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Effect of electron temperature on formation of travelling waves in plasma: Kinetic and hydrodynamic models 电子温度对等离子体行波形成的影响:动力学和流体动力学模型
IF 0.6 4区 数学 Q4 MATHEMATICS, APPLIED Pub Date : 2023-03-01 DOI: 10.1515/rnam-2023-0006
E. V. Chizhonkov, A. A. Frolov
Abstract The kinetic formulation of the model problem of plasma waves excitation by a powerful short laser pulse is numerically studied for the first time. Kinetic and simplest hydrodynamic plasma models are also compared for the problem under consideration. It is shown that the considered hydrodynamic models do not provide good approximations to the solution to the Vlasov kinetic equation, namely, one leads to discontinuous solutions and the other has a significant qualitative distinction. At a low plasma temperature, the effect of non-isothermicity of the process is small, but it can lead to significant distortions of the solution during further heating. The results obtained here imply that the first two moments of the distribution function are not enough to describe the plasma hydrodynamics; higher-order moments should be used.
摘要首次对强短激光脉冲激发等离子体波模型问题的动力学公式进行了数值研究。对于所考虑的问题,还比较了动力学等离子体模型和最简单的流体动力学等离子体模型。结果表明,所考虑的流体动力学模型不能很好地近似Vlasov动力学方程的解,即一个模型导致不连续解,另一个模型具有显著的定性差异。在较低的等离子体温度下,该过程的非等温性影响很小,但在进一步加热过程中会导致溶液的显著扭曲。所得结果表明,分布函数的前两个矩不足以描述等离子体流体力学;应使用高阶矩。
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引用次数: 0
Dependence of optimal disturbances on periodic solution phases for time-delay systems 时滞系统最优扰动与周期解相的关系
IF 0.6 4区 数学 Q4 MATHEMATICS, APPLIED Pub Date : 2023-03-01 DOI: 10.1515/rnam-2023-0008
M. Y. Khristichenko, Y. Nechepurenko, G. Bocharov
Abstract The paper is focused on the dependence of optimal disturbances of stable periodic solutions of time-delay systems on phases of such solutions. The results of numerical experiments with the well-known model of the dynamics of infection caused by lymphocytic choriomeningitis virus are presented and discussed. A new more efficient method for computing the optimal disturbances of periodic solutions is proposed and used.
研究了时滞系统稳定周期解的最优扰动与周期解相位的关系。本文介绍并讨论了著名的淋巴细胞性脉络丛脑膜炎病毒感染动力学模型的数值实验结果。提出并应用了一种新的更有效的周期解最优扰动计算方法。
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引用次数: 0
Finite difference scheme for a non-linear subdiffusion problem with a fractional derivative along the trajectory of motion 沿运动轨迹具有分数导数的非线性次扩散问题的有限差分格式
IF 0.6 4区 数学 Q4 MATHEMATICS, APPLIED Pub Date : 2023-02-01 DOI: 10.1515/rnam-2023-0003
A. Lapin, V. Shaydurov, R. Yanbarisov
Abstract The article is devoted to the construction and study of a finite-difference scheme for a one-dimensional diffusion–convection equation with a fractional derivative with respect to the characteristic of the convection operator. It develops the previous results of the authors from [5, 6] in the following ways: the differential equation contains a fractional derivative of variable order along the characteristics of the convection operator and a quasi-linear diffusion operator; a new accuracy estimate is proved, which singles out the dependence of the accuracy of mesh scheme on the curvature of the characteristics.
摘要考虑对流算子的特征,构造并研究了一类具有分数阶导数的一维扩散对流方程的有限差分格式。它在以下方面发展了前人[5,6]的结果:微分方程包含一个沿对流算子和拟线性扩散算子特征的变阶分数阶导数;提出了一种新的精度估计方法,该方法排除了网格格式精度对特征曲率的依赖关系。
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引用次数: 1
Mesh-independent multidimensional coupling of surface and subsurface water flow models 地表和地下水流模型的网格无关多维耦合
IF 0.6 4区 数学 Q4 MATHEMATICS, APPLIED Pub Date : 2023-02-01 DOI: 10.1515/rnam-2023-0004
K. Novikov
Abstract We present a new approach for multidimensional surface–subsurface flow coupling. The method does not require mesh-to-canal refinement or alignment and is based on numerical characteristics of the intersection of one-dimensional hydraulic object beds and the surface faces of the 3D tetrahedral mesh. The method is validated using widely recognized tilted v-catchment with subsurface and Borden catchment benchmarks.
摘要我们提出了一种新的多维地表-地下流动耦合方法。该方法不需要网格到运河的细化或对齐,并且基于一维水力物体床和三维四面体网格的表面相交的数值特征。该方法使用公认的倾斜v型集水区和地下和波登集水区基准进行了验证。
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引用次数: 0
The new sea ice thermodynamics code for the INM RAS Earth System model: The design and comparison of one- and zero-dimensional approaches with the observational data INM-RAS地球系统模型的新海冰热力学代码:一维和零维方法的设计和与观测数据的比较
IF 0.6 4区 数学 Q4 MATHEMATICS, APPLIED Pub Date : 2023-02-01 DOI: 10.1515/rnam-2023-0005
Sergey S. Petrov, Vladimir K. Zyuzin, N. Iakovlev
Abstract This work is devoted to the comparison of one- (1-D) and zero-dimensional (0-D) models of sea ice thermodynamics. 1-D thermodynamics solvers imply the solution of the diffusion equation with penetrating radiation in the moving domain (moving boundary problem), while 0-D implementations neglect the heat capacity of ice and penetrating radiation, that leads to a linear temperature profile by the construction. So far, some climate models use 0-D implementation of thermodynamics in a block of sea ice, while other models use 1-D implementation with a small number of nodes. In this work we present our fully implicit 0-D and 1-D version of snow–ice thermodynamics, which relieves the model of Courant-type time step constraints. Implicitness is achieved by the relaxation method for nonlinear heat capacity and thermal conductivity coefficients with simultaneous search for the temperature that satisfies the boundary conditions. We introduce the experiment with analytical forcing to compare evolution of temperature profiles. This model experiment shows that 0-D model underestimates ice thickness and overestimates the amplitude of temperature profile variation compared to 1-D solution. Despite the large differences in thickness and internal temperatures, the surface temperatures are very close. The models were also validated on the data of the SHEBA field experiment. According to comparison with observation data, the 0-D model predicts ice thickness and spatiotemporal temperature distribution much worse compared to 1-D model, but the amplitude of error in surface temperature is slightly greater for 0-D code. It can be concluded that 0-D model of sea ice thermodynamics is a good tool for predicting surface temperature, but it gives a large error in thickness and temperature distribution.
本文研究了海冰热力学的一维(1维)和零维(0维)模型的比较。一维热力学解算意味着在运动域(运动边界问题)中具有穿透辐射的扩散方程的解,而0-D实现忽略了冰和穿透辐射的热容,从而导致线性温度分布的构造。到目前为止,一些气候模型在一块海冰中使用0-D实现热力学,而其他模型使用少量节点的1-D实现。在这项工作中,我们提出了完全隐式的0-D和1-D版本的冰雪热力学,这减轻了courant型时间步长约束的模型。通过松弛法求解非线性热容系数和导热系数,同时寻找满足边界条件的温度,实现了隐式求解。我们介绍了用解析强迫的实验来比较温度分布的演变。模型实验表明,与一维模型相比,0-D模型低估了冰厚,高估了温度剖面变化幅度。尽管厚度和内部温度差异很大,但表面温度非常接近。并在SHEBA田间试验数据上对模型进行了验证。与实测数据比较,0-D模式对冰厚和时空温度分布的预测较1-D模式差很多,但0-D模式对地表温度的误差幅度略大。结果表明,0-D海冰热力学模型是预测海面温度的良好工具,但在厚度和温度分布上存在较大误差。
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引用次数: 0
Stochastic simulation of a signal on a photodetector matrix of a laser navigation system 激光导航系统光电探测器矩阵上信号的随机模拟
IF 0.6 4区 数学 Q4 MATHEMATICS, APPLIED Pub Date : 2023-02-01 DOI: 10.1515/rnam-2023-0002
E. Kablukova, V. Oshlakov, S. Prigarin
Abstract Algorithms for stochastic simulation of the signal arriving at the photodetector matrix of the aircraft navigation system are constructed. During the operation of the aircraft landing navigation system, the laser beam of the navigation system coincides in its direction with the glide path determining safe landing. Two photodetector units placed on board of the aircraft determine the glide path position in the coordinate system of the aircraft, which allows one to adjust the position of the touch point on the runway in poor visibility conditions. In this case, the estimation of the power and angular distributions of radiation recorded by the receiver of the navigation system is a relevant problem. In addition, it is interesting to study the effect of scattering of various multiplicities on the recorded signal. The algorithms developed here are based on direct statistical modelling (estimation over collisions) and local estimates of the Monte Carlo method. The calculations show that the proposed methods allow us to evaluate the efficiency of the laser navigation system in various conditions.
摘要构造了飞机导航系统中到达光电探测器矩阵信号的随机仿真算法。在飞机着陆导航系统运行过程中,导航系统的激光束方向与决定飞机安全着陆的滑翔路径重合。放置在飞机上的两个光电探测器单元确定飞机在坐标系统中的滑行路径位置,这允许人们在能见度低的情况下调整跑道上触点的位置。在这种情况下,导航系统接收机记录的辐射的功率和角分布的估计是一个相关的问题。此外,还研究了不同倍数的散射对记录信号的影响。这里开发的算法是基于直接统计建模(碰撞估计)和蒙特卡罗方法的局部估计。计算结果表明,所提出的方法可以评估激光导航系统在各种条件下的效率。
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引用次数: 0
Sensitivity of functionals of the solution to a variational data assimilation problem with heat flux reconstruction for the sea thermodynamics model 海洋热力学模型热通量重建变分数据同化问题解的泛函敏感性
IF 0.6 4区 数学 Q4 MATHEMATICS, APPLIED Pub Date : 2022-12-01 DOI: 10.1515/rnam-2022-0030
V. Shutyaev, E. Parmuzin
Abstract The problem of variational observation data assimilation is considered for the mathematical thermodynamics model developed at the Marchuk Institute of Numerical Mathematics of RAS with the aim to reconstruct the sea surface heat flux. The sensitivity of functionals of solutions to observation data is studied for the considered variational assimilation problem and the results of numerical experiments for the Black Sea dynamics problem are presented.
摘要针对英国科学院Marchuk数值数学研究所建立的海洋表面热通量重建数学热力学模型,考虑了变分观测资料同化问题。本文研究了变分同化问题解的泛函对观测数据的敏感性,并给出了黑海动力学问题的数值实验结果。
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引用次数: 1
Estimation of the average particle flux in a stochastically homogeneous medium by Monte Carlo method 用蒙特卡罗方法估计随机均匀介质中平均粒子通量
IF 0.6 4区 数学 Q4 MATHEMATICS, APPLIED Pub Date : 2022-12-01 DOI: 10.1515/rnam-2022-0029
G. Lotova, G. A. Mikhailov
Abstract The paper is focused on the study of the superexponential growth of the average number of particles in a stochastically homogeneous propagating medium. A mosaic Voronoi field (‘mosaic’) is considered as a random density model. The notion of ‘effective’ correlation radius is introduced to compare the results with previously obtained estimates of superexponential parameters for a spherically symmetric layered mosaic. It is shown that transition from the layered random density model to a chaotic one preserving the correlation scale and one-dimensional distribution weakens the ‘superexponential’ property of the particle flux.
摘要本文主要研究在随机均匀传播介质中粒子平均数的超指数增长。马赛克Voronoi场(“马赛克”)被认为是一个随机密度模型。引入“有效”相关半径的概念,将结果与先前获得的球对称层状镶嵌的超指数参数估计值进行比较。结果表明,从分层随机密度模型到保持相关尺度和一维分布的混沌模型的转变削弱了粒子通量的“超指数”特性。
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引用次数: 0
Stochastic perturbation of tendencies and parameters of parameterizations in the global ensemble prediction system based on the SL-AV model 基于SL-AV模型的全球系综预测系统中趋势和参数化参数的随机扰动
IF 0.6 4区 数学 Q4 MATHEMATICS, APPLIED Pub Date : 2022-12-01 DOI: 10.1515/rnam-2022-0027
K. Alipova, G. Goyman, M. Tolstykh, V. G. Mizyak, V. Rogutov
Abstract Algorithms for stochastic perturbation of parameters and tendencies of physical parameterizations for subgrid-scale processes are implemented into the ensemble prediction system. This system is based on the global semi-Lagrangian atmospheric model SL-AV with the resolution of 0.9 × 0.72 degrees in longitude and latitude, respectively, 96 vertical levels, and our implementation of the Local Ensemble Tranform Kalman Filter (LETKF). The use of stochastically perturbed parameterizations allows to generate ensembles with a significantly larger spread compared to one obtained with the method of static parameter perturbation. An improvement in the probabilistic estimates of the ensemble forecast for different seasons is shown.
在集成预测系统中实现了子网格尺度过程的参数随机扰动和物理参数化趋势的抽象算法。该系统基于经度和纬度分别为0.9×0.72度、96个垂直水平的全球半拉格朗日大气模型SL-AV,以及我们实现的局部集合变换卡尔曼滤波器(LETKF)。与用静态参数扰动方法获得的系综相比,随机扰动参数化的使用允许生成具有显著更大扩展的系综。显示了对不同季节的集合预测的概率估计的改进。
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引用次数: 0
INM-IM: INM RAS Earth ionosphere F region dynamical model INM- im: INM RAS地球电离层F区动力学模型
IF 0.6 4区 数学 Q4 MATHEMATICS, APPLIED Pub Date : 2022-12-01 DOI: 10.1515/rnam-2022-0028
D. Kulyamin, P. A. Ostanin, V. Dymnikov
Abstract A new INM RAS global dynamical model of Earth’s ionosphere F region (100–500 km), which takes into account plasma-chemical processes, ambipolar diffusion, and advective ion transport due to electromagnetic drifts and neutral wind is presented. The model includes parameterizations of polar electric fields induced by magnetospheric convection and simplified equatorial drifts considerations. The focus of the paper is directed on the description of specific methods developed and utilized in the ionospheric model. Key processes responsible for the formation of global ionospheric features are outlined and their representation in the model is evaluated. The main global ionospheric characteristic features, such as seasonal and diurnal cycles, the equatorial ionization anomaly (EIA), polar ionization caps and the main trough have been adequately reproduced based on this model.
摘要提出了一个考虑等离子体化学过程、双极扩散以及电磁漂移和中性风引起的平流离子输运的地球电离层F区(100-500 km)全球动力学模型。该模型包括磁层对流引起的极电场的参数化和简化的赤道漂移考虑。本文的重点是描述电离层模型中开发和使用的具体方法。概述了全球电离层特征形成的关键过程,并对其在模型中的表示进行了评估。该模型充分再现了全球电离层的主要特征,如季节周期和日周期、赤道电离异常(EIA)、极地电离帽和主槽。
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引用次数: 1
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Russian Journal of Numerical Analysis and Mathematical Modelling
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