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Title: Comparison of equilibrium ohmic and nonequilibrium swarm models for monitoring conduction electron evolution in high-altitude EMP calculations

Journal Article · · Journal of Geophysical Research: Atmospheres
DOI:https://doi.org/10.1002/2016JD024970· OSTI ID:1329596
 [1];  [2];  [2]; ORCiD logo [3]
  1. Rensselaer Polytechnic Inst., Troy, NY (United States); Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
  2. Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
  3. Rensselaer Polytechnic Inst., Troy, NY (United States)

Abstract Atmospheric electromagnetic pulse (EMP) events are important physical phenomena that occur through both man‐made and natural processes. Radiation‐induced currents and voltages in EMP can couple with electrical systems, such as those found in satellites, and cause significant damage. Due to the disruptive nature of EMP, it is important to accurately predict EMP evolution and propagation with computational models. CHAP‐LA ( C ompton H igh A ltitude P ulse‐ L os A lamos) is a state‐of‐the‐art EMP code that solves Maxwell s equations for gamma source‐induced electromagnetic fields in the atmosphere. In EMP, low‐energy, conduction electrons constitute a conduction current that limits the EMP by opposing the Compton current. CHAP‐LA calculates the conduction current using an equilibrium ohmic model. The equilibrium model works well at low altitudes, where the electron energy equilibration time is short compared to the rise time or duration of the EMP. At high altitudes, the equilibration time increases beyond the EMP rise time and the predicted equilibrium ionization rate becomes very large. The ohmic model predicts an unphysically large production of conduction electrons which prematurely and abruptly shorts the EMP in the simulation code. An electron swarm model, which implicitly accounts for the time evolution of the conduction electron energy distribution, can be used to overcome the limitations exhibited by the equilibrium ohmic model. We have developed and validated an electron swarm model previously in Pusateri et al. (2015). Here we demonstrate EMP damping behavior caused by the ohmic model at high altitudes and show improvements on high‐altitude, upward EMP modeling obtained by integrating a swarm model into CHAP‐LA.

Research Organization:
Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)
Sponsoring Organization:
USDOE
Grant/Contract Number:
AC52-06NA25396
OSTI ID:
1329596
Alternate ID(s):
OSTI ID: 1402162
Report Number(s):
LA-UR-16-20896
Journal Information:
Journal of Geophysical Research: Atmospheres, Journal Name: Journal of Geophysical Research: Atmospheres; ISSN 2169-897X
Publisher:
American Geophysical UnionCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 11 works
Citation information provided by
Web of Science

References (5)

Determination of equilibrium electron temperature and times using an electron swarm model with BOLSIG+ calculated collision frequencies and rate coefficients journal August 2015
Femtosecond ultraviolet laser pulse induced lightning discharges in gases journal March 1995
Detection of the Electromagnetic Radiation from Nuclear Explosions in Space journal March 1965
On the Electromagnetic Pulse Produced by Nuclear Explosions journal February 1978
Prompt Nuclear EMP and Synchrotron Radiation: A Resolution of Two Approaches journal August 2005

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