Deep-sea sediment redistribution induced by a meandering Gulf Stream

蜿蜒的墨西哥湾流引起的深海沉积物重新分布

• 批准号: 1949536
• 负责人: Olivier Marchal
• 金额: $ 68.26万
• 依托单位: Woods Hole Oceanographic Institution
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2020
• 资助国家: 美国
• 起止时间: 2020-04-01 至 2023-03-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1949536&HistoricalAwards=false
• 关键词: Deep; sea; sediment; redistribution; induced

The abyssal region of the ocean, below a water depth of about 1000 m, is the largest portion of the world's oceans. The original perception of this region as a quiet, almost stagnant, layer of water has been overthrown by observations made with instruments that can withstand the high pressures and corrosive conditions that prevail in the deep sea. In particular, deep oceanic basins underlying strong and variable surface currents witness episodes of high near-bottom velocities and sediment resuspension, leading to the formation of particle-rich layers near the seafloor that are called benthic nepheloid layers (BNLs). Nepheloid refers. Nepheloid refers to the Greek word for "cloud" and indeed BNLs are visually cloudy when disturbed. Although these episodes, called “benthic storms”, have been discovered about 40 years ago, how they form remains a mystery. In this project, a detailed computer model of ocean circulation and sediment transport will be applied to study the plausibility of two mechanisms responsible for benthic storms in the western North Atlantic. One possible mechanism is that the instability of the Gulf Stream, leading to meanders, rings, and eddies generates the benthic storms. The other possible mechanism is that the passage of atmospheric disturbances, such as tropical storms and hurricanes generates them. Both mechanisms have been postulated to produce a downward transfer of energy throughout the water column and to lead to benthic storms, a process that links the atmosphere, the ocean, and the seafloor sediment. Through detailed model simulations and comparison with observations of the sediment left by benthic storms, the project will advance the understanding of the origin of benthic storms and BNLs. Moreover, because such sediments are used by scientists for studying the paleoclimate of the oceans, the work will provide an assessment of the effect of ocean dynamics on this major geologic archive. The work will also help to evaluate the impact of sediment resuspension on the distribution of particles in the oceans, such as those targeted by the ongoing international oceanographic program GEOTRACES. The project will have a broader impact by involving a Post-Doctoral Investigator (PDI) and two Undergraduate Students (USs). All of the results will be shared with the public by creating a web site and by archiving the computer codes developed for this project at an official NSF-funded software registry. The codes will be produced from an open source platform and will be accompanied by a “how-to” document for broader public accessibility.The project will apply an eddy-resolving model of ocean circulation and sediment transport to explore the effects of Gulf Stream meanders, rings, and eddies, as well as the effects of atmospheric disturbances, on the movement of fine sediments at abyssal depths in the western North Atlantic. The work plan will be in three steps. (1) An existing model of ocean circulation and sediment transport will be configured to represent two different domains in the western North Atlantic. A relatively small domain centered on the Nova Scotia Rise where benthic storms have been particularly well documented will be used to produce local but detailed (submesoscale) simulations of sediment transport. A larger domain will be used to produce less detailed but basin-scale simulations of sediment transport in the intense mesoscale eddy field that characterizes the western North Atlantic. (2) Numerical experiments will be conducted with the model for varying atmospheric conditions and sediment characteristics. (3) Model results will be compared to physical observations collected from hydrographic compilations, field programs, and satellite altimetry, to distributions of particle concentration derived from gravimetric, chemical, and optical measurements, and to time series of current velocity and water turbidity obtained from bottom-tethered instruments. From these comparisons, the project will assess the potential of various dynamical phenomena – deep cyclones, topographic Rossby waves, and internal waves – to redistribute sediments on the seafloor and produce benthic storms.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.

海洋的深海区域，水深约1 000米以下，是世界海洋的最大部分。人们最初认为这一区域是一个平静的、几乎停滞的水层，但用能够承受深海中普遍存在的高压和腐蚀性条件的仪器进行的观测推翻了这一看法。特别是，在强而多变的表层海流之下的深海盆地，会出现近底流速高和沉积物再悬浮的情况，导致在海底附近形成被称为底栖云状层的富含颗粒层。类神经元是指。星云状星云是指希腊语中的“云”，实际上BNL在受到干扰时在视觉上是多云的。虽然这些被称为“海底风暴”的事件在大约40年前就被发现了，但它们是如何形成的仍然是一个谜。在这个项目中，将利用一个详细的海洋环流和沉积物迁移计算机模型，研究造成北大西洋西部海底风暴的两种机制的可解释性。一个可能的机制是墨西哥湾流的不稳定性，导致弯曲，环和漩涡产生底栖风暴。另一种可能的机制是，热带风暴和飓风等大气扰动的通过产生了它们。这两种机制都被假定为在整个水柱中产生向下的能量转移，并导致海底风暴，这一过程将大气、海洋和海底沉积物联系起来。通过详细的模型模拟和与海底风暴留下的沉积物观测结果的比较，该项目将促进对海底风暴和生物核泄漏起源的了解。此外，由于这些沉积物被科学家用于研究海洋的古气候，这项工作将评估海洋动力学对这一主要地质档案的影响。这项工作还将有助于评估沉积物再悬浮对海洋中颗粒分布的影响，例如正在进行的国际海洋学计划GEOTRACES所针对的颗粒。该项目将通过涉及博士后研究员（PDI）和两名本科生（US）产生更广泛的影响。所有的成果都将通过建立一个网站和将为该项目开发的计算机代码存档在国家科学基金会资助的官方软件登记处与公众分享。这些代码将在一个开放源平台上制作，并将附有一份“操作指南”文件，供公众更广泛地查阅，该项目将采用海洋环流和沉积物输运的涡流解析模型，以探讨墨西哥湾流曲流、环和涡流以及大气扰动对北大西洋西部深海深处细沉积物移动的影响。工作计划将分三步进行。(1)现有的海洋环流和沉积物输运模型将被配置为代表北大西洋西部的两个不同领域。一个相对较小的领域集中在新斯科舍省上升，海底风暴已特别好地记录将用于产生当地的，但详细的（亚中尺度）模拟泥沙输运。一个更大的域将被用来产生不太详细，但在强烈的中尺度涡动场的特点，北大西洋西部的沉积物输运流域规模的模拟。(2)将对不同的大气条件和沉积物特性用该模式进行数值试验。(3)模型的结果将进行比较，收集水文汇编，实地计划，卫星测高，重力，化学和光学测量的颗粒浓度分布，并从底部系留仪器获得的流速和水浊度的时间序列的物理观测。通过这些比较，该项目将评估各种动力现象--深海气旋、地形Rossby波和内波--重新分布海底沉积物和产生海底风暴的潜力。该奖项反映了NSF的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准进行评估，被认为值得支持。