Nowcast Formulas for Kp from GOES Magnetometer Data

 

 

Results from UPOS Project COX

January 2004

 

Patrick T. Newell

Johns Hopkins University Applied Physics Laboratory

 

 

Background:

   When the GOES satellites are on the nightside of the Earth, the extent to which the Earth’s magnetic field has been stretched from its natural dipole inclination into a long magnetotail is measured by the GOES magnetometers.  The more stretched the Earth’s magnetic field, the more active is the state of the magnetosphere.  GOES magnetometer data is available real-time from NOAA’s space data center.

   Kp is defined based on ground magnetometer stations, rather than actual space borne measurements.  Nonetheless, there is a substantial relationship (correlations between 0.4 and 0.75) between what is inferred from the ground via Kp over a 3-hour interval, and what is measured over the last hour by GOES while on the nightside.

 

Empirical Formulas for the GOES to Kp Relationship

 

   The following equations were developed under UPOS to convert the GOES nightside magnetometer readings into a nowcast Kp.  Note that when GOES is not at one of the listed local times, these formulas cannot be applied.  A running average over the previous 1 hour is used for the GOES data to reduce short term fluctuations.  (The inclination angles themselves are averaged, rather than an inclination angle being calculated from an average magnetic field).

   In terms of representing the state of the magnetosphere, these correlation coefficients understate the quality of the GOES data.  Kp itself is only a rough measure of the magnetosphere’s state, while magnetotail stretching is a rather basic property of the Earth’s space environment.  Thus the GOES “nowcast Kp” is actually an independent assessment of the magnetosphere’s condition, couched in the familiar Kp nomenclature.

 

T = magnetotail inclination angle

T = atan(v/h)

v,h are GOES magnetometer measurements

 

Kp = a*T + b

Kp is a number between 0 and 9

(T is measured in degrees in equations below)

 


 

GOES

Local Time                   a                      b                      corr. coeff. with actual Kp

 

16                                -0.110              16.9                 -0.75

17                                -0.077              13.4                 -0.52

18                                -0.050              10.4                 -0.52

19                                -0.136              22.0                 -0.69

20                                -0.045              8.7                   -0.47

21                                -0.050              10.0                 -0.52

22                                -0.040              8.5                   -0.16

23                                -0.041              8.0                   -0.42

00                                -0.064              12.0                 -0.55

01                                -0.041              9.0                   -0.16

02                                -0.076              12.7                 -0.60

03                                -0.095              17.2                 -0.63

04                                -0.098              16.9                 -0.53

05                                -0.047              8.8                   -0.41