Stratified Fluids and Completely Integrable PDEs
Stratified Fluids and Completely Integrable PDEs
批准号:
2006212
负责人:
Yilun Wu
金额:
$16.4万
依托单位国家:
美国
项目类别:
Continuing Grant
财政年份:
2020
资助国家:
美国
项目状态:
已结题
起止时间:
2020-08-01 至 2024-07-31
中文摘要
在研究海洋中的水波和空气中的大气波时,通常使用渐近模型来代替一般的流体力学方程。这些模型通过抑制流体运动的不重要细节,提供了对基础动力学的有效描述。这是通过对波幅、波长和流体深度施加一定的定标制度来实现的。这个项目涉及对理解两层流体问题的一些主要渐近模型的长时间行为的关键方法的发展。这种情况出现在由不同盐度的水分层的内部海洋波中,这对包括厄尔尼诺效应在内的中期气候模型以及长期气候预测都很重要。水下内波也会与表面波相互作用,产生类似无赖波的现象,可能会损坏或摧毁远洋船只或固定结构。为了对基本方程进行数学研究,在20世纪80年代提出了特殊的求解方法。这些方法试图将原始方程中复杂的非线性动力学转化为可预测的线性动力学。然而,对这些方法的可行性缺乏严格的数学分析。通过开展研究和教育活动的结合,PI将为这些方法发展数学理论,并与合作学科建立联系,同时吸引潜在的学生进入相关领域。在本项目中,PI将发展Benjamin-Ono(BO)方程和中长波(ILW)方程的完全可积性理论。它们都是两层流体问题的一维渐近模型。BO和ILW是具有哈密顿结构的重要的非线性色散方程。此外,提出了直接散射变换(DST)的形式作用角微分同胚,将相空间上的动力学映射到无限维环面上的角平移。如果DST可以逆(IST),人们将有一个强有力的方法来研究这些方程的长期渐近性。然而,目前还没有针对BO的大数据IST理论,甚至没有针对ILW的小数据DST理论。与许多其他完全可积方程的IST理论一样,BO和ILW的IST理论可以表示为Riemann-Hilbert(RH)问题。然而,BO和ILW的RH问题涉及某些非局部跳跃条件。缺乏对非局部RH问题的理论研究,阻碍了BO和ILW的求解。对于BO,PI将使用新发现的散射函数之间的关系来将RH问题归结为求零指数的Fredholm型算子。然后,PI将尝试使用新的恒等式来表明该Fredholm运算符具有平凡的核。对于ILW,PI将DST问题转化为卷积型算子的逆算子,并证明了卷积核上的某些一致估计。PI将通过正则化和在特定加权空间中的求解来构建ILW的IST理论。该奖项反映了NSF的法定使命,并通过使用基金会的智力优势和更广泛的影响审查标准进行评估,被认为值得支持。
英文摘要
In the study of water waves in the ocean and atmospheric waves in the air, it is customary to use asymptotic models to replace general equations of fluid mechanics. These models provide efficient descriptions of the underlying dynamics by suppressing unimportant details of the fluid motion. This is achieved by imposing certain scaling regimes of the wave amplitudes, wavelengths, and fluid depths. This project is concerned with the development of methods critical in the understanding of long-time behavior of some major asymptotic models of the two-layer fluid problem. Such scenarios arise in internal ocean waves layered by water of different salinity, such as are important for medium-term climate modeling including the El Nino effect, as well as long-term climate prediction. Sub-surface internal waves can also interact with surface waves and produce phenomena like rogue waves that can damage or destroy ocean vessels or fixed structures. To study the underlying equations mathematically, special solution methods were proposed in the 1980s. These methods attempt to transform the complicated nonlinear dynamics in the original equations into well predictable linear dynamics. However, rigorous mathematical analysis of the feasibility of these methods is missing. By carrying out a combination of research and educational activities, the PI will develop the mathematical theory for these methods, and make connections to partner disciplines, while attracting prospective students into the related fields. In the current project, the PI will develop complete integrability theories for the Benjamin-Ono (BO) equation and the intermediate long wave (ILW) equation. They are both 1D asymptotic models for the two-layer fluid problem. BO and ILW are important nonlinear dispersive equations with Hamiltonian structures. Furthermore, formal action-angle diffeomorphisms known as the direct scattering transforms (DST) were conjectured to map the dynamics on phase space to angular translations on infinite dimensional tori. If the DST can be inverted (IST), one will have a powerful method to study long-time asymptotics of these equations. However, currently there is no large data IST theory for BO, nor is there even a small data DST theory for ILW. Like those for many other completely integrable equations, the IST theories for BO and ILW can be formulated as Riemann-Hilbert (RH) problems. Nevertheless, the RH problems for BO and ILW involve certain nonlocal jump conditions. Lack of theory for nonlocal RH problems hinders the solution of BO and ILW. For BO, the PI will use a newly discovered relation between the scattering functions to reduce the RH problem to inverting a Fredholm operator of zero index. The PI will then attempt to use a new identity to show that this Fredholm operator has trivial kernel. For ILW, the PI will recast the DST problem as inverting a convolution type operator and prove certain uniform estimates on the convolution kernel. The PI will construct the IST theory for ILW by regularization and solution in certain weighted spaces.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.
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会议论文
Gravitational Effects on Rotating Stars and Deep Water Waves
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批准号:1841750
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项目类别:Continuing Grant
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资助金额:$10.22万
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财政年份:2018
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负责人:Yilun Wu
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依托单位:
Gravitational Effects on Rotating Stars and Deep Water Waves
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批准号:1714343
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项目类别:Continuing Grant
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资助金额:$13.65万
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财政年份:2017
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负责人:Yilun Wu
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依托单位:
海外基金