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On the reconstruction of magnetospheric plasma pressure distributions from empirical geomagnetic field models. / Tsyganenko, N. A.

In: Journal of Geophysical Research: Space Physics, Vol. 115, No. A7, 07211, 15.07.2010.

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@article{90a374d880dc4f1ea5d8836be8154871,
title = "On the reconstruction of magnetospheric plasma pressure distributions from empirical geomagnetic field models",
abstract = "Four data-based models of the magnetospheric magnetic field were tested for the degree of their consistency with a static balance between the magnetic and plasma stresses. To that end, best fit distributions of the plasma sheet pressure and its anisotropy were derived in the midnight meridian plane, using two specific forms of the particle distribution function. The tailward limit of the modeling region was placed at R = 20 R(E), where the condition of pressure balance with the tail lobe field was used to avoid the multiplicity of solutions of the force balance equation. Best fit solutions were derived by minimizing the rms difference between the magnetic and plasma stress vectors over a set of points within the model plasma sheet at distances 5",
keywords = "DAWN-DUSK ASYMMETRY, MAGNETIC-FIELD, BIRKELAND CURRENTS, SHEET, BALANCE, CONSISTENT, PARAMETERS, ANISOTROPY",
author = "Tsyganenko, {N. A.}",
year = "2010",
month = jul,
day = "15",
doi = "10.1029/2009JA015012",
language = "Английский",
volume = "115",
journal = "Journal of Geophysical Research: Biogeosciences",
issn = "0148-0227",
publisher = "American Geophysical Union",
number = "A7",

}

RIS

TY - JOUR

T1 - On the reconstruction of magnetospheric plasma pressure distributions from empirical geomagnetic field models

AU - Tsyganenko, N. A.

PY - 2010/7/15

Y1 - 2010/7/15

N2 - Four data-based models of the magnetospheric magnetic field were tested for the degree of their consistency with a static balance between the magnetic and plasma stresses. To that end, best fit distributions of the plasma sheet pressure and its anisotropy were derived in the midnight meridian plane, using two specific forms of the particle distribution function. The tailward limit of the modeling region was placed at R = 20 R(E), where the condition of pressure balance with the tail lobe field was used to avoid the multiplicity of solutions of the force balance equation. Best fit solutions were derived by minimizing the rms difference between the magnetic and plasma stress vectors over a set of points within the model plasma sheet at distances 5

AB - Four data-based models of the magnetospheric magnetic field were tested for the degree of their consistency with a static balance between the magnetic and plasma stresses. To that end, best fit distributions of the plasma sheet pressure and its anisotropy were derived in the midnight meridian plane, using two specific forms of the particle distribution function. The tailward limit of the modeling region was placed at R = 20 R(E), where the condition of pressure balance with the tail lobe field was used to avoid the multiplicity of solutions of the force balance equation. Best fit solutions were derived by minimizing the rms difference between the magnetic and plasma stress vectors over a set of points within the model plasma sheet at distances 5

KW - DAWN-DUSK ASYMMETRY

KW - MAGNETIC-FIELD

KW - BIRKELAND CURRENTS

KW - SHEET

KW - BALANCE

KW - CONSISTENT

KW - PARAMETERS

KW - ANISOTROPY

U2 - 10.1029/2009JA015012

DO - 10.1029/2009JA015012

M3 - статья

VL - 115

JO - Journal of Geophysical Research: Biogeosciences

JF - Journal of Geophysical Research: Biogeosciences

SN - 0148-0227

IS - A7

M1 - 07211

ER -

ID: 5072883