Collaborative Research: Reconstructing the Meridional SST Gradient and Climate Conditions of the Early Pliocene

合作研究：重建上新世早期经向海温梯度和气候条件

• 批准号: 0901921
• 负责人: Alexey Fedorov
• 金额: $ 20.22万
• 依托单位: Yale University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2009
• 资助国家: 美国
• 起止时间: 2009-08-01 至 2012-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0901921&HistoricalAwards=false
• 关键词: Collaborative; Research; Reconstructing; Meridional; SST

This award is funded under the American Recovery and Reinvestment Act of 2009 (Public Law 111-5).The majority of proxy temperature records indicate that during the early Pliocene, roughly 3 to 5 million years ago, the tropical Pacific was characterized by a permanently warm El Niño-like mean state. Specifically, the sea surface temperature (SST) gradient along the equator was very small or nonexistent. At the same time, the meridional SST gradient from the equator to the subtropics was also reduced, implying that the ocean tropical warm pool extended much farther poleward than at present. Such climate conditions persisted even though external factors that control climate, such as atmospheric CO2 concentrations, were essentially the same as today. The goal of this study is to generate proxy SST data in several critical regions of the Pacific Ocean that would enable us to carefully reconstruct the latitudinal SST distribution in the Pacific and to investigate mechanisms that can explain climate observations in the early Pliocene. In parallel with generating new data, the PIs will reconstruct the thermal structure of the upper ocean and atmospheric circulation using calculations with atmospheric and ocean General Circulation Models (GCMs), and with coupled GCMs. The coupled experiments will use two complimentary approaches, constrained and unconstrained, and investigate the role of ocean vertical mixing in maintaining El Niño-like conditions and an expanded warm pool. The ultimate goal of the project is to create a comprehensive picture of the early Pliocene climate in the tropics and subtropics, identify the factors that will facilitate modeling this state with coupled GCMs, and link the Pliocene climate to contemporary climate change. A post-doctoral researcher and graduate student will be supported with this award.

该奖项是根据2009年美国复苏和再投资法案（公法111-5）资助的。大多数代用温度记录表明，在上新世早期，大约300万至500万年前，热带太平洋的特点是一个永久温暖的厄尔尼诺平均状态。具体而言，沿赤道沿着的海表温度梯度非常小或不存在。与此同时，赤道到副热带的纬向SST梯度也在减小，这意味着海洋热带暖池比现在更远地向极地延伸。尽管控制气候的外部因素，如大气中的二氧化碳浓度，与今天基本相同，但这种气候条件仍然存在。本研究的目标是在太平洋的几个关键区域生成代理SST数据，这将使我们能够仔细重建太平洋的纬度SST分布，并调查可以解释上新世早期气候观测的机制。在生成新数据的同时，PI将利用大气和海洋环流模型以及耦合的大气环流模型的计算，重建上层海洋和大气环流的热结构。耦合实验将使用两种互补的方法，约束和无约束，并调查海洋垂直混合在维持厄尔尼诺样条件和扩大暖池中的作用。该项目的最终目标是创建热带和亚热带上新世早期气候的综合图片，确定有助于用耦合GCM模拟这种状态的因素，并将上新世气候与当代气候变化联系起来。一名博士后研究员和研究生将获得该奖项的支持。