Collaborative Research: Paleoclimate perspective on the response of Southwest North American rainfall to elevated greenhouse gases

合作研究：北美西南部降雨对温室气体升高的响应的古气候视角

• 批准号: 1903650
• 负责人: Ran Feng
• 金额: $ 14.95万
• 依托单位: University of Connecticut
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2019
• 资助国家: 美国
• 起止时间: 2019-08-15 至 2024-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1903650&HistoricalAwards=false
• 关键词: Collaborative; Research; Paleoclimate; perspective; response

In recent years, severe drought in southwestern North America has prompted intense interest in understanding the future trajectory of hydroclimate in this vulnerable region. Studying past greenhouse climates can help identify the processes that might drive future rainfall changes in the Southwest. One such interval, the mid-Pliocene Warm Period, which occurred 3.3 million years ago and featured CO2 concentrations similar to near-future values, presents an interesting conundrum. Simulations of the Pliocene suggest widespread dry conditions across the Southwest, just as models predict drying across much of the southwest by the end of the 21st century. However, multiple lines of geological evidence suggest wetter conditions in the Pliocene. This research project aims to resolve this apparent paradox using a combination of state-of-the-art, high-resolution climate model simulations and new reconstructions of southwestern rainfall spanning the Pliocene to the present. The reconstructions will provide some of the first constraints on the Pliocene history of regional climate features like the North American Monsoon. These data and model simulations will be used to evaluate sources of bias in model simulations of the Pliocene and to understand how this past interval of climate change may have differed from current warming. The project has direct applications to improving projections of southwestern rainfall in a warming world. The results of the work will be disseminated to the public and stakeholders via museum lectures, and will complement ongoing efforts to develop hands-on research experiences for high school students. Paleoclimatic research can clarify the future behavior of regional climates by studying the past. This project exemplifies this goal by using new data from the mid-Pliocene Warm Period, specifically the mid-Piacenzian, to understand the response of North American Southwest rainfall to elevated greenhouse gases. This project tests the hypothesis that the spatial footprint of summer rainfall was much more extensive in the Pliocene. The research will reconstruct Plio-Pleistocene rainfall seasonality from marine sediment cores along the California margin and Baja California. Measurements of stable isotopes in leaf waxes will explicitly resolve changes in the balance of summer vs. winter rainfall. Complementary measurements of ocean surface temperature from organic proxies like alkenones will provide additional, independent constraints on regional environmental change. The project will also conduct a suite of Earth system model simulations to explore how changes in atmospheric parameterizations and model configuration influence simulated patterns of Pliocene rainfall. Proxy data and model simulations will be interpreted synergistically, with models helping inform proxy interpretations, and proxies helping to assess model skill. The research meets two major goals: first, it provides novel constraints on the Plio-Pleistocene evolution of key regional rainfall regimes like the North American Monsoon (NAM). Second, the project will help clarify the factors that influence model skill at simulating Pliocene hydroclimate, with broad implications for our understanding of the model configurations that most reliably predict regional responses to elevated CO2.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.

近年来，北美西南部的严重干旱引发了人们对了解这一脆弱地区未来水文气候轨迹的浓厚兴趣。研究过去的温室气候可以帮助确定可能驱动西南地区未来降雨变化的过程。其中一个时期是上新世中期暖期，它发生在 330 万年前，二氧化碳浓度与近期值相似，这是一个有趣的难题。对上新世的模拟表明西南部地区普遍存在干旱，正如模型预测到 21 世纪末西南部大部分地区将出现干旱一样。然而，多种地质证据表明上新世的气候条件更为湿润。该研究项目旨在结合最先进的高分辨率气候模型模拟和对上新世至今西南降雨量的新重建来解决这一明显的悖论。这些重建将为上新世区域气候特征（如北美季风）的历史提供一些初步的限制。这些数据和模型模拟将用于评估上新世模型模拟中的偏差来源，并了解过去的气候变化时期与当前的变暖有何不同。该项目可直接应用于改善全球变暖情况下西南降雨量的预测。这项工作的结果将通过博物馆讲座向公众和利益相关者传播，并将补充目前为高中生培养实践研究经验的努力。古气候研究可以通过研究过去来阐明区域气候的未来行为。该项目通过使用上新世中期暖期（特别是皮亚琴兹中期）的新数据来例证这一目标，以了解北美西南部降雨对温室气体升高的反应。该项目测试了这样的假设：上新世夏季降雨的空间足迹要广泛得多。该研究将从加利福尼亚州边缘和下加利福尼亚州的海洋沉积物岩心重建上里奥-更新世降雨季节性。叶蜡中稳定同位素的测量将明确解决夏季与冬季降雨平衡的变化。利用烯酮等有机替代物对海洋表面温度进行补充测量将为区域环境变化提供额外的、独立的约束。该项目还将进行一套地球系统模型模拟，以探索大气参数化和模型配置的变化如何影响上新世降雨的模拟模式。代理数据和模型模拟将被协同解释，模型帮助告知代理解释，代理帮助评估模型技能。该研究实现了两个主要目标：首先，它为北美季风（NAM）等关键区域降雨状况的上里奥-更新世演化提供了新的约束。其次，该项目将有助于阐明影响模拟上新世水文气候的模型技能的因素，对我们理解最可靠地预测区域对二氧化碳升高的反应的模型配置具有广泛的影响。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。

项目成果

Evaluation of Arctic warming in mid-Pliocene climate simulations

• DOI: 10.5194/cp-16-2325-2020
• 发表时间: 2020-11-23
• 期刊: CLIMATE OF THE PAST
• 影响因子: 4.3
• 作者: de Nooijer, Wesley;Zhang, Qiong;Brierley, Chris M.
• 通讯作者: Brierley, Chris M.

Drier tropical and subtropical Southern Hemisphere in the mid-Pliocene Warm Period

• DOI: 10.1038/s41598-020-68884-5
• 发表时间: 2020-08
• 期刊: Scientific Reports
• 影响因子: 4.6
• 作者: G. Pontes;I. Wainer;A. Taschetto;Alexander Sen Gupta;A. Abe‐Ouchi;E. Brady;W. Chan;D. Chandan;C. Contoux;R. Feng;S. Hunter;Yoichi Kame;G. Lohmann;B. Otto‐Bliesner;W. Peltier;C. Stepanek;J. Tindall;N. Tan;Qiong Zhang;Zhongshi Zhang;Zhongshi Zhang;Zhongshi Zhang

Mid-Pliocene mesic subtropical hydroclimate over continents driven by land surface changes

地表变化驱动的上新世中期大陆副热带水文气候

• 发表时间: 2021
• 期刊: EGU General Assembly 2021
• 作者: Ran Feng, Tripti Bhattacharya

The Pliocene Model Intercomparison Project Phase 2: large-scale climate features and climate sensitivity

• DOI: 10.5194/cp-16-2095-2020
• 发表时间: 2020-11-04
• 期刊: CLIMATE OF THE PAST
• 影响因子: 4.3
• 作者: Haywood, Alan M.;Tindall, Julia C.;Lunt, Daniel J.
• 通讯作者: Lunt, Daniel J.

Expansion and Intensification of the North American Monsoon During the Pliocene

• DOI: 10.1029/2022av000757
• 发表时间: 2022-11
• 期刊: AGU Advances
• 影响因子: 8.4
• 作者: Tripti Bhattacharya;R. Feng;J. Tierney;Claire B. Rubbelke;N. Burls;Scott Knapp;M. Fu