Swarm SCARF Dedicated Ionospheric Field Inversion chain

The geomagnetic daily variation at mid-to-low latitudes, referred to as the geomagnetic Sq field, is generated by electrical currents within the conducting layers of the ionosphere on the dayside of the Earth. It is enhanced in a narrow equatorial band, due to the equatorial electrojet. The upcoming...

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Veröffentlicht in:Earth, planets, and space Jg. 65; H. 11; S. 1271 - 1283
Hauptverfasser: Chulliat, Arnaud, Vigneron, Pierre, Thébault, Erwan, Sirol, Olivier, Hulot, Gauthier
Format: Journal Article
Sprache:Englisch
Veröffentlicht: Berlin/Heidelberg Springer Berlin Heidelberg 01.01.2013
Springer Nature B.V
Springer / Terra Scientific Publishing Company
Schlagworte:
Algorithms
Earth and Environmental Science
Earth orbits
Earth Sciences
Geology
Geophysics
Geophysics/Geodesy
Ionosphere
Magnetic fields
Research institutions
Satellites
Sciences of the Universe
inversion
space magnetometry
ionosphere
geomagnetism
Swarm
ISSN:1343-8832, 1880-5981
Online-Zugang:Volltext
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Zusammenfassung:The geomagnetic daily variation at mid-to-low latitudes, referred to as the geomagnetic Sq field, is generated by electrical currents within the conducting layers of the ionosphere on the dayside of the Earth. It is enhanced in a narrow equatorial band, due to the equatorial electrojet. The upcoming ESA Swarm satellite mission, to be launched end of 2013, will consist of three satellites in low-Earth orbit, providing a dense spatial and temporal coverage of the ionospheric Sq field. A Satellite Constellation Application and Research Facility (SCARF) has been set up by a consortium of research institutions, aiming at producing various level-2 data products during the Swarm mission. The Dedicated Ionospheric Field Inversion (DIFI) chain is a SCARF algorithm calculating global, spherical harmonic models of the Sq field at quiet times. It describes seasonal and solar cycle variations, separates primary and induced magnetic fields based upon advanced 3D-models of the mantle electrical conductivity, and relies on core, lithospheric and magnetospheric field models derived from other SCARF algorithms for removing non-ionospheric fields from the data. The DIFI chain was thoroughly tested on synthetic data during the SCARF preparation phase; it is now ready to be used for deriving models from real Swarm data.
Bibliographie:SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 14
ISSN:1343-8832
1880-5981
DOI:10.5047/eps.2013.08.006