30 June 2013 to 3 July 2013
Island of Santorini, Greece (http://en.wikipedia.org/wiki/Santorini)
Europe/Athens timezone

Search for a Radiation Belts Storage Ring in the Cluster-CIS data

3 Jul 2013, 12:30
1h
Island of Santorini, Greece (http://en.wikipedia.org/wiki/Santorini)

Island of Santorini, Greece (http://en.wikipedia.org/wiki/Santorini)

Bellonio Cultural Centre, Fira
Poster Waves, Wave-Particle Interactions and Radiation Belt Dynamics Poster Session

Speaker

Iannis Dandouras (IRAP, CNRS / University of Toulouse)

Description

Following the launch by NASA of the Radiation Belt Storm Probes (RBSP) twin spacecraft, now named the Van Allen Probes, the discovery of a storage ring was announced: Baker et al., Science, 2013. This transient feature was observed during September 2012, following the arrival of an interplanetary shock, was located between L=3.0 and L=3.5 and consisted of about 4 to 6 MeV electrons. During that period the Cluster spacecraft had a high-inclination orbit, with a perigee just above 2 Re. The CIS experiment onboard Cluster is sensitive to penetrating energetic electrons (E > 2 MeV), which produce background counts and thus allow to localise the boundaries of the outer and inner radiation belts (Ganushkina et al., JGR, 2011). A search was undertaken in the September 2012 CIS data for eventual signatures of the storage ring, and indeed a small increase of the instrument background was observed between L=3.0 and L=3.5. This is clearly separated from the main outer radiation belt, which presents a much stronger background due to higher fluxes of relativistic electrons. A mono-energetic ion drift band was also observed by CIS inside the storage ring, at about 5 keV for He+ and O+ ions. This result provides an independent confirmation for the storage ring. In addition, it allows also to examine Cluster data from earlier years, covering a full solar cycle, for other such signatures of a transient storage ring.

Primary author

Iannis Dandouras (IRAP, CNRS / University of Toulouse)

Co-authors

Henri Reme (IRAP, CNRS / University of Toulouse) Natalia Ganushkina (Finnish Meteorological Institute)

Presentation materials

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