Abstract—An effective absorbing boundary condition (ABC) based on the second-order approximations of Engquist and Majda’s wave equations is presented for terminating three-dimen-sional finite-difference time-domain (FDTD) models employing the E-J collocated magnetized cold plasma algorithm. Numerical tests demonstrate that this ABC can effectively terminate magnetized plasma models involving arbitrary and spatially varying directions of the background magnetic field, a capability that is not provided by the recently developed KPML or NIMPML for magnetized cold plasma. This new capability will permit implementation of the Engquist and Majda-based ABC of this letter into localized and particularly global FDTD models of the Earth–ionosphere sy...
Abstract—A stochastic finite-difference time-domain (S-FDTD) algorithm is presented for electromagne...
The Finite-Difference Time-Domain (FDTD) method in cylindrical coordinates is used to describe elect...
Global magnetohydrodynamic (MHD) simulations of the Earth's magnetosphere must be coupled with a dy...
pre-printAn effective absorbing boundary condition (ABC) based on the second-order approximations of...
For almost two decades, the finite-difference time-domain (FDTD) method has been applied towards mod...
Abstract—A new three-dimensional finite-difference time-do-main (FDTD) numerical model is proposed h...
pre-printA new three-dimensional finite-difference time-domain (FDTD) numerical model is proposed he...
Abstract—Modeling electromagnetic wave propagation in the upper atmosphere is important for space we...
In this thesis, I use H-J collocated finite-difference time-domain (FDTD) method and E-J collocated ...
The magnetised plasma of near-Earth space (magnetosphere) supports two ultra-low frequency (ULF ;1-1...
Abstract ─ Finite-Difference Time-Domain (FDTD) modeling of electromagnetic wave propagation in the ...
pre-printComputational investigations of electromagnetic wave propagation in the upper atmosphere ar...
The Finite-Difference Time-Domain (FDTD) method in cylindrical coordinates is used to describe elect...
Abstract Advances in computing technologies in recent decades have provided a means of generating an...
dissertationThe primary objective of this dissertation is to investigate the behavior of ground-leve...
Abstract—A stochastic finite-difference time-domain (S-FDTD) algorithm is presented for electromagne...
The Finite-Difference Time-Domain (FDTD) method in cylindrical coordinates is used to describe elect...
Global magnetohydrodynamic (MHD) simulations of the Earth's magnetosphere must be coupled with a dy...
pre-printAn effective absorbing boundary condition (ABC) based on the second-order approximations of...
For almost two decades, the finite-difference time-domain (FDTD) method has been applied towards mod...
Abstract—A new three-dimensional finite-difference time-do-main (FDTD) numerical model is proposed h...
pre-printA new three-dimensional finite-difference time-domain (FDTD) numerical model is proposed he...
Abstract—Modeling electromagnetic wave propagation in the upper atmosphere is important for space we...
In this thesis, I use H-J collocated finite-difference time-domain (FDTD) method and E-J collocated ...
The magnetised plasma of near-Earth space (magnetosphere) supports two ultra-low frequency (ULF ;1-1...
Abstract ─ Finite-Difference Time-Domain (FDTD) modeling of electromagnetic wave propagation in the ...
pre-printComputational investigations of electromagnetic wave propagation in the upper atmosphere ar...
The Finite-Difference Time-Domain (FDTD) method in cylindrical coordinates is used to describe elect...
Abstract Advances in computing technologies in recent decades have provided a means of generating an...
dissertationThe primary objective of this dissertation is to investigate the behavior of ground-leve...
Abstract—A stochastic finite-difference time-domain (S-FDTD) algorithm is presented for electromagne...
The Finite-Difference Time-Domain (FDTD) method in cylindrical coordinates is used to describe elect...
Global magnetohydrodynamic (MHD) simulations of the Earth's magnetosphere must be coupled with a dy...