Statistical analysis of ionospheric responses to solar flares in the solar cycle 23

2013 ◽  
Vol 118 (1) ◽  
pp. 576-582 ◽  
Author(s):  
Huijun Le ◽  
Libo Liu ◽  
Yiding Chen ◽  
Weixing Wan
Solar Physics ◽  
2015 ◽  
Vol 290 (3) ◽  
pp. 841-874 ◽  
Author(s):  
M. Dierckxsens ◽  
K. Tziotziou ◽  
S. Dalla ◽  
I. Patsou ◽  
M. S. Marsh ◽  
...  

2015 ◽  
Vol 55 (2) ◽  
pp. 696-704 ◽  
Author(s):  
R. Mawad ◽  
Mosalam Shaltout ◽  
M. Ewaida ◽  
M. Yousef ◽  
S. Yousef

2008 ◽  
Vol 113 (A8) ◽  
pp. n/a-n/a ◽  
Author(s):  
Y. Zhang ◽  
W. Sun ◽  
X. S. Feng ◽  
C. S. Deehr ◽  
C. D. Fry ◽  
...  

2019 ◽  
Vol 5 (2) ◽  
pp. 76-80
Author(s):  
Владимир Смирнов ◽  
Vladimir Smirnov ◽  
Елена Смирнова ◽  
Elena Smirnova

Using data from the GPS and GLONASS navigation satellite systems, we analyze the responses of the mid-latitude ionosphere to the extreme solar flares that occurred at the maximum of solar cycle 23 (October 28, 2003) and at the minimum of solar cycle 24 (September 6, 2017) during the same season at close solar zenith angles. To obtain the response, we use the rate of change of the total electronic content, which is practically independent of characteristics of equipment and is determined only by parameters of a propagation medium (the ionosphere in our case). The ionospheric response is shown to be almost independent of the total duration of the flare. In both cases, the duration of the main response at a level of 0.5 is about 1.5–2 min, whereas the total duration of the response is about 10 min and fairly independent of solar flare importance.


2006 ◽  
Vol 24 (12) ◽  
pp. 3569-3583 ◽  
Author(s):  
R. Rawat ◽  
S. Alex ◽  
G. S. Lakhina

Abstract. The frequency of occurrence of disruptive transient processes in the Sun is enhanced during the high solar activity periods. Solar cycle-23 evidenced major geomagnetic storm events and intense solar energetic particle (SEP) events. The SEP events are the energetic outbursts as a result of acceleration of heliospheric particles by solar flares and coronal mass ejections (CMEs). The present work focuses on the geomagnetic variations at equatorial and low-latitude stations during the four major SEP events of 14 July 2000, 8 November 2000, 24 September 2001 and 4 November 2001. These events have been reported to be of discernible magnitude following intense X-ray flares and halo coronal mass ejections. Low-latitude geomagnetic records evidenced an intense main phase development subsequent to the shock impact on the Earth's magnetosphere. Satellite observations show proton-flux enhancements associated with solar flares for all events. Correlation analysis is also carried out to bring out the correspondence between the polar cap magnetic field perturbations, AE index and the variations of low-latitude magnetic field. The results presented in the current study elucidate the varying storm development processes, and the geomagnetic field response to the plasma and interplanetary magnetic field conditions for the energetic events. An important inference drawn from the current study is the close correspondence between the persistence of a high level of proton flux after the shock in some events and the ensuing intense magnetic storm. Another interesting result is the role of the pre-shock southward IMF Bz duration in generating a strong main phase.


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