F. R. Foust
Stanford University
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Featured researches published by F. R. Foust.
Journal of Geophysical Research | 2010
D. I. Golden; M. Spasojevic; F. R. Foust; N. G. Lehtinen; Nigel P. Meredith; U. S. Inan
This study explores the manner in which the plasmapause is responsible for dictating which magnetospheric source regions of ELF/VLF chorus are able to propagate to and be received by midlatitude stations on the ground. First, we explore the effects of plasmapause extent on ground‐based observations of chorus via a 3 month study of ground‐based measurements of chorus at Palmer Station, Antarctica (L = 2.4, 50°S geomagnetic latitude), and data on the plasmapause extent from the IMAGE EUV instrument. It is found that chorus normalized occurrence peaks when the plasmapause is at L ∼ 2.6, somewhat higher than Palmers L shell, and that this occurrence peak persists across a range of observed chorus frequencies. Next, reverse ray tracing is employed to evaluate the portion of the equatorial chorus source region, distributed in radial distance and wave normal, from which chorus is able to reach Palmer Station via propagation in a nonducted mode. The results of ray tracing are similar to those of observations, with a peak of expected occurrence when the plasmapause is at L ∼ 3. The exact location of the peak is frequency dependent. This supports the conclusion that the ability of chorus to propagate to low altitudes and the ground is a strong function of instantaneous plasmapause extent and that peak occurrence of chorus at a given ground station may occur when the L shell of the plasmapause is somewhat beyond that of the observing station. These results also suggest that chorus observed on the ground at midlatitude stations propagates predominantly in the nonducted mode.
Physics of Plasmas | 2011
F. R. Foust; T. F. Bell; M. Spasojevic; U. S. Inan
We present results showing the measured Landau damping rate using a high-order discontinuous Galerkin particle-in-cell (DG-PIC) [G. B. Jacobs and J. S. Hesthaven, J. Comput. Phys. 214, 96 (2006)] method. We show that typical damping rates measured in particle-in-cell (PIC) simulations can differ significantly from the linearized Landau damping coefficient and propose a simple numerical method to solve the plasma dispersion function exactly for moderate to high damping rates. Simulation results show a high degree of agreement between the high-order PIC results and this calculated theoretical damping rate.
Geophysical Research Letters | 2007
J. A. Payne; U. S. Inan; F. R. Foust; T. W. Chevalier; T. F. Bell
Journal of Geophysical Research | 2013
Nicholas L. Bunch; M. Spasojevic; Y. Y. Shprits; Xudong Gu; F. R. Foust
Journal of Geophysical Research | 2010
F. R. Foust; U. S. Inan; T. F. Bell; N. G. Lehtinen
Journal of Geophysical Research | 2013
K. L. Graf; M. Spasojevic; R. A. Marshall; N. G. Lehtinen; F. R. Foust; U. S. Inan
Journal of Geophysical Research | 2011
F. R. Foust; M. Spasojevic; T. F. Bell; U. S. Inan
Journal of Geophysical Research | 2013
Nicholas L. Bunch; M. Spasojevic; Y. Y. Shprits; Xudong Gu; F. R. Foust
Journal of Geophysical Research | 2013
K. L. Graf; M. Spasojevic; R. A. Marshall; N. G. Lehtinen; F. R. Foust; U. S. Inan
Journal of Geophysical Research | 2011
F. R. Foust; M. Spasojevic; T. F. Bell; U. S. Inan