INFORMATION AND COMPUTER TECHNOLOGIES
Journal Title: Вестник КРАУНЦ. Физико-математические науки - Year 2018, Vol 2, Issue
Abstract
The paper proposes a numerical method for solving the problem, based on the use of the method of lines to reduce the problem to a system of ordinary differential equations with unknown parameters. Next, we use a special representation of the solution of the obtained boundary value problem for a linear system of differential equations with nonlocal conditions, by means of which the problem of parametric identification reduces to solving auxiliary boundary value problems and a system of algebraic equations. It is important to note that, unlike optimization approaches, The construction of any iterative procedures or minimizing sequences is used.
Authors and Affiliations
Vagif Abdullayev
ABOUT POSSIBLE SELF-CONSISTENT MECHANISM OF FORMATION AND DISINTEGRATION OF A RING CURRENT EARTH
The paper presents one of the possible mechanisms of formation and decay of the ring current.
TECHNOLOGY OF RADIATION MONITORING: TRACERS-INDICATORS OF DANGEROUS NATURAL AND TECHNOGENIC PHENOMENA
The analysis of results of experimental investigation concerning the influence of natural and technogenic events on radioactive gas and aerosols dynamics as well as structure and dynamics of different types of ionizing r...
FEATURES OF WALKS IN CHAINS RELATED SEISMIC EVENTS
Consider a statistical model of the seismic process in the subduction zone of the KurilKamchatka island arc according to the catalog of seismic moment tensor [1] over the period 1976–2005, using spatial, temporal and ene...
ON THE UNIQUNESS OF THE SOLUTION TO THE BOUNDARY VALUE PROBLEM FOR A MIXED DEGENERATE HYPERBOLIC EQUATION
In this paper the uniquness of the boundary value problem solution for the mixed elliptichyperbolic equation of the second order.
SHOCK WAVE IN IONOSPHERE DURING EARTHQUAKE
Fundamentally new model of the shock wave (SW) generation in atmosphere and ionosphere during earthquake is proposed. The model proceeds from the idea of cooperative shock water crystallization in a cloud