Collaborative Research: Impacts of Ocean physics on the Arabian Sea Oxygen Minimum Zone

合作研究：海洋物理学对阿拉伯海最低氧气区的影响

• 批准号: 0727761
• 负责人: Julian McCreary
• 金额: $ 38.56万
• 依托单位: University of Hawaii
• 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: 2007-10-01 至 2012-09-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0727761&HistoricalAwards=false
• 关键词: Collaborative; Research; Impacts; Ocean; physics

Oxygen minimum zones (OMZs) in the world's oceans typically occur below regions of high productivity where oxygen is utilized in the remineralization of sinking detritus by bacteria. The Arabian Sea OMZ is one of the most intense such zones in the world ocean with near-total depletion of oxygen in the eastern-central Arabian Sea at a depth from 100-1000 m. Remarkably, the zone is shifted well to the east of the most productive regions of which are located in the western basin. In this project, scientists from the University of Hawaii and the University of Maryland will collaborate with international partners from India and Japan in order to understand the processes that determine the strength and location of the Arabian Sea OMZ. Their working hypothesis is that physical, and not biological, processes shift this zone to the eastern basin through eddy processes. A hierarchy of physical models will be utilized for this study, each will be coupled to a biological model (NPZD) with an oxygen package. The research aims to understand basic biophysical processes of the Arabian Sea oxygen minimum zone and the results should be applicable to other such regions in the world's oceans. Because of its intensity, understanding the dynamics of the Arabian Sea OMZ is of global importance. Because of its "reducing conditions," the zone impacts the global nitrogen inventory and hence the degree of nitrogen limitation and carbon export. In addition, through the production of N2O, the zone also influences greenhouse gas accumulation in the atmosphere. Finally, the zone is known to have varied considerably on geological time scales which suggests that it may be affected by modern climate change.The research also contributes to international programs including the development of the CLIVAR/GOOS Indian Ocean observing system and Integrated Marine Biology and Ecosystem Research (IMBER).

世界海洋中的最低含氧区通常出现在高生产力区域之下，在那里，细菌利用氧气使下沉的碎屑生物化。阿拉伯海OMZ是世界海洋中最强烈的此类区域之一，阿拉伯海中东部100-1000米深度的氧气几乎完全耗尽。值得注意的是，这一地带向东部转移得很好，而最多产的地区位于西部盆地。在这个项目中，来自夏威夷大学和马里兰州大学的科学家将与来自印度和日本的国际合作伙伴合作，以了解决定阿拉伯海OMZ强度和位置的过程。他们的工作假设是，物理的，而不是生物的，过程通过涡流过程将这个区域转移到东部盆地。本研究将使用物理模型的层次结构，每个模型将与带有氧气包的生物模型（NPZD）耦合。这项研究的目的是了解阿拉伯海最低含氧区的基本生物物理过程，研究结果应适用于世界各大洋其他此类区域。由于其强度，了解阿拉伯海OMZ的动态具有全球重要性。由于其“还原条件”，该区域影响全球氮库存，从而影响氮限制和碳输出的程度。此外，通过产生N2 O，该区域还影响大气中温室气体的积累。最后，该区域在地质时间尺度上变化很大，这表明它可能受到现代气候变化的影响，该研究还有助于国际计划，包括开发CLIVAR/GOOS印度洋观测系统和综合海洋生物学和生态系统研究（IMBER）。