Multivariable Comprehensive Analysis of Two Great Geomagnetic Storms of 2015

被引:28
|
作者
Kashcheyev, A. [1 ,2 ]
Migoya-Orue, Y. [1 ]
Amory-Mazaudier, C. [1 ,3 ]
Fleury, R. [4 ]
Nava, B. [1 ]
Alazo-Cuartas, K. [1 ]
Radicella, S. M. [1 ]
机构
[1] Abdus Salam Int Ctr Theoret Phys ICTP T ICT4D, Trieste, Italy
[2] Natl Acad Sci Ukraine, Inst Radio Astron, Dept Radiophys Geospace, Kharkov, Ukraine
[3] UPMC Univ Paris 06, Sorbonne Univ, Lab Phys Plasmas, UMR 7648, Paris, France
[4] UMR6285 Inst Mines Telecom, LAB STICC, Brest, France
关键词
geomagnetic storm; multivariable analysis; ionosphere; plasma bubble; PATRICKS DAY STORM; IONOSPHERIC DISTURBANCE DYNAMO; MAGNETIC STORMS; LOW-LATITUDE; THERMOSPHERE; FLUCTUATIONS; MIDDLE; EVENT; GPS;
D O I
10.1029/2017JA024900
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
During the year 2015 two great geomagnetic storms (Dst < -200 nT) occurred on 17 March and 22 June. These two geomagnetic storms have similarities. They occurred during the same decreasing phase of the sunspot cycle 24. The interplanetary and magnetospheric environments were calm before the beginning of the storms. Both events were due to Coronal Mass Ejections and High-Speed Solar Wind. Variations of the solar wind velocity and the Bz component of the interplanetary magnetic field were also similar. Two key features that are different for these storms are UT time of the beginning (04:45 UT for 17 March and 18:33 UT for 22 June) and season (equinox and solstice). The comparison of the impact of the storms on the Earth ionosphere and magnetosphere has been performed using diverse parameters including global ionospheric maps of vertical total electron content, data from individual Global Navigation Satellite System receivers, ionosondes, magnetometers, and instruments from different space missions. Visualizing global ionospheric map data as the difference of vertical total electron content between consecutive days allowed understanding better the effect of the storms as a function of time of the beginning of the storm and of the season. It is shown that the presence or absence of scintillations in Global Navigation Satellite System signals during these two storms in African longitude sector is clearly related to the local time at a given station at the beginning of the storm.
引用
收藏
页码:5000 / 5018
页数:19
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