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GEOPHYSICAL RESEARCH LETTERS,
VOL. 33,
L18301,
doi:10.1029/2006GL027083,
2006
A global model of mantle conductivity derived from 5 years of CHAMP, Ørsted, and SAC-C magnetic data
Alexei Kuvshinov
Danish National Space Center, Copenhagen, Denmark
Nils Olsen
Danish National Space Center, Copenhagen, Denmark
Abstract
We present a global 1-D conductivity model which is obtained by analysis of five years (2001–2005) of simultaneous magnetic
data from the three satellites Ørsted, CHAMP and SAC-C. After removal of core and crustal fields as predicted by a recent
field model we used non-polar scalar and vector observations from the night-side sector, and interpret the field residuals
in terms of a large-scale contribution from the magnetospheric ring current and its induced counterpart. We then derive transfer
functions between internal (induced) and external expansion coefficients of the magnetic potential and provide globally-averaged
C-responses in the period range between 14 hours and 4 months. Since the satellite responses are probably influenced by induction
in the oceans for periods shorter than a few days, we correct the data for this effect. Interpreting the corrected responses
yields a 1-D conductivity model which is rather similar to models derived from ground-based data.
Received 2
June
2006;
accepted 1
August
2006;
published 16
September
2006.
Index Terms: 1515 Geomagnetism and Paleomagnetism: Geomagnetic induction; 1555 Geomagnetism and Paleomagnetism: Time variations: diurnal to decadal; 2778 Magnetospheric Physics: Ring current.
Read Full Article (file size: 411714 bytes) Cited by
Citation: Kuvshinov, A., and N. Olsen
(2006),
A global model of mantle conductivity derived from 5 years of CHAMP, Ørsted, and SAC-C magnetic data,
Geophys. Res. Lett.,
33,
L18301,
doi:10.1029/2006GL027083.
Copyright 2006 by the American Geophysical Union.
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