Issue |
EPJ Web Conf.
Volume 157, 2017
22 Topical Conference on Radio-Frequency Power in Plasmas
|
|
---|---|---|
Article Number | 02005 | |
Number of page(s) | 6 | |
Section | Invited Papers | |
DOI | https://doi.org/10.1051/epjconf/201715702005 | |
Published online | 23 October 2017 |
https://doi.org/10.1051/epjconf/201715702005
2D full-wave simulation of waves in space and tokamak plasmas
1 Princeton Plasma Physics Laboratory, Princeton University, Princeton NJ 08540, USA
2 Department of Engineering and Computer Science, Andrews University, Berrien Springs, MI 49103, USA
* Corresponding author: ehkim@pppl.gov
Published online: 23 October 2017
Simulation results using a 2D full-wave code (FW2D) for space and NSTX fusion plasmas are presented. The FW2D code solves the cold plasma wave equations using the finite element method. The wave code has been successfully applied to describe low frequency waves in planetary magnetospheres (i.e., dipole geometry) and the results include generation and propagation of externally driven ultra-low frequency waves via mode conversion at Mercury and mode coupling, refraction and reflection of internally driven field-aligned propagating left-handed electromagnetic ion cyclotron (EMIC) waves at Earth. In this paper, global structure of linearly polarized EMIC waves is examined and the result shows such resonant wave modes can be localized near the equatorial plane. We also adopt the FW2D code to tokamak geometry and examine radio frequency (RF) waves in the scape-off layer (SOL) of tokamaks. By adopting the rectangular and limiter boundary, we compare the results with existing AORSA simulations. The FW2D code results for the high harmonic fast wave heating case on NSTX with a rectangular vessel boundary shows excellent agreement with the AORSA code.
© The authors, published by EDP Sciences, 2017
This is an Open Access article distributed under the terms of the Creative Commons Attribution License 4.0, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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