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Association of large geomagnetic storms with halo CMEs and CIRs observed during 1997–2007

机译:在1997-2007年期间观测到的大型地磁风暴与晕波CME和CIR的关联

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In the present study, we have analysed large geomagnetic storms associated with storm time index (Dst) decrease of more than 100 nT observed during 1997–2007 and found 90 geomagnetic storms falling in our selection criteria. We have analyzed the association of the above selected 90 large geomagnetic storms with three types of solar drivers: single front-side halo CME (S-type), multiple front-side halo CMEs (M-type) and corotating interaction region, CIR (C-type). It is found that 58% storms were caused by single front-side halo CME (S-type), whereas 30% storms were caused by multiple front-side halo CMEs (M-type). Rest 12% storms were caused by corotating interaction region (CIR). We find that there is an east-west asymmetry and north-south asymmetry as well. We have also shown the association of the selected 90 large geomagnetic storms with three types of surface source region: active region, quiet region and coronal holes. We find that 62% storms were caused by active region whereas 10% storms were caused by quiet region. 12% storms were caused by coronal holes. Surface source region of rest 16% storms are unknown due to data gap.
机译:在本研究中,我们分析了与1997-2007年间暴风雨时间指数(D sub )下降超过100 nT相关的大型地磁暴雨,发现有90个地磁暴雨符合我们的选择标准。我们分析了以上选择的90个大地磁风暴与三种类型的太阳驱动器的关联:单个正面晕CME(S型),多个正面晕CME(M型)和同向相互作用区域CIR( C型)。发现58%的风暴是由单个正面光晕CME(S型)引起的,而30%的风暴是由多个正面光晕CME(M型)引起的。其余12%的风暴是由共同作用区域(CIR)引起的。我们发现还有东西向不对称和南北不对称。我们还显示了所选的90个大型地磁风暴与三种类型的地表源区域的关联:活动区域,安静区域和日冕洞。我们发现62%的风暴是由活动区域引起的,而10%的风暴是由安静区域引起的。 12%的风暴是由日冕孔引起的。由于数据缺口,其余16%风暴的地表源区域未知。

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