Award Abstract # 0955404
CAREER: 3-D Global Full Maxwell's Equations Modeling of the Effects of a Coronal Mass Ejection on the Earth

NSF Org: AGS
Division of Atmospheric and Geospace Sciences
Recipient: UNIVERSITY OF NEW MEXICO
Initial Amendment Date: August 25, 2010
Latest Amendment Date: August 25, 2010
Award Number: 0955404
Award Instrument: Standard Grant
Program Manager: Robert M. Robinson
AGS
 Division of Atmospheric and Geospace Sciences
GEO
 Directorate for Geosciences
Start Date: September 1, 2010
End Date: May 31, 2013 (Estimated)
Total Intended Award Amount: $462,507.00
Total Awarded Amount to Date: $462,507.00
Funds Obligated to Date: FY 2010 = $157,916.00
History of Investigator:
  • Jamesina Simpson (Principal Investigator)
    jamesina.simpson@utah.edu
Recipient Sponsored Research Office: University of New Mexico
1 UNIVERSITY OF NEW MEXICO
ALBUQUERQUE
NM  US  87131-0001
(505)277-4186
Sponsor Congressional District: 01
Primary Place of Performance: University of New Mexico
1 UNIVERSITY OF NEW MEXICO
ALBUQUERQUE
NM  US  87131-0001
Primary Place of Performance
Congressional District:
01
Unique Entity Identifier (UEI): F6XLTRUQJEN4
Parent UEI:
NSF Program(s): AERONOMY,
MAGNETOSPHERIC PHYSICS,
EPSCoR Co-Funding
Primary Program Source: 01001011DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 1187, 4444, 1045, 0000, OTHR, 9150
Program Element Code(s): 152100, 575000, 915000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

This project will develop a global numerical model of the electromagnetic fields produced by ionospheric electromagnetic currents with the research goal of enabling better prediction of the impact of space weather on the electric power grid. The methodology involves finite-difference time domain (FDTD) computational solutions of the full-vector three-dimensional time-dependent Maxwell's equations for electromagnetic wave propagation within the global Earth-ionosphere system. In particular, the atmosphere-lithosphere volume between 400 km above the Earth's surface to 400 km below will be studied in unprecedented detail at high spatial resolutions. The research will build on previous and current work in this area by using Active Magnetosphere and Planetary Electrodynamics Response Experiment (AMPERE) data and by establishing collaborations with the Electric Power Research Institute SUNBURST monitoring network project. The model will simulate the effects of ionospheric currents that develop as the result of coronal mass ejections in order to improve our understanding of the resultant electrodynamics. The fine spatial resolution of the newly computed FDTD solutions will provide improved information for assessing and mitigating potential hazards specific to the operations of inland and coastal power grids and oil pipelines. One education goal is to develop a sequence of three computational electromagnetic courses at the University of New Mexico. A second goal is to initiate and establish a Residential College system at the University of New Mexico.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Jamesina J. Simpson "On the possibility of high-level transient coronal mass ejection - induced ionospheric current coupling to electric power grids" Journal of Geophysical Research -- Space Physics , v.116, A1 , 2011 10.1029/2011JA016830
Y. Yu and J. J. Simpson "A magnetic field-independent absorbing boundary condition for magnetized cold plasma" IEEE Antennas and Wireless Propagation Letters , v.10 , 2011 , p.294-297 10.1109/LAWP.2011.2139191

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