| dc.description.abstract |
In this paper, we present the responses of the ionospheric total electron content (TEC) to coronal
mass ejection (CME), and co-rotating interaction region (CIR) driven storms using stations that
lie 37
E-39
E geographic longtude in low latitude region from 2013-2017. CME driven geomagnetic
storm generally characterised by strong magnetic field, low proton temperature, enhanced
solar wind speed and short recovery phase, while CIR driven storm have been characterised by
weak magnetic field, high temperature and long recovery phase as compared with CME driven
storm. Disturbance time index(Dst
<-88nT ) were considered for this study. In this study
three CIR and seven CME driven geomagnetic storm has been selected with available TEC data
over the selected year and GPS station. TEC data used in this study was derived from the Global
Navigation Satellite System observations in RINEX format, that processed by Gps-Gopi soft
ware, and ploted by matlab program by importing the file. Statistical analysis of ionospheric
storm effect were computed over the selected GPS station by computing VTEC deviation from
quiet day monthly running median of VTEC. The number of CIR driven storm is more dominant
during the decline phase of the solar cycle period. The number of CME is maximum during
March equinox and June solistic.
Our analysis had been shown positive ionospheric response is more prolonged during the recovery
for CIR driven storm in the evenning and non significant response during the main phase. Positive
ionospheric response highly observed during the main and recovery phase of CME driven driven
storm. On low latitude, most positive response obserbed before sunrise at around the midnight
due to higher order of ionospheric irregularity.
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