紧迫的关切领域之一。研究地球地质历史中过去的温暖事件提供了一个机会来测试气候模型在预测区域水文变化方面的技能。具体来说，最近对古新世-始新世热极大期（PETM，约5600万年前）异常温暖条件的气候模型模拟表明，热带大西洋特别容易在更温暖的条件下明显转向更干旱（蒸发更多，降水更少）的状态。该项目将使用来自热带大西洋的深海沉积物岩心，通过地球化学方法限制整个PETM的区域水文变化，来测试该模型的预测。通过分析海洋钻井项目1258站点（热带北大西洋Demerara隆起）表层浮游有孔虫的氧同位素，将限制整个PETM的区域水文变化。由于有孔虫的氧同位素反映了温度和海水成分的组合，因此还将测量同一有孔虫的镁钙比（Mg/Ca），以纠正温度效应，从而产生贯穿始新世（PETM）的表层海水氧同位素组成变化记录。这种变化的意义和幅度将与最近使用NCAR的同位素支持的群落地球系统模型（iCESM）模拟始新世变暖进行比较。在提议的工作中开发的方法也将应用于其他几个有孔虫氧同位素和Mg/Ca记录已发表的地点，从而产生一个全球数据模型，综合整个PETM的水文变化。这种比较要么将增强模型预测在变暖条件下区域水文变化的可信度，要么将确定需要改进的领域。该项目将资助一名博士生，并提供分析地球化学和气候模型解释方面的培训和经验。该奖项反映了美国国家科学基金会的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准进行评估，被认为值得支持。