Substorms manifestation at high and mid-latitudes during two large magnetic storm

IF 0.6 Q4 ENGINEERING, AEROSPACE
V. Guineva, I. Despirak, N. Kleimenova
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引用次数: 1

Abstract

The dynamics of magnetic substorms at high and middle latitudes during two severe geomagnetic storms: on 17March 2015 and on 22–23 June2015has been analyzed. The storms were rather similar: both storms were a result of the solar wind Sheath impact and both storms were characterized by a strong intensity (SYM/Hmin<–200nT). We studied the magnetic substorms during these storms on the base of the INTERMAGNET and IMAGE networks data. The attendant solar wind and Interplanetary Magnetic Field (IMF) parameters were taken from the OMNI data base. The spatial-temporal dynamics of three substorms was studied in detail: at 17:29 UT and at 22:55 UT during the first storm and at 18:33 UT during the second storm. The substorms on 17.03.2015originated during the main storm phase, and the onset of the substorm on 22.06.2015 followed the storm sudden commencement (SSC) of the second storm. All three substorms were characterized by a sharp poleward expansion of the westward electrojet simultaneously with a slower motion to lower latitudes. They were observed also at middle and low latitudes as positive magnetic bays. The westward electrojet reached ~71°CGMLat during the first two substorms and surpassed 75°CGMLat during the third substorm. Therefore, the first two events were “classical” substorms, and the third one –an “expanded” substorm. We suggested that this behavior is related to the different solar wind conditions: the “classical” substorms developed under magnetic cloud (MC) conditions, and the “expanded” –under the Sheath region effect.
两次大磁暴期间高纬度和中纬度亚暴的表现
分析了2015年3月17日和2015年6月22日至23日两次强地磁暴期间高纬度和中纬度地区磁亚暴的动力学特征。两场风暴非常相似:两场风暴都是太阳风鞘层撞击的结果,两场风暴的特征都是强强度(SYM/Hmin< -200nT)。我们利用INTERMAGNET和IMAGE网络资料研究了这些风暴期间的磁亚暴。伴随的太阳风和行星际磁场(IMF)参数取自OMNI数据库。详细研究了第一次风暴期间17:29、22:55和第二次风暴期间18:33三个亚暴的时空动态。2015年3月17日的次暴发生在主风暴阶段,2015年6月22日的次暴发生在第二次风暴突然开始(SSC)之后。这三次亚暴的特征都是西向电喷流向极地急剧扩张,同时向低纬度移动速度较慢。它们在中低纬度地区也被观察到为正磁湾。西向电急流在前两次亚暴期间达到~71°CGMLat,在第三次亚暴期间超过75°CGMLat。因此,前两个事件是“经典”亚暴,而第三个事件是“扩展”亚暴。我们认为这种行为与不同的太阳风条件有关:“经典”亚暴是在磁云(MC)条件下形成的,而“扩展”是在鞘区效应下形成的。
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来源期刊
Aerospace Research in Bulgaria
Aerospace Research in Bulgaria ENGINEERING, AEROSPACE-
自引率
33.30%
发文量
17
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