Space Weather Magnetometer Aboard GEO-KOMPSAT-2A
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Published:2020-10-21
Issue:8
Volume:216
Page:
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ISSN:0038-6308
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Container-title:Space Science Reviews
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language:en
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Short-container-title:Space Sci Rev
Author:
Magnes W.,Hillenmaier O.,Auster H.-U.,Brown P.,Kraft S.,Seon J.,Delva M.,Valavanoglou A.,Leitner S.,Fischer D.,Berghofer G.,Narita Y.,Plaschke F.,Volwerk M.,Wilfinger J.,Strauch C.,Ludwig J.,Constantinescu D.,Fornacon K.-H.,Gebauer K.,Hercik D.,Richter I.,Eastwood J. P.,Luntama J. P.,Hilgers A.,Heil M.,Na G. W.,Lee C. H.
Abstract
AbstractThe South Korean meteorological and environmental satellite GEO-KOMPSAT-2A (GK-2A) was launched into geostationary orbit at $128.2^{\circ}$
128.2
∘
East on 4 December 2018. The space weather observation aboard GK-2A is performed by the Korea Space Environment Monitor. It consists of three particle detectors, a charging monitor and a four-sensor Service Oriented Spacecraft Magnetometer (SOSMAG).The magnetometer design aims for avoiding strict magnetic cleanliness requirements for the hosting spacecraft and an automated on-board correction of the dynamic stray fields which are generated by the spacecraft. This is achieved through the use of two science grade fluxgate sensors on an approximately one meter long boom and two additional magnetoresistance sensors mounted within the spacecraft body.This paper describes the instrument design, discusses the ground calibration methods and results, presents the post-launch correction and calibration achievements based on the data which were acquired during the first year in orbit and demonstrates the in-flight performance of SOSMAG with two science cases.The dynamic stray fields from the GK-2A spacecraft, which was built without specific magnetic cleanliness considerations, are reduced up to a maximum factor of 35. The magnitude of the largest remnant field from an active spacecraft disturber is 2.0 nT. Due to a daily shadowing of the SOSMAG boom, sensor intrinsic offset oscillations with a periodicity up to 60 minutes and peak-to-peak values up to 5 nT remain in the corrected data product.The comparison of the cleaned SOSMAG data with the Tsyganenko 2004 magnetic field model and the magnetic field data from the Magnetospheric Multiscale mission demonstrates that the offset error is less than the required 5 nT for all three components and that the drift of the offsets over 10 months is less than 7 nT.Future work will include a further reduction of the remaining artefacts in the final data product with the focus on lessening the temperature driven sensor oscillations with an epoch based identification and correction.
Funder
European Space Agency
Publisher
Springer Science and Business Media LLC
Subject
Space and Planetary Science,Astronomy and Astrophysics
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