Variations in the solar wind cause changes in electric currents that flow in the magnetosphere and ionosphere. The associated changes in the magnetic field can be observed using magnetometers on the ground. There exist various types of geomagnetic indices to monitor the intensity of geomagnetic disturbance associated with solar wind variations (Mayaud, 1980). The Kp index is one of the most widely used indices of geomagnetic activity. The derivation, application and historical background of Kp are detailed in , and thus are described here only briefly.Kp is derived from K indices (Bartels et al., 1939) evaluated at 13 subauroral observatories from both northern and southern hemispheres. A K index expresses geomagnetic activity on a scale of 0-9 at each observatory for a given 3-hourly interval of the UT day (00-03, 03-06, …, 21-24 UT). It is based on the range of geomagnetic disturbance over the 3-hourly interval, which may contain geomagnetic pulsations (McPherron, 2005;Saito, 1969), bays associated with substorms (McPherron, 1970;Lyons, 1996), sudden storm commencements and sudden impulses (Araki, 1994), geomagnetic storm main phase (Gonzalez et al., 1994) and solar-flare and eclipse effects (Yamazaki & Maute, 2017). K is designed to have a similar frequency distribution regardless of observatory, and thus it does not depend on latitude. K indices are converted to standardized Ks indices, which take into account the influence of seasonal and UT biases. Kp is the average of the 13 Ks indices expressed in units of thirds (0o, 0+, 1−, 1o, 1+, 2−, …, 9o), thus it represents planetary, rather than local, geomagnetic activity. The complete time series of the definitive Kp index since 1932 and nowcast indices for the most recent hours