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Ionospheric simulation compared with Dynamics Explorer observations for November 22, 1981
Author(s) -
Sojka J. J.,
Bowline M.,
Schunk R. W.,
Craven J. D.,
Frank L. A.,
Sharber J. R.,
Winningham J. D.,
Brace L. H.
Publication year - 1992
Publication title -
journal of geophysical research: space physics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/91ja02215
Subject(s) - ionosphere , substorm , electric field , polar , trough (economics) , convection , geophysics , precipitation , electron precipitation , atmospheric sciences , physics , geology , meteorology , magnetosphere , plasma , astronomy , quantum mechanics , economics , macroeconomics
Dynamics Explorer (DE) 2 electric field and particle data have been used to constrain the inputs of a time‐dependent ionospheric model (TDIM) for a simulation of the ionosphere on November 22, 1981. The simulated densities have then been critically compared with the DE 2 electron density observations. This comparison uncovers a model‐data disagreement in the morning sector trough, generally good agreement of the background density in the polar cap and evening sector trough, and a difficulty in modelling the observed polar F layer patches. From this comparison, the consequences of structure in the electric field and precipitation inputs can be seen. This is further highlighted during a substorm period for which DE 1 auroral images were available. Using these images, a revised dynamic particle precipitation pattern was used in the ionospheric model; the resulting densities were different from the original simulation. With this revised dynamic precipitation model, improved density agreement is obtained in the auroral/polar regions where the plasma convection is not stagnant. However, the dynamic study also reveals a difficulty of matching dynamic auroral patterns with static empirical convection patterns. In this case, the matching of the models produced intense auroral precipitation in a stagnation region, which, in turn, led to exceedingly large TDIM densities.

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