EAR-PF: Reconstructing late Holocene hydroclimatic variability in western Central America using multi-proxy analyses of lacustrine sediments

EAR-PF：利用湖泊沉积物的多代理分析重建中美洲西部全新世晚期水文气候变化

• 批准号: 2204484
• 负责人: Derek Gibson
• 金额: $ 18万
• 依托单位: Gibson, Derek K
• 依托单位国家: 美国
• 项目类别: Fellowship Award
• 财政年份: 2022
• 资助国家: 美国
• 起止时间: 2022-10-01 至 2024-09-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2204484&HistoricalAwards=false
• 关键词: EAR; PF; Reconstructing; late; Holocene

Dr. Derek Gibson has been awarded an NSF EAR Postdoctoral Fellowship to carry out research and education plans at Missouri University of Science and Technology under the mentorship of Dr. Jonathan Obrist-Farmer. Hydroclimate extremes, particularly droughts, have resulted in an unprecedented increase in climate refugees from Central America over the past decade, creating a humanitarian, economic, and national security crisis. Current climate models predict that Central American precipitation will further decrease by the end of the century. However, the models used to predict such changes rely on records of past climate change and, at present, regional data that reflect how Central American precipitation changed in the past are sparse. This project will use sediment cores collected from Guatemala and southern Mexico to produce evidence of past changes in Central American precipitation that spans the past 2,000 years. In turn, these new records will improve current predictive models of Central American precipitation, which is critical to building a climate-resilient future in Central America and reducing the extent of climate-driven human migration over the upcoming decades. In addition to producing new climate data, K-12 partnerships will extend the impact of this research by educating the next generation of scientists on the mechanisms and impacts of climate change. Educational activities and international collaborations will involve students from elementary to graduate school and provide opportunities for historically underserved students to contribute to solving one of the major climate science questions of the 21st century.Predictable precipitation patterns are critical to the food security and economic stability of Central America. However, inter-model heterogeneity among current climate models, due in part to a paucity of high-resolution and local-scale paleoclimate records that span the late Holocene, make reliable projections of future precipitation difficult. The proposed research will utilize sediment cores from six watersheds located across Guatemala and the Yucatán Peninsula in order to produce multi-proxy reconstructions of local-scale hydroclimatic variability within the context of the synoptic-scale climate changes that occurred during the Medieval Climate Anomaly, Little Ice Age, and Current Warm Period. The proposed field sites are situated such that sediment cores collected from these sites can be used to investigate variability through time in the relative influences of the Inter-tropical Convergence Zone, Caribbean Low-Level Jet, El Niño Southern Oscillation, and topography. Specifically, stratigraphic variability of δ2H in leaf-wax long chain (n-C27, n-C29, n-C31) n-alkanes preserved in the sediment cores will be used as a proxy for regional hydroclimatic variability, while the δ2H of short chain (n-C21, n C23) n-alkanes will be used to reconstruct precipitation/evaporation balance at the local (water column to watershed) scale. These data will be a critical component of predictive models used in the Central American climate resilience and adaptation plans that must be implemented before climate-driven human migration leads to further suffering.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.

德里克吉布森博士已被授予美国国家科学基金会博士后奖学金，在乔纳森奥布里斯特法默博士的指导下，在密苏里州科技大学开展研究和教育计划。极端水文气候，特别是干旱，导致中美洲气候难民在过去十年中空前增加，造成人道主义，经济和国家安全危机。目前的气候模式预测，到世纪末，中美洲的降水量将进一步减少。然而，用于预测这种变化的模型依赖于过去气候变化的记录，目前，反映中美洲降水量过去如何变化的区域数据很少。该项目将使用从危地马拉和墨西哥南部收集的沉积物岩心，以提供过去2,000年中美洲降水变化的证据。反过来，这些新记录将改善目前中美洲降水的预测模型，这对于在中美洲建立一个气候适应性未来和减少未来几十年气候驱动的人类迁移程度至关重要。除了产生新的气候数据外，K-12伙伴关系还将通过教育下一代科学家了解气候变化的机制和影响来扩大这项研究的影响。教育活动和国际合作将涉及从小学到研究生院的学生，并为历史上得不到充分服务的学生提供机会，为解决21世纪世纪的一个重大气候科学问题作出贡献。可预测的降水模式对中美洲的粮食安全和经济稳定至关重要。然而，目前的气候模型之间的模型异质性，部分原因是缺乏高分辨率和当地规模的古气候记录，跨越晚全新世，使可靠的预测未来的降水困难。拟议的研究将利用沉积岩芯从六个流域位于危地马拉和尤卡坦半岛，以产生多代理重建局部尺度水文气候变率的背景下，天气尺度的气候变化，发生在中世纪的气候异常，小冰期，目前温暖期。拟议的实地地点的位置使从这些地点收集的沉积物岩心可用于调查热带辐合带、加勒比低空急流、厄尔尼诺南方涛动和地形的相对影响随时间的变化。具体而言，沉积物岩心中保存的叶蜡长链（n-C27，n-C29，n-C31）正构烷烃中δ 2 H的地层变异性将被用作区域水文气候变异性的代表，而短链（n-C21，n-C23）正构烷烃的δ 2 H将被用于重建局部（水柱到流域）尺度的降水/蒸发平衡。这些数据将成为中美洲气候复原力和适应计划中使用的预测模型的关键组成部分，这些计划必须在气候驱动的人类迁移导致进一步痛苦之前实施。该奖项反映了NSF的法定使命，并被认为值得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来支持。