TY - JOUR
T1 - Grad-Shafranov reconstruction
T2 - An overview
AU - Sonnerup, Bengt U.Ö
AU - Hasegawa, Hiroshi
AU - Teh, Wai Leong
AU - Hau, Lin Ni
PY - 2006/9/1
Y1 - 2006/9/1
N2 - Grad-Shafranov reconstruction is a data analysis tool for the reconstruction of two-dimensional (2-D) coherent field and flow structures from data collected as the structures move past an observing platform. To date, the method has been applied with good success to reconstruct magnetohydrostatic structures in Earth's magnetopause, in the solar wind, and in the geomagnetic tail, as the structures move past one or more observing spacecraft. However, with suitable modification, the reconstruction method can be extended to other applications, three of which are presented here: 2-D magneto-hydrodynamic structures in which dynamically important field-aligned flow is present, 2-D flow transverse to the magnetic field in the magnetospheric low-latitude boundary layer, and 2-D ordinary gasdynamic/hydrodynamic flow. We develop the fundamental equations required in the reconstructions, both for isotropic pressure and, in Appendix A, for the case where the pressures parallel and perpendicular to the magnetic field are described by the double-polytropic laws. Applications to actual or simulated data are discussed but not included in the present paper.
AB - Grad-Shafranov reconstruction is a data analysis tool for the reconstruction of two-dimensional (2-D) coherent field and flow structures from data collected as the structures move past an observing platform. To date, the method has been applied with good success to reconstruct magnetohydrostatic structures in Earth's magnetopause, in the solar wind, and in the geomagnetic tail, as the structures move past one or more observing spacecraft. However, with suitable modification, the reconstruction method can be extended to other applications, three of which are presented here: 2-D magneto-hydrodynamic structures in which dynamically important field-aligned flow is present, 2-D flow transverse to the magnetic field in the magnetospheric low-latitude boundary layer, and 2-D ordinary gasdynamic/hydrodynamic flow. We develop the fundamental equations required in the reconstructions, both for isotropic pressure and, in Appendix A, for the case where the pressures parallel and perpendicular to the magnetic field are described by the double-polytropic laws. Applications to actual or simulated data are discussed but not included in the present paper.
UR - http://www.scopus.com/inward/record.url?scp=33947531686&partnerID=8YFLogxK
U2 - 10.1029/2006JA011717
DO - 10.1029/2006JA011717
M3 - 期刊論文
AN - SCOPUS:33947531686
SN - 2169-9380
VL - 111
JO - Journal of Geophysical Research: Space Physics
JF - Journal of Geophysical Research: Space Physics
IS - 9
M1 - A09204
ER -