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An empirical model for prediction of geomagnetic storms using initially observed CME parameters at the Sun
被引:26
作者:
Kim, R. -S.
[1
,2
]
Cho, K. -S.
[3
]
Moon, Y. -J.
[4
]
Dryer, M.
[5
]
Lee, J.
[6
]
Yi, Y.
[1
]
Kim, K. -H.
[4
]
Wang, H.
[6
]
Park, Y. -D.
[3
]
Kim, Yong Ha
[1
]
机构:
[1] Chungnam Natl Univ, Dept Astron & Space Sci, Taejon 305754, KR, South Korea
[2] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[3] Korea Astron & Space Sci Inst, Solar & Space Weather Res Grp, Taejon 305348, KR, South Korea
[4] Kyung Hee Univ, Sch Space Res, Yongin 446701, KR, South Korea
[5] Natl Ocean & Atmospher Adm, Boulder, CO 80305 USA
[6] New Jersey Inst Technol, Dept Phys, Newark, NJ 07102 USA
关键词:
CORONAL MASS EJECTIONS;
INTERPLANETARY SHOCK;
EARTHWARD DIRECTION;
SOLAR-WIND;
HALO CMES;
GEOEFFECTIVENESS;
D O I:
10.1029/2010JA015322
中图分类号:
P1 [天文学];
学科分类号:
0704 ;
摘要:
In this study, we discuss the general behaviors of geomagnetic storm strength associated with observed parameters of coronal mass ejection (CME) such as speed (V) and earthward direction (D) of CMEs as well as the longitude (L) and magnetic field orientation (M) of overlaying potential fields of the CME source region, and we develop an empirical model to predict geomagnetic storm occurrence with its strength (gauged by the Dst index) in terms of these CME parameters. For this we select 66 halo or partial halo CMEs associated with M-class and X-class solar flares, which have clearly identifiable source regions, from 1997 to 2003. After examining how each of these CME parameters correlates with the geoeffectiveness of the CMEs, we find several properties as follows: (1) Parameter D best correlates with storm strength Dst; (2) the majority of geoeffective CMEs have been originated from solar longitude 15 W, and CMEs originated away from this longitude tend to produce weaker storms; (3) correlations between Dst and the CME parameters improve if CMEs are separated into two groups depending on whether their magnetic fields are oriented southward or northward in their source regions. Based on these observations, we present two empirical expressions for Dst in terms of L, V, and D for two groups of CMEs, respectively. This is a new attempt to predict not only the occurrence of geomagnetic storms, but also the storm strength (Dst) solely based on the CME parameters.
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