Ocean Circulation, Oxygen and Nutrient Cycles During the Last Glacial Period

末次冰河期的海洋环流、氧气和养分循环

• 批准号: 0728315
• 负责人: Andreas Schmittner
• 金额: --
• 依托单位: Oregon State University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2007
• 资助国家: 美国
• 起止时间: 2007-08-01 至 2011-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0728315&HistoricalAwards=false
• 关键词: Ocean; Circulation; Oxygen; Nutrient; Cycles

Ocean Circulation, Oxygen and Nutrient Cycles During the Last Glacial PeriodAndreas Schmittner-BoeschOregon State UniversityAbstractThis proposal seeks to test a primary hypothesis that observed millennial variations of sedimentary nitrogen isotope data from the N. Pacific during the last ice age reflect the collapse of North Atlantic Deep Water formation, which then led to a global decrease in upper-ocean nutrient concentrations and plankton productivity. This ecological shift in-turn led to reduced remineralization of organic matter, shrinkage of the oxygen minimum zones, and a decline in denitrification on a global scale, with a rapid response on the scale of hundreds of years. To address this question the PI's will embed a model of nitrogen isotope cycling in a newly improved coupled atmosphere-ocean model of intermediate complexity that includes biogeochemistry, and is capable of multi-millennial runs. Simulations with this model and comparison with the marine geological record will provide new and important information on mechanisms controlling past changes in ocean circulation, productivity, oxygen and nutrient cycling. Several elements of the model will be improved, including the physical circulation (tropical dynamics), and biogeochemistry (both primary biological components, and interactions with the bottom for benthic denitrification). The model will predict the regional distribution, amplitude, and timing of d15N (and other tracers) change for direct comparison with geologic data. Broader impacts include support for undergraduates and graduates and an early-career scientist who has not been funded previously by NSF. The PI's will develop their Earth system model and distribute it for community use at the end of the project.

最后一次冰期的海洋环流、氧和营养循环俄勒冈州立大学的Andreas Schmittner-Boesch摘要这项提议试图检验一个主要的假设，即从北大西洋的沉积物中观察到的氮同位素数据的千年变化。在最后一个冰河时期，太平洋的海洋生态变化反映了北大西洋深水形成的崩溃，这导致了全球上层海洋营养物质浓度和浮游生物生产力的下降。这种生态转变反过来又导致有机物的矿化度降低，氧气最小区缩小，全球范围内的反硝化作用下降，并在数百年的规模上迅速作出反应。为了解决这个问题，PI将在新改进的中等复杂性的大气-海洋耦合模型中嵌入氮同位素循环模型，该模型包括生物地球化学，并且能够运行多个千年。利用这一模式进行模拟并与海洋地质记录进行比较，将提供关于控制海洋环流、生产力、氧气和营养物循环过去变化的机制的新的重要信息。该模型的若干要素将得到改进，包括物理循环（热带动力学）和海洋地球化学（两个主要生物组成部分，以及与海底的相互作用，以实现海底脱氮）。该模型将预测d15 N（和其他示踪剂）变化的区域分布、幅度和时间，以便与地质数据进行直接比较。更广泛的影响包括对本科生和研究生的支持，以及一位以前没有得到NSF资助的早期职业科学家。PI将开发他们的地球系统模型，并在项目结束时分发给社区使用。