Ionospheric Response to the Magnetic Storm of 22 June 2015

被引:15
|
作者
Mansilla, Gustavo A. [1 ,2 ]
机构
[1] Univ Nacl Tucuman, Fac Ciencias Exactas & Tecnol, Dept Fis, Av Independencia 1800, RA-4000 San Miguel De Tucuman, Tucuman, Argentina
[2] Consejo Nacl Invest Cient & Tecn, RA-2290 Godoy Cruz, Buenos Aires, Argentina
关键词
Geomagnetic storm; global TEC; physical mechanisms; GEOMAGNETIC STORMS; F2-REGION RESPONSE; REGION; THERMOSPHERE; DISTURBANCES; EQUATORIAL; LATITUDES; TEC;
D O I
10.1007/s00024-017-1741-5
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
A global study is made of the response of the total electron content of the ionosphere (TEC) to the geomagnetic storm occurred on 22 June 2015 (one of the strongest geomagnetic storms of the current Solar Cycle 24). Using data from 44 sites, a hemispheric comparison is made by considering high latitudes (> 50A degrees), middle latitudes (30A degrees-50A degrees) and low latitudes (30A degrees N-30A degrees S). The main features observed were: increases in TEC at high latitudes prior to the storm main phase, a considerable asymmetry of TEC response at middle and low latitudes of the Northern Hemisphere and the Southern Hemisphere and decreases at equatorial latitudes. The long duration enhancements in TEC were well correlated with increases in the O/N-2 ratio but decreases in TEC had not associated decreases in the O/N-2 ratio as occur with the decreases in the electron density. Besides, prompt penetration electric fields can play an important role in the equatorial and low-latitude ionosphere during main phase of the storm.
引用
收藏
页码:1139 / 1153
页数:15
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