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Geomagnetic and ionospheric response to the interplanetary shock on January 24, 2012

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Figure

Fig. 1 The interplanetary shock detected on January 24, 2012, during time interval 1400–1900 UT by GEOTAIL: the solar wind velocity [nent (km/s)], solar wind density Vx compo-N  (cm−3), plasma temperature (K), IMF magnetic field magnitude B (nT) and component Bz (nT), SYM-H index (nT), and AE index (nT)
Table 1 Magnetometers, riometers, and GPS receivers
Fig. 3 The magnetograms (X-component in  104 nT) of the latitudinal profile of stations TALO, RANK, FCHU, GILL, ISLL, PINA, and THRF from the CARISMA array during the time period 1440–1540 UT
Fig. 4 Data from the Russian Arctic shore magnetometers (X-component in  104 nT) AMD, DIK, TIK, and PBK and riometer TIX during the period 1400–2000 UT
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