In regions close to the polar circles highly dynamic polar lights can be seen regularly. They often move equatorward and exhibit many different colors. Such an event may indicate the start of a magnetic substorm, during which energetic particles are accelerated and move from the magnetosphere along the magnetic field lines into the upper atmosphere. During substorms records of the geomagnetic field exhibit very rapid variations.
The scientific payload of the five THEMIS spacecraft consists of a fluxgate magnetometer (FGM), instruments for the detection of low energetic particles (electrostatic analyzer, ESA) as well as high energetic particles (solid state telescope, SST), a search coil magnetometer (SCM), and an electric field instrument (EFI). One of the main instruments, the fluxgate magnetometer, was developed at the Institute for Geophysics and Extraterrestrial Physics of the University of Braunschweig. The calibration of the magnetometers was carried out in close cooperation with the Institute of Space Research in Graz.
In order to enhance our understanding of the plasmaphysical processes causing a substorm as well as to ascertain its development in space, the THEMIS mission (Time History of Events and Macroscopic Interactions during Substorms) was selected by NASA in March 2003 out of 42 competing proposals as a Medium Class Explorer (MIDEX) Mission. It consists of 5 spacecraft, which surround the Earth on highly elliptical orbits, and numerous ground stations located in the northern parts of the United States and Canada. With their help the temporal course of events during a substorm is being investigated. The particle populations in the radiation belts, the direct solar wind interaction with the terrestrial magnetic field and its indirect interaction with the ionospheric regions constitute other areas of scientific interest.
This project is financially supported by the German Bundesministerium für Wirtschaft und Technologie and the Deutsches Zentrum für Luft- und Raumfahrt under contract (Förderkennzeichen) 50 OC 0302.
The five THEMIS spacecraft were launched from the Kennedy Space Center at Cape Canaveral (Florida, USA) on February 17th, 2007. Launch and separation of the satellites from the launching vehicle were carried out smoothly. In the first months of operation (the coast phase) the five spacecraft were flying in a row on a common orbit. This string-of-pearls configuration has proven to be particularly helpful for the investigation of dayside wave phenomena occurring inside the magnetosphere and on its outer boundary, the magnetopause. The injection of the spacecraft into their final orbits took place in September, 2007. In this main mission configuration the probes align themselves at their apogees with the THEMIS ground stations. This configuration is, hence, optimal for the investigation of the spatial and temporal evolution of substorms. At the end of mission a second major configuration change is planned: Two of the spacecraft may be injected into a stabile orbit around the Moon to research its interaction with the solar wind and the magnetosphere of the Earth.
Currently there are two competing models to explain the substorm process: the Current-Disruption Model (CDM) und das Near Earth Neutral Line Model (NENL).
The CDM requires a local plasmainstability in the nightside magnetosphere at a distance of about 8-10 RE, causing a disruption of the tail current in the magnetosphere and subsequent closure of this current in the ionosphere. As a result of this current disruption a rarefaction wave is generated, propagating tailward at large velocities and triggering magnetic reconnection at about a distance of 25 RE.
In contrast to this the NENL requires magnetic reconnection at a distance of about 25 RE as the trigger of the substorm process. So-called bursty bulk flows transport large amounts of energy into the inner magnetosphere where this energy is converted to thermal energy and flow diversion around the Earth at the inner edge of the plasma sheet occurs. The field-aligned currents of the substorm current wedge are generated by the process.
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