We present an empirical model of the inner magnetosphere, based on proton measurements performed by the CHEM instrument in the energy range 1â300 keV and in the L-range 3â9 during 3 years of the AMPTE-CCE mission (1985 to 1987, i.e. near solar minimum). We have fitted the average proton fluxes at low geomagnetic activity (AE < 100 nT) and obtained a multi-parametric function, which is the sum of five different parts and depends on energy, L-shell, magnetic local time, and a few independent factors. The model is able to accurately reproduce the average perpendicular proton fluxes in the equatorial inner magnetosphere. The various segments of the model function reproduce the effects of physical processes, such as diffusion, on magnetospheric plasma. We describe the methodology followed for the development of the model. Empirical models like this one are critical in our effort to exploit global neutral atom imaging measurements of ongoing and future missions. Furthermore, they serve as a benchmark of theoretical models and numerical simulations of the inner magnetosphere.
Empirical model of proton fluxes in the equatorial inner magnetosphere. 1. Development
2001
Abstract
We present an empirical model of the inner magnetosphere, based on proton measurements performed by the CHEM instrument in the energy range 1â300 keV and in the L-range 3â9 during 3 years of the AMPTE-CCE mission (1985 to 1987, i.e. near solar minimum). We have fitted the average proton fluxes at low geomagnetic activity (AE < 100 nT) and obtained a multi-parametric function, which is the sum of five different parts and depends on energy, L-shell, magnetic local time, and a few independent factors. The model is able to accurately reproduce the average perpendicular proton fluxes in the equatorial inner magnetosphere. The various segments of the model function reproduce the effects of physical processes, such as diffusion, on magnetospheric plasma. We describe the methodology followed for the development of the model. Empirical models like this one are critical in our effort to exploit global neutral atom imaging measurements of ongoing and future missions. Furthermore, they serve as a benchmark of theoretical models and numerical simulations of the inner magnetosphere.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
