Geomagnetic variation consists of quiet variation, which is regular in appearance and mostly of solar electromagnetic radiation origin, and geomagnetic disturbance, which is irregular in appearance and mostly driven by the solar wind. The purpose of the Kp index, or Kp for short, is to monitor subauroral geomagnetic disturbance on a global scale. Bartels (1949) introduced the standardized Ks and the planetary Kp indices (see also Bartels, 1957aBartels, , 1957bSiebert & Meyer, 1996), which are derived from observatory-specific three-hourly K indices (Bartels, 1938(Bartels, , 1939Bartels et al., , 1940. The methodology to determine Ks and Kp indices is based on earlier indices, namely the global Km index and the reduced Kr and global Kw indices (Bartels et al., 1940). The K index, for which is an early and excellent description in English, is defined as a quasi-logarithmic measure, ranging in steps of 1 from 0 to 9, of the range of geomagnetic disturbance at a geomagnetic observatory in a three-hourly UT interval (00-03, 03-06, …, 21-24). Geomagnetic disturbance is also denoted as K-variation. The concept of K-variation, also referred to as geomagnetic activity or disturbance, predates the discovery of the solar wind and historically, K-variation was seen as the effect of 'solar particle radiation' (e.g. Bartels, 1957a). Siebert (1971) and Siebert and Meyer (1996) use this definition: "K-variations are all irregular disturbances of the geomagnetic field caused by solar particle radiation within the 3 h interval concerned. All other regular and irregular disturbances are non-K-variations. Geomagnetic activity is the occurrence of K-variations." We regard geomagnetic disturbance that is instantaneously driven by the solar wind as K-variation.The sum of the K-variation and its counterpart, the non-K-variation, equals the measured geomagnetic field variation at a geomagnetic observatory. K-variation includes geomagnetic pulsations, bays or substorms, sudden commencements, geomagnetic storms (with the exception of the recovery phase, see below) and other geomagnetic disturbance from fast changes in the ring-current and other magnetospheric and ionospheric currents. The non-K-variation includes phenomena related to energetic electromagnetic solar radiation (EUV, X-ray) like the daily solar and lunar quiet variation Yamazaki & Maute, 2017) and the rare solar flare effects (SFE;Curto & Gaya-Piqué, 2009;Veldkamp & van Sabben, 1960). However, some phenomena that are related to the solar wind also contribute to the non-K-variation because of their regular appearance. Examples are the quiet-time magnetospheric fields of the tail current, the magnetopause current and the ring current that appear as diurnal variation of the geomagnetic field at a point rotating with the Earth (e.g., Maus & Lühr, 2005). Another example is the slow decay of the ring current field in the recovery phase of a geomagnetic storm (e.g., Kamide & Maltsev, 2007). While the ring current field is driven by the solar wind, its decay in the recovery phase i...