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Geoscientific Instrumentation, Methods and Data Systems An interactive open-access journal of the European Geosciences Union
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Volume 3, issue 1
Geosci. Instrum. Method. Data Syst., 3, 41–48, 2014
https://doi.org/10.5194/gi-3-41-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Calibration methods and results of the in-situ experiments...

Geosci. Instrum. Method. Data Syst., 3, 41–48, 2014
https://doi.org/10.5194/gi-3-41-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 16 Apr 2014

Research article | 16 Apr 2014

Background subtraction for the Cluster/CODIF plasma ion mass spectrometer

C. G. Mouikis, L. M. Kistler, G. Wang, and Y. Liu C. G. Mouikis et al.
  • Space Science Center, University of New Hampshire, Durham, New Hampshire, USA

Abstract. The CODIF instrument on the Cluster spacecraft is a time-of-flight (TOF) ion mass spectrometer. Although TOF spectrometers are relatively immune to background contamination due to the inherent double coincidence requirement, high background rates can still result in false coincidences. Along the Cluster orbit, false coincidences are commonly observed due to the penetrating radiation of relativistic electrons during the encounters with the Earth's radiation belts. A second type of background in these instruments occurs when events of one species fall into the time-of-flight range defined for another species. Although the fraction of the H+ events that spill into the He+ measurement is small, when the actual He+ fluxes are low this can result in significant contamination. In this paper we present two techniques that allow the subtraction of the false coincidences and the H+ "spill" from the CODIF measurements.

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