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Numerical solutions for the two-dimensional reaction-diffusion equation with nonlocal nonlinearity are obtained. The solutions reveal formation of dissipative structures. Structures arising from initial distributions with one and several centers of localization are considered. Formation of extending circular structures is shown. Peculiarities of formation and interaction of extending circular structures depending on  nonlocal interaction are considered.

For modeling and statistical analysis of data characterized by cyclicity (periodicity) in various areas of science are used circular or wrapped distribution models. The phase distribution function of a harmonic and phase-shift-keying signal in case additive white Gaussian noise is considered. Algorithms for modeling random phases sample of harmonic and modulated signals with specified parameters and correlation function are presented. Expressions for the phase distribution density of the phase-shift-keying signal are given. It is shown that the phase probability density function of the phase-shift-keying signal becomes multimodal. In addition, the probability density function under consideration is a periodic function, which means that the trigonometric Fourier basis can be used to decompose it into a series. In paper for the first time, analytical expressions for the coefficients of the Fourier series when decomposing the density under consideration into a harmonic basis are obtained, and the derivation of the corresponding expressions are presented. Examples of computer modeling and corresponding graphical materials of calculating Fourier coefficients of the phase probability density function for harmonic and phase-shift-keying signals are presented. A formula for the cumulative distribution function and its decomposition into a Fourier series are also obtained. Based on the representation of the phase probability density function in the form of a Fourier series, a comparison is made with other circular distributions often used in practical problems, the Mises distribution and the wrapped normal distribution. The results obtained in this work are of theoretical and practical interest for modeling and statistical analysis of signal phases in various applied problems in area radio engineering, digital communication, radar, etc. In particular, in the problems of estimating the signal-to-noise ratio, the bit error rate, as well as the reliability of demodulator solutions, i. e. soft demodulation of phase-shift-keying signals. Analytical expressions for the Fourier series coefficients can be used to estimate the empirical probability density function.

In this article, a meshfree-spectral method for numerical investigation of dynamics of planar geophysical flows is proposed. We investigate inviscid incompressible fluid flows with the presence of planetary rotation. Mathematically this problem is described by the non-steady system of two partial differential equations in terms of stream and vorticity functions with different boundary conditions (closed flow region and periodic conditions). The proposed method is based on several assumptions. First of all, the vorticity field is given by its values on the set of particles. The function of vorticity distribution is approximated by piecewise cubic polynomials. Coefficients of polynomials are found by least squares method. The stream function is calculated by using the spectral global Bubnov –Galerkin method at each time step.

The dynamics of fluid particles is calculated by pseudo-symplectic Runge –Kutta method. A detailed version of the method for periodic boundary conditions is described in this article for the first time. The adequacy of numerical scheme was examined on test examples. The dynamics of the configuration of four identical circular vortex patches with constant vorticity located at the vertices of a square with a center at the pole is investigated by numerical experiments. The effect of planetary rotation and the radius of patches on the dynamics and formation of vortex structures is studied. It is shown that, depending on the direction of rotation, the Coriolis force can enhance or slow down the processes of interaction and mixing of the distributed vortices. At large radii the vortex structure does not stabilize.