Collaborative Research: Understanding Tidal Resonances in the Present-Day and Ice-Age Oceans
合作研究:了解当今和冰河时代海洋的潮汐共振
基本信息
- 批准号:0623611
- 负责人:
- 金额:--
- 依托单位:
- 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:2006-10-01 至 2010-09-30
- 项目状态:已结题
- 来源:
- 关键词:
项目摘要
The suggestion that dissipation of tidal energy contributes significantly to mixing of the abyssal oceans, has renewed interest in tides, and their influence on the large scale ocean circulation. The postulated connection between tides, mixing, and the meridional overturning circulation raises interesting questions regarding the role of tides in the past. Two recent studies have demonstrated that the North Atlantic tides of the most recent ice age were substantially larger than they are today. Ice-age tides differ from those of today because tides are resonant phenomena, and are therefore likely to be quite sensitive to changes in sea level and associated changes in basin geometry. The principal objective of this proposal is to address the question of how the astronomical tidal forcing, sea level and basin geometry, and dissipation conspire to produce the observed tidal response. Motivated by recent advances in forward tide modeling, the proposed research seeks to understand tides of both the present-day and of the ice-ages. There are 3 principal elements to the proposed research: (1) Computation of the normal modes of Laplace's tidal equations for the global ocean at a resolution of 1 degree, (2) Simulations with a global forward model of tides to investigate the oceanic response to different forcing frequencies, basin geometries, and sea-levels; and (3) Interpretation of the forward model results in terms of damped-driven oscillator theory, using, as inputs, the eigenfrequencies and associated spatial patterns determined from the normal mode calculation. An improved understanding of tides and how they respond to sea-level change would be an important step toward being able to address a range of issues related to the impact of tides on the large scale circulation. The work will contribute to our understanding of the relative importance of the spatial structure of the forcing, the forcing frequency, and the dissipation, in setting the amplitude of tides in the present day and in the ice ages. The research has broad impact because tides and tidal dissipation affect oceanic circulation (via tidal mixing), sea ice, floating ice shelves, and continental ice sheets. The work has implications for paleoclimate, because of the effects of tidal mixing on oceanic circulation, and also because ice-age tides were very large in the Labrador Sea, site of the Heinrich event iceberg discharges (tides have been proposed as a factor in the iceberg discharges). Finally, this research will provide a framework for predicting the tides of a future with potentially much higher sea levels, with application for coastal cities. The PIs play an active role in teaching, mentoring, and outreach, and this project will provide continued support for those activities, including support for an undergraduate student who will work on this project under the PIs' direction. Results and numerical code will be made freely available to the research community.
潮汐能的耗散对深海混合有重大影响,这一观点重新引起了人们对潮汐及其对大规模海洋环流影响的兴趣。 潮汐、混合和经向翻转环流之间的假设联系提出了有关潮汐在过去的作用的有趣问题。 最近的两项研究表明,最近一个冰河时代的北大西洋潮汐比现在大得多。 冰河时代的潮汐与今天的潮汐不同,因为潮汐是共振现象,因此可能对海平面的变化和盆地几何形状的相关变化非常敏感。 该提案的主要目标是解决天文潮汐强迫、海平面和盆地几何形状以及耗散如何共同产生观测到的潮汐响应的问题。 受正潮模拟最新进展的推动,拟议的研究旨在了解当今和冰河时代的潮汐。 拟议研究有 3 个主要内容:(1) 计算分辨率为 1 度的全球海洋拉普拉斯潮汐方程的正态模态,(2) 使用全球正演潮汐模型进行模拟,以研究海洋对不同的强迫频率、盆地几何形状和海平面; (3) 使用由简正模计算确定的特征频率和相关空间模式作为输入,根据阻尼驱动振荡器理论解释正演模型结果。 更好地了解潮汐及其对海平面变化的反应将是解决与潮汐对大规模环流影响相关的一系列问题的重要一步。这项工作将有助于我们理解强迫的空间结构、强迫频率和耗散在确定当今和冰河时期潮汐幅度方面的相对重要性。这项研究具有广泛的影响,因为潮汐和潮汐消散会影响海洋环流(通过潮汐混合)、海冰、漂浮冰架和大陆冰盖。这项工作对古气候具有重要意义,因为潮汐混合对海洋环流的影响,也因为拉布拉多海(海因里希事件冰山排放的地点)冰河时代的潮汐非常大(潮汐被认为是影响古气候的一个因素)冰山排放)。 最后,这项研究将为预测未来海平面可能更高的潮汐提供一个框架,并应用于沿海城市。 PI 在教学、指导和推广方面发挥着积极作用,该项目将为这些活动提供持续的支持,包括为将在 PI 的指导下从事该项目的本科生提供支持。结果和数字代码将免费提供给研究界。
项目成果
期刊论文数量(0)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
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Samar Khatiwala其他文献
Recent and future trends in atmospheric radiocarbon
大气放射性碳的近期和未来趋势
- DOI:
- 发表时间:
2022 - 期刊:
- 影响因子:0
- 作者:
Heather Graven;Ryo Fujita;Ralph Keeling;Samar Khatiwala;Joeri Rogelj;Xiaomei Xu - 通讯作者:
Xiaomei Xu
Samar Khatiwala的其他文献
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{{ truncateString('Samar Khatiwala', 18)}}的其他基金
NSFGEO-NERC: Understanding the Drivers of Inert Gas Saturation to Better Constrain Ice Core-Derived Records of Past Mean Ocean Temperature
NSFGEO-NERC:了解惰性气体饱和的驱动因素,以更好地限制冰芯记录的过去平均海洋温度
- 批准号:
NE/W007258/1 - 财政年份:2021
- 资助金额:
-- - 项目类别:
Research Grant
NSFGEO-NERC: Quantifying the Modern and Glacial Ocean's Carbon Cycle Including Isotopes
NSFGEO-NERC:量化现代和冰川海洋的碳循环(包括同位素)
- 批准号:
NE/T009357/1 - 财政年份:2019
- 资助金额:
-- - 项目类别:
Research Grant
Collaborative Research: Fast Spin Up of Ocean General Circulation Models Using Newton-Krylov Methods
合作研究:使用牛顿-克雷洛夫方法快速旋转海洋环流模型
- 批准号:
0824635 - 财政年份:2008
- 资助金额:
-- - 项目类别:
Standard Grant
Accelerated Dynamical Spin Up of Ocean General Circulation Models
海洋环流模型的加速动态旋转
- 批准号:
0449703 - 财政年份:2004
- 资助金额:
-- - 项目类别:
Standard Grant
Collaborative Research:Interaction of eddies with mixed layers
合作研究:涡流与混合层的相互作用
- 批准号:
0336808 - 财政年份:2003
- 资助金额:
-- - 项目类别:
Continuing Grant
Sensitivity of Persistence Characteristics of Atmospheric Weather Regimes
大气天气状况持续特征的敏感性
- 批准号:
0233853 - 财政年份:2003
- 资助金额:
-- - 项目类别:
Standard Grant
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