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Relating 27-Day Averages of Solar, Interplanetary MediumParameters, and Geomagnetic Activity Proxies in SolarCycle 24
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  • Yvelice Soraya Castillo Rosales,
  • Maria Alexandra Pais,
  • João Fernandes,
  • Paulo Ribeiro,
  • Anna Morozova,
  • Fernando Pinheiro
Yvelice Soraya Castillo Rosales
National Autonomous University of Honduras, National Autonomous University of Honduras

Corresponding Author:yvelice.castillo@unah.edu.hn

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Maria Alexandra Pais
University of Coimbra, University of Coimbra
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João Fernandes
University of Coimbra,University of Coimbra, University of Coimbra,University of Coimbra
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Paulo Ribeiro
University of Coimbra, University of Coimbra
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Anna Morozova
Universidade de Coimbra, Universidade de Coimbra
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Fernando Pinheiro
Universidade de Coimbra, Universidade de Coimbra
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Abstract

We analyzed correlations between solar, interplanetary-medium parameters, and geomagnetic-activity proxies in 27-day averages (a Bartels rotation) for the 2009 – 2016 time interval. We considered two new proxies: I) Bzs GSM (Geocentric Solar Magnetic), calculated as the daily percentage of the IMF southward component along the GSM z-axis and then averaged every 27 days; ii) four magnetospheric indices (T-indices), calculated from the local north-south (X) contributions of the magnetosphere’s cross-tail (TAIL), the symmetric ring current (SRC), the partial ring current (PRC), and the Birkeland current (FAC), derived from the Tsyganenko and Sitnov (J. Geophys. Res. 110, A03208, 2005: TS05) semi-empirical magnetospheric model. Our results suggest, among the parameters tested here, solar facular areas, interplanetary-magnetic field intensity and new proxies derived here could be taken into account in an empirical model, with a 27-day resolution, to explain geomagnetic activity felt on the Earth’s surface in terms of solar surface features and the IMF condition. We further retrieve a clear annual oscillation in series of 27-day-mean values of toward/away asymmetries of geomagnetic-activity indices, which can be interpreted in the light of the Russell–McPherron hypothesis for the semiannual variation of geomagnetic activity (Russell, C.T., and R. L. McPherron (1973), J. Geophys. Res., 78, 92 – 108).