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Comparing the Dynamic Global Core Plasma Model with ground-based plasma mass density observations
被引:8
|作者:
Jorgensen, Anders M.
[1
]
Heilig, Balazs
[2
]
Vellante, Massimo
[3
]
Lichtenberger, Janos
[4
,5
]
Reda, Jan
[6
]
Valach, Fridrich
[7
]
Mandic, Igor
[8
]
机构:
[1] New Mexico Inst Min & Technol, Elect Engn Dept, Socorro, NM 87801 USA
[2] Geol & Geophys Inst Hungary, Budapest, Hungary
[3] Univ Aquila, Dept Phys & Chem Sci, Laquila, Italy
[4] Eotvos Lorand Univ, Dept Geophys & Space Sci, Budapest, Hungary
[5] RCAES, Geodet & Geophys Inst, Sopron, Hungary
[6] Polish Acad Sci, Inst Geophys, Warsaw, Poland
[7] Slovak Acad Sci, Earth Sci Inst, Geomagnet Observ, Hurbanovo, Slovakia
[8] Univ Zagreb, Dept Geophys, Zagreb, Croatia
关键词:
plasmasphere;
field line resonance;
ground based;
modeling;
inner magnetosphere;
magnetometer data;
FIELD LINE RESONANCES;
GEOSYNCHRONOUS ORBIT;
ELECTRON-DENSITY;
IONOSPHERE;
D O I:
10.1002/2016JA023229
中图分类号:
P1 [天文学];
学科分类号:
0704 ;
摘要:
The Dynamic Global Core Plasma Model (DGCPM) is an empirical dynamical model of the plasmasphere which, despite its simple mathematical form, or perhaps because of its simple mathematical form, has enjoyed wide use in the space physics modeling community. In this paper we present some recent observations from the European quasi-Meridional Magnetometer Array (EMMA) and compare these with the DGCPM. The observations suggest more rapid daytime refilling and loss than what is described in the DGCPM. We then modify the DGCPM by changing the values of some of its parameters, leaving the functional form intact. The modified DGCPM agrees much better with the EMMA observations. The modification resulted in an order-of-magnitude faster daytime refilling and nighttime loss. These results are also consistent with previous observations of daytime refilling.
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页码:7997 / 8013
页数:17
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