Internal Tide and Waves on the Oregon Continental Shelf

俄勒冈大陆架的内潮和波浪

• 批准号: 0623132
• 负责人: Murray Levine
• 金额: $ 40.11万
• 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: 2006
• 资助国家: 美国
• 起止时间: 2006-09-15 至 2010-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0623132&HistoricalAwards=false
• 关键词: Internal; Tide; Waves; Oregon; Continental

The goal of this research project is to improve our understanding of the generation, propagation and dissipation of the oceanic internal tide on the continental shelf. The internal tide is an internal wave generated when the stratified ocean is forced over bathymetric relief by the barotropic tide. The internal tide that propagates across the shelf toward the shore can become quite complex and often develops into packets of nonlinear internal waves. The internal tide is a major source of variability on continental shelves around the world and is potentially an important source of energy for generating the turbulence responsible for mixing scalars and momentum. It is important to determine the role the internal tide plays in the energy and momentum budgets to better understand and model coastal ocean circulation. It is also important to know the contribution of the internal tide to processes that lead to cross-shelf transport of mass, which includes nutrients, larvae, and sediment. The specific scientific objectives of this project are to: characterize the amplitude, energy flux, and vertical structure of the internal response near tidal frequencies on the shelf, describe the vertical structure and propagation characteristics of the nonlinear internal tide as it propagates across the shelf, quantify the internal wave background frequency continuum on the shelf, and assess the potential impact of the internal tide on cross-shelf transport of biota and sediment and parameterizations of mixing used in current numerical models of coastal circulation. The approach to accomplish these objectives is to analyze the wealth of observations made off the Oregon coast during three comprehensive experiments in summer 1999, summer 2001 and winter 2003. Previously funded analysis focused on the low-frequency wind-forced circulation. This project focuses on the internal tide and higher frequencies. A two-dimensional primitive equation numerical model of the internal tide will be used as a tool to guide the analysis. The purpose of the model is to help us understand the basic physical balances that are consistent with the observations.Broader Impacts: The internal tide contributes to the dissipation of energy and mixing, however, the tide is typically not explicitly included in circulation models. Research, such as that proposed here, will help determine the potential importance of internal tide, eventually leading to direct inclusion of the tide into models, or modification of the existing parameterization used for mixing. Nonlinear internal wave packets may be important in transporting biota, such as larvae, onshore, and sediment offshore. This study will provide some insight into these processes, including information on their spatial and temporal variability. There is much interest in understanding the impacts of cross-shelf transport on biological processes and the ecology of the Oregon shelf and coast. The data analysis methods and the numerical model developed here will be used directly in the education of graduate students in a class being offered by Levine on the internal tide at Oregon State University during the 2006-07 academic year. This class will be taken by graduate students pursuing PhDs in oceanography. The students will learn about the internal tide by running the model and analyzing observations for themselves.

该研究项目的目标是提高我们对大陆架上海洋内潮的产生、传播和消散的认识。内潮是层化海洋在正压潮作用下被迫越过地形时产生的内波。穿过陆架向海岸传播的内潮可以变得相当复杂，并且经常发展成非线性内波包。内潮是世界各地大陆架变化的主要来源，也是产生湍流的潜在重要能量来源，而湍流是标量和动量混合的原因。确定内潮在能量和动量收支中的作用对于更好地理解和模拟沿海海洋环流是很重要的。了解内潮对导致物质跨大陆架迁移的过程的贡献也很重要，其中包括营养物、幼虫和沉积物。该项目的具体科学目标是：表征陆架上潮汐频率附近的内部响应的振幅、能量通量和垂直结构，描述非线性内潮在其跨越陆架传播时的垂直结构和传播特性，量化陆架上的内波背景频率连续体，并评估内潮对生物群和沉积物跨大陆架迁移的潜在影响以及目前沿海环流数值模型中使用的混合参数化。实现这些目标的方法是分析1999年夏季、2001年夏季和2003年冬季三次综合实验期间在俄勒冈州海岸附近进行的大量观测结果。以前资助的分析集中在低频风强迫环流。该项目的重点是内潮和更高的频率。一个二维原始方程内潮数值模型将被用作指导分析的工具。该模型的目的是帮助我们理解与观测结果一致的基本物理平衡。更广泛的影响：内潮有助于能量的耗散和混合，然而，潮汐通常不明确地包括在环流模型中。研究，如这里提出的，将有助于确定内潮的潜在重要性，最终导致直接纳入模型的潮汐，或修改现有的参数化用于混合。非线性内波包可能是重要的，在运输生物群，如幼虫，岸上，和近海沉积物。这项研究将提供一些深入了解这些进程，包括其空间和时间的变异性的信息。人们对了解跨大陆架迁移对生物过程和俄勒冈州大陆架和海岸生态的影响很感兴趣。数据分析方法和数值模型将直接用于教育的研究生在一类由莱文提供的内潮在俄勒冈州州立大学在2006-07学年。这门课将由攻读海洋学博士学位的研究生选修。学生将通过运行模型和分析自己的观察来了解内部潮汐。