Initial geomagnetic field model from Magsat vector data

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

14

Geomagnetism, Magnetic Field Configurations, Magsat Satellites, Secular Variations, Dipole Moments, Scalars, Spherical Harmonics, Vector Analysis

Scientific paper

Magsat data from the magnetically quiet days of November 5-6, 1979, were used to derive a thirteenth degree and order spherical harmonic geomagnetic field model, MGST(6/80). The model utilized both scalar and high-accuracy vector data and fit that data with root-mean-square deviations of 8.2, 6.9, 7.6 and 7.4 nT for the scalar magnitude, B(r), B(theta), and B(phi), respectively. The model includes the three first-order coefficients of the external field. Comparison with averaged Dst indicates that zero Dst corresponds with 25 nT of horizontal field from external sources. When compared with earlier models, the earth's dipole moment continues to decrease at a rate of about 26 nT/yr. Evaluation of earlier models with Magsat data shows that the scalar field at the Magsat epoch is best predicted by the POGO(2/72) model but that the WC80, AWC/75 and IGS/75 are better for predicting vector fields.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Initial geomagnetic field model from Magsat vector data does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Initial geomagnetic field model from Magsat vector data, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Initial geomagnetic field model from Magsat vector data will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-948508

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.