Nm. Rotanova et Sd. Odintsov, Model of the MAGSAT magnetic anomaly field over Europe using spherical capharmonic analysis, PHYS CH P A, 24(5), 1999, pp. 455-459
Citations number
15
Categorie Soggetti
Earth Sciences
Journal title
PHYSICS AND CHEMISTRY OF THE EARTH PART A-SOLID EARTH AND GEODESY
Based on the MAGSAT magnetic anomaly fields over Europe and the adjacent ar
eas spherical cap models have been derived. The method of spherical cap har
monic analysis, due to Haines (1985), has been applied for the modelling of
the MAGSAT magnetic anomalies. The data set used in the analysis included
the 1 degrees x 1 degrees gridded values of the MAGSAT anomaly fields betwe
en latitudes phi = 6 degrees to 60 degrees N and longitudes lambda = 19 deg
rees W to 70 degrees E. The pole of the cap is at phi = 33 degrees N and la
mbda = 26 degrees E and its half-angle is 40 degrees. The maximum index (K-
m,) of the model is 18 and the total number of model coefficients is 361. A
minimum wavelength corresponding to this index at the Earth's surface is s
imilar to 1000 km. The RMS deviations between the calculated and observed v
alues are similar to 4 nT for Delta X, similar to 3 nT for Delta Y, and 3,5
nT for Delta Z respectively. The spherical cap harmonic model was used for
the construction of magnetic anomaly maps for all components and at differ
ent altitudes. (C) 1999 Elsevier Science Ltd. All rights reserved.