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Development of substorm bulges during storms of different interplanetary origins

机译:在不同行星际起源的暴风雨中亚暴风雨凸起的发展

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Different solar wind structures are observed: magnetic clouds (MC), recurrent streams (RS), and regions of their interaction with undisturbed solar wind (Sheath and CIR). Three of these structures, Sheath, CIR, MC, are the sources of geomagnetic storms. We have searched for distinctions in the development of substorm bulges occurring during geomagnetic storms connected with the MC, Sheath and CIR. Solar wind parameters were taken from the Wind spacecraft and the auroral bulge parameters were obtained from the Ultra Violet Imager onboard Polar spacecraft. We determined the dimensions of the auroral bulges, the poleward aurora propagation, and the onset latitude of auroral bulges. It is shown that auroral bulges "geometry" is different for the examined types of storms. In consequence, the ratio between longitudinal and latitudinal sizes is also different.
机译:观察到不同的太阳风结构:磁云(MC),循环流(RS)以及它们与不受干扰的太阳风的相互作用区域(鞘和CIR)。这些结构中的三个,Sheath,CIR,MC是地磁风暴的来源。我们一直在寻找与MC,Sheath和CIR相关的地磁风暴期间发生的亚风暴凸起的发展差异。太阳风参数来自“风”飞船,而极光凸起参数则来自极地飞船上的“紫外线成像仪”。我们确定了极光凸起的尺寸,极地极光的传播以及极光凸起的起始纬度。结果表明,对于所检查的风暴类型,极光凸起的“几何形状”是不同的。结果,纵向尺寸和横向尺寸之间的比率也不同。

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