二阶Stokes波作用下多孔弹性海床动力响应解析解

基于二阶Stokes波理论,研究了非线性海洋波作用下多孔弹性海床的动力响应问题。利用Biot固结理论以及Verruijt储存方程,在笛卡尔坐标下建立了海床的控制方程。通过将海洋波函数拓展到复数域,采用严格的数学推导求得了海床动力响应的解析解,并将该解与既有解进行对比验证。最后分析了波浪和海床特征参数对海床有效应力、剪切应力和孔压分布的影响,结果表明波浪和海床的参数对海床动力响应具有显著的影响。其中波浪周期和水深对二阶Stokes波的二阶项有较大影响,渗透系数和剪切模量则分别影响海床动力响应的变化速率和幅值。

Typhoon-Induced Ocean Waves and Stokes Drift:A Case Study of Typhoon Mangkhut(2018)

Ocean waves and Stokes drift are generated by typhoons.This study investigated the characteristics of ocean waves and wave-induced Stokes drift and their effects during Typhoon Mangkhut using European Centre for MediumRange Weather Forecasts(ECMWF)ERA5 datasets and observational data.The results revealed that the typhoon generated intense cyclones and huge typhoon waves with a maximum wind speed of 45 m/s,a minimum pressure of955 h Pa,and a maximum significant wave height of 12 m.The Stokes drift caused by typhoon waves exceeded 0.6m/s,the Stokes depth scale exceeded 18 m,and the maximum Stokes transport reached 6 m^(2)/s.The spatial distribution of 10-m wind speed,typhoon wave height,Stokes drift,Stokes depth,and Stokes transport during the typhoon was highly correlated with the typhoon track.The distribution along the typhoon track showed significant zonal asymmetry,with greater intensity on the right side of the typhoon track than on the left side.These findings provide important insights into the impact of typhoons on ocean waves and Stokes drift,thus improving our understanding of the interactions between typhoons and the ocean environment.This study also investigated the contribution of Stokes transport to the total net transport during typhoons using Ekman-Stokes Numbers as a comparative measure.The results indicated that the ratio of Stokes transport to the total net transport reached up to 50%within the typhoon radius,while it was approximately 30%outside the radius.Strong Stokes transport induced by typhoon waves led to divergence in the transport direction,which resulted in upwelling of the lower ocean as a compensation current.Thus,Stokes transport played a crucial role in the vertical mixing of the ocean during typhoons.The findings suggested that Stokes transport should be paid more attention to,particularly in high latitude ocean regions,where strong winds can amplify its effects.

Effects of layer interactions on instantaneous stability of finite Stokes flows

The stability analysis of a finite Stokes layer is of practical importance in flow control. In the present work, the instantaneous stability of a finite Stokes layer with layer interactions is studied via a linear stability analysis of the frozen phases of the base flow. The oscillations of two plates can have different velocity amplitudes, initial phases, and frequencies. The effects of the Stokes-layer interactions on the stability when two plates oscillate synchronously are analyzed. The growth rates of two most unstable modes when δ < 0.12 are almost equal, and δ = δ*/h*, where δ*and h*are the Stokes-layer thickness and the half height of the channel, respectively. However, their vorticities are different. The vorticity of the most unstable mode is symmetric, while the other is asymmetric. The Stokes-layer interactions have a destabilizing effect on the most unstable mode when δ < 0.68, and have a stabilizing effect when δ > 0.68. However, the interactions always have a stabilizing effect on the other unstable mode. It is explained that one of the two unstable modes has much higher dissipation than the other one when the Stokes-layer interactions are strong. We also find that the stability of the Stokes layer is closely related to the inflectional points of the base-flow velocity profile. The effects of inconsistent velocity-amplitude, initial phase, and frequency of the oscillations on the stability are analyzed. The energy of the most unstable eigenvector is mainly distributed near the plate of higher velocity amplitude or higher oscillation frequency. The effects of the initial phase difference are complicated because the base-flow velocity is extremely sensitive to the initial phase.

全球Stokes漂流的时空分布特征研究

利用海浪模式WWIII(Wave Watch III)2008年的模拟结果对海面Stokes漂流、Stokes输运、Stokes深度以及全球Langmuir数的年平均分布特征和季节平均分布特征分别进行了详细的研究与分析。结果表明,海面Stokes漂流和Stokes输运均呈现高纬度偏大的特征,以南极绕极流海域最为突出。全球大部分海域Stokes漂流影响深度在20 m以内,呈现大洋东部偏大,西部偏小的分布特征。全球大部分海域的混合作用是剪切不稳定性和Langmuir湍效应并存的状态,甚至有些海域是以Langmuir湍效应为主。因此,在进行大尺度的海洋数值模拟时,应该考虑波浪导致的混合效应。

Role of Stokes Drift in Ocean Dynamics Under Typhoon Conditions in the Bohai Sea

The effect of Stokes drift production(SDP),which includes Coriolis-Stokes forcing,Langmuir circulation,and Craik-Lei-bovich vortexes,on the upper ocean during typhoon passage in the Bohai Sea(BS),China,is investigated by using a coupled wave-current model.The role of SDP in turbulent mixing and the further dynamics during the entire typhoon period are comprehensively stud-ied.Experimental results show that SDP greatly increases turbulent mixing at all depths under typhoon conditions by up to seven times that under normal weather conditions.SDP generally strengthens sea surface cooling by more than 0.4℃,with the maximum reduction in sea surface temperature(SST)at the during-typhoon stage exceeding 2℃,which is approximately seven times larger than that under normal weather conditions.The SDP-induced decrease in current speed can exceed 0.2ms^(-1),and the change in current direction is generally opposite the wind direction.These results suggest that Stokes drift depresses the effect of strong winds on currents by intensifying turbulent mixing.Mixed layer depth(MLD)is distinctly increased by O(1)during typhoons due to SDP and can deepen by more than 5m.In addition,the continuous effects of SDP on SST,current,and MLD at the after-typhoon stage indi-cate a hysteretic response between SDP and typhoon actions.

THE GLOBAL EXISTENCE OF STRONG SOLUTIONS TO THERMOMECHANICAL CUCKER-SMALE-STOKES EQUATIONS IN THE WHOLE DOMAIN

We study the global existence and uniqueness of a strong solution to the kinetic thermomechanical Cucker-Smale(for short,TCS) model coupled with Stokes equations in the whole space.The coupled system consists of the kinetic TCS equation for a particle ensemble and the Stokes equations for a fluid via a drag force.In this paper,we present a complete analysis of the existence of global-in-time strong solutions to the coupled model without any smallness restrictions on the initial data.

非定常Stokes方程的混合有限元法的高精度逼近

针对二维非定常Stokes方程,采用Taylor-Hood混合有限元法进行数值模拟。首先,利用虚功原理将方程转化为变分形式;其次,将求解区域均匀划分为有限个三角形单元,在每个逻辑单元建立与等参单元之间的联系,为速度u选取二次元基函数,为压力p选取线性基函数,从而构造空间尺度的有限元空间;然后,构造时间尺度的全离散θ-型隐格式,选取θ=0.5的Crank-Nicolson六点对称有限差分格式;最后,原问题转化为常微分方程求其数值解,并通过数值算例检验该方法的可行性与有效性。理论构造和数值结果均验证,非定常问题在空间层、时间层离散分别使用线性有限元和二次有限元计算均可得到稳定的一致收敛结果,且二次有限元的精度更高、收敛更快。为了更直观生动地展示实验结果,文章最后给出了精确解与有限元解的三维误差图。

基于机器学习的矩形腔内Stokes流场预测

熔体输送过程发生在单螺杆挤出机均化段,涉及压力建立和混合机理。流体流动可简化为矩形腔内高黏度流体上盖拖动的流动问题,因此,速度场的精确求解非常重要。目前,流场求解多采用传统的数值模拟方法和可视化实验测试方法完成,所需的时间成本高。基于涡量-速度方法,通过数值模拟方法获得矩形腔内高黏度牛顿流体流场,抽取局部速度场作为数据集,尝试一种全新的从局部推测全局的流场预测方法。训练集、验证集和测试集的比例为1∶1∶8,使用机器学习方法,基于Tensor Flow建立多输入、多输出的6层人工神经网络模型,对腔体内全局速度场进行拓展预测研究。结果表明,在仅用10%训练数据的情况下,人工神经网络模型也能得到较精准的全局速度场预测结果。对比数值模拟全局数据,水平方向速度及垂直方向速度的MSE、L_(2)相对误差均达到了较小的范围,并且R_(2)均达到了0.99,证实了该方法的可行性与可靠性。所做工作为今后采集局部流场数据开展全局流场预测提供依据,也为采用神经网络模型实现挤出机内全局速度场插值进而开展流体运动数值模拟追踪提供了新思路。

Stokes公式的自由度及其在计算积分中的应用

考察了Stokes公式中蕴含的自由度问题.基于这种自由度,得到了计算第二类曲面积分(或一般的流形上的积分)的分部积分法和更改被积曲面积分法的两个对偶公式.用具体例子说明了这两个公式的应用.

区域大地水准面确定中Stokes核函数的应用

结合DNSC08-GRA模型中的美国近海测高重力数据,分析比较五种Stokes核函数的计算精度。结果表明,在测试区域,改进的核函数较球形Stokes核函数在精度上有了明显的提高(约3.4 cm);而各改进核函数之间差异不明显。利用GPS/水准数据进行检核发现,拟合前后的大地水准面约有1.17 m的系统差,拟合后标准差减小约7 cm。

Meissel-Stokes核函数应用于区域大地水准面分析

为提高区域大地水准面计算精度,基于EGM2008地球重力场位系数模型分析Meissel-Stokes核函数、截断误差系数以及截断误差。选取实验区,采用移去-恢复法评价Meissel-Stokes核函数计算大地水准面的精度。结果表明:Meissel-Stokes核函数及其截断误差系数收敛速度快;截断误差小且稳定。在积分半径不易扩展的情况下,应用Meissel-Stokes核函数计算区域大地水准面,比标准Stokes计算大地水准面精度略高。

深水Stokes漂流公式的一种新形式

本文在未将Stokes波的势函数参数β近似为波面振幅a的前提下使用近似解迭代方法重新推导了Stokes波的水质点的轨迹方程。在具体推导中发现水平位移与垂向位移在作近似解迭代时,收敛于精确解的速度是不相同的,垂向位移在一次迭代后即与精确解非常近似,而对于水平位移必须做二次迭代才能达到较好的精度。由二次迭代的水平位移方程即可获得Stokes漂流公式的一种新形式,该形式表明,在三阶精度下Stokes漂流与所在深度的水质点的振幅A的平方成正比。运用由垂向位移方程解得的振幅与参数β的关系式可证明经典Stokes漂流公式可以看作是新漂流公式在特定坐标系下的特定垂直断面处的结果。

反Stokes荧光制冷实验中的温度测量技术

反Stokes荧光制冷(anti-Stokes fluorescent cooling)是近年来快速发展起来的一种新颖的固体材料激光冷却技术。文中首先简单介绍了反Stokes荧光制冷的基本原理;其次,详细介绍了固体材料激光制冷实验中温度测量的各种新方法、新原理和新结果及其最新进展,最后简单比较了各种温度测量技术的分辨率及其优缺点。

Effect of wave-induced Stokes drift on the dynamics of ocean mixed layer

The wave-forcing 'Coriolis-Stokes forcing' and 'Stokes-vortex force' induced by Stokes drift affect the upper ocean jointly.To study the effect of the wave-induced Stokes drift on the dynamics of the ocean mixed layer,a new three-dimensional(3D) numerical model is derived using the primitive basic equations and Eulerian wave averaging.The Princeton Ocean Model(POM),a 3D primitive equation ocean model is used with the upper wave-averaged basic equations.The global ocean circulation is simulated using the POM model,and the Stokes drift is evaluated based on the wave data generated by WAVEWATCH III.We compared simulations with and without the Stokes drift.The results show that the magnitude of the Stokes drift is comparable with the Eulerian mean current.Including the Stokes drift in the ocean model affects both the Eulerian current and the Lagranian drift and causes the vertical mixing coefficients to increase.

关于定常Stokes绕流的悖论

证明了定常Ｓｔｏｋｅｓ绕流ｖ≡０，即Ｓｔｏｋｅｓ悖论，如果相应的Ｄｉｒｉｃｈｌｅｔ积分有限，或者，当｜ｘ｜→∞时，｜ｖ（ｘ）｜＝Ｏ（ｌｎα｜ｘ｜）（α≥０，ｎ＝２），｜ｖ（ｘ）｜＝Ｏ（｜ｘ｜２－ｎ）（ｎ＞２）．

从Stokes第一问题的精确解谈起

以Stokes第一问题为例,阐述在Nrdvier-Stokes方程精确解的教学过程中,如何引导学生从不同数学方法的角度展开积极思维。研究发现,除了在国内外流体力学教材中普遍使用的量纲分析法,还可以使用分离变量法、拉普拉斯变 换和运算微积法等多种方法求解Stokes第一问题。在此基础上,可不断提出新问题,鼓励学生探索创新,给出了几个例子。

绕带角点障碍物Stokes流动的边界元解法

对以带有角点区域边界为边界的外部无限域上的Stokes方程的Dirichlet问题，在利用单层位势求解时，不仅产生的第一类积分方程的核具有奇异性，而且积分方程的解在角点处也具有r^-1/2的奇异性。为了准确的反映这种奇异性，引入奇异边界单元，即在角点处采用特殊形式的形函数，探讨边界是带有角点区域的边界，求解区域是该边界外的无限区域上的Stokes方程的Dirichlet问题的边界元解法。该问题可以反映流体绕一形状不规则障碍物（含有角点）运动时的流场及压力分布。

VK—Stokes核函数的性能分析

为了获取高精度大地水准面、克服重力数据不能实现全球覆盖所带来的问题，常应用修正Stokes核函数。它能改善标准Stokes核函数特性，使其在较小积分范围内达到较高计算精度。本文基于地球重力场位系数模型EGM2008，分析了修正核函数（VK—Stokes）特性及其远区截断误差。计算分析表明：在近区0．2°积分半径内，VK—Stokes与标准Stokes和WG—Stokes核函数值接近；但随着积分半径增加，VK—Stokes较标准Stokes核函数收敛更快，且其远区截断误差数值也相对较小。由此可见，应用VK—Stokes核函数，既可实现在较小积分范围内提高计算能力，又能抑制其远区截断误差影响。

确定球近似大地水准面的积分Stokes方法

文章介绍了计算求解大地水准面的Stokes公式的一种新方法——积分Stokes方法。给出了积分Stokes函数,通过该函数计算大地水准面时,在计算点处不存在奇异性。作为示例文章采用了连续分布的重力异常函数进行了试算,结果表明,利用该方法计算所得的结果与普通的数值积分方法比较具有较高的精度。

Stokes漂流对全球海表面温度模拟的影响

Stokes漂流对海洋上混合层中的流场和温度场结构具有不可忽视的作用。本文基于WAVEWATCHⅢ海浪模式模拟的海浪要素计算得到Stokes漂流,将其引入SBPOM模式的动量方程中,从体积输运的角度研究Stokes漂流对全球海表面温度的影响。分析发现Stokes漂流与Stokes输运在全球呈现高纬度强于中低纬度的带状分布特征,且这种流动与输运对全球海表面温度具有降温作用,该降温作用的分布与全球Stokes输运强度相对应,高纬降温作用大于中低纬度,特别是南极绕极流海域平均降温明显大于其余海域,最大降温可达1.5℃,且全球月平均降温超过0.1℃。