K, Kp, and ap Indices
The K-index is quasi-logarithmic local index of the 3-hourly range in magnetic activity
relative to an assumed quiet-day curve for a single geomagnetic observatory site. First
introduced by J. Bartels in 1938, it consists of a single-digit 0 thru 9 for each 3-hour
interval of the universal time day (UT).
The planetary 3-hour-range index Kp is the mean
standardized K-index from 13 geomagnetic observatories between 44 degrees and 60 degrees
northern or southern geomagnetic latitude. The scale is O to 9 expressed in thirds of a
unit, e.g. 5- is 4 2/3, 5 is 5 and 5+ is 5 1/3. This planetary index is designed to measure
solar particle radiation by its magnetic effects. The 3-hourly ap (equivalent range) index
is derived from the Kp index as follows:
Kp = 0o 0+ 1- 1o 1+ 2- 2o 2+ 3- 3o 3+ 4- 4o 4+
ap = 0 2 3 4 5 6 7 9 12 15 18 22 27 32
Kp = 5- 5o 5+ 6- 6o 6+ 7- 7o 7+ 8- 8o 8+ 9- 9o
ap = 39 48 56 67 80 94 111 132 154 179 207 236 300 400
Other planetary indices include the Ap* and AA*. The Ap* index is defined as the earliest occurring maximum 24-hour value obtained by
computing an 8-point running average of successive 3-hour ap indices during a geomagnetic storm
event and is uniquely associated with the storm event. The AA* index is similar to the Ap* index, but has a longer history and is based on reports from only two stations.
You can download the Kp, Ap, and other indices via
FTP
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