Field and Laboratory Program to Evaluate Atlantic Intermediate Circulation During the Past 25,000 Years

评估过去 25,000 年大西洋中间环流的现场和实验室计划

• 批准号: 0750880
• 负责人: Delia Oppo
• 金额: $ 59.94万
• 依托单位: Woods Hole Oceanographic Institution
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2008
• 资助国家: 美国
• 起止时间: 2008-09-15 至 2012-02-29
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0750880&HistoricalAwards=false
• 关键词: Field; Laboratory; Program; Evaluate; Atlantic

In this project, the PIs will study how changes in deep ocean circulation influenced the distribution of heat, nutrients, and carbon within the ocean, and their link to earth's climate and levels of CO2 in the atmosphere. The research will test the hypothesis that the northward flow of Antarctic Intermediate Water (AAIW) in the Atlantic Ocean is linked to its role as a supplier of North Atlantic Deep Water (NADW), which derives from sinking of surface waters at high northern latitudes and then flows southward in the Atlantic. The PIs predict that when NADW fills more of the deep Atlantic, AAIW penetrates farther northward to supply NADW. In contrast, during abrupt cold events when the formation of NADW was disrupted, the northward penetration of AAIW would have decreased. To address this hypothesis, the PIs will collect new sediment cores from the western tropical Atlantic (~8 N) using the new RV Knorr long coring system. Stable isotope and Mg/Ca data from fossil foraminifera will be used to generate time series of water mass tracers from depths spanning all subsurface water masses, including AAIW and NADW. Better knowledge of the history of the distribution of these water masses will provide a clearer understanding of how deep ocean circulation changes influence climate and atmospheric CO2. The broader impact of this research includes the participation of four graduate and one undergraduate students on the cruise. One graduate student will use the new material for thesis research while an undergraduate will develop a website focusing on the cruise and its scientific significance. Data obtained from this project will be archived with the NGDC website and will be included in historical reconstructions used to improve simulations of past ocean circulation and to test the suitability of general circulation models to predict future climate change. The sediment will be available to other investigators.

在这个项目中，PI将研究深海环流的变化如何影响海洋中热量，营养物质和碳的分布，以及它们与地球气候和大气中二氧化碳水平的联系。这项研究将检验这样一个假设，即大西洋中南极中层水向北流动与其作为北大西洋深层水供应者的作用有关，后者来自北方高纬度地区表层沃茨的下沉，然后在大西洋中向南流动。PI预测，当NADW填充更多的大西洋深处时，AAIW向更北渗透以供应NADW。 相反，在突然的冷事件期间，NADW的形成被破坏，AAIW向北的渗透会减少。为了解决这一假设，PI将使用新的RV Knorr长芯系统从热带大西洋西部（~8 N）收集新的沉积物芯。 有孔虫化石的稳定同位素和Mg/Ca数据将用于生成涵盖所有地下水团（包括AAIW和NADW）深度的水团示踪剂时间序列。更好地了解这些水团的分布历史将有助于更清楚地了解深海环流变化如何影响气候和大气CO2。 这项研究的更广泛影响包括四名研究生和一名本科生参加了这次巡航。一名研究生将使用新材料进行论文研究，而一名本科生将开发一个专注于巡航及其科学意义的网站。从该项目获得的数据将在NGDC网站存档，并将被纳入历史重建，用于改进对过去海洋环流的模拟，并测试大气环流模型对预测未来气候变化的适用性。 沉积物将提供给其他调查人员。