Variability of Comet Halley's coma: VEGA-1 and VEGA-2 magnetic field observations

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Cometary Atmospheres, Halley'S Comet, Interplanetary Magnetic Fields, Plasma Diagnostics, Vega Project, Computerized Simulation, Discontinuity, Magnetic Field Configurations, Solar Wind

Scientific paper

The differences of the VEGA-1 and VEGA-2 magnetic field investigations near Comet Halley are discussed. The different draping structures of the magnetic field observed by VEGA-1 and VEGA-2 are caused by variations of the solar wind parameters and of the cometary activity during this period. The magnetic field reversal region observed only during the closest approach of VEGA-1 is correlated with high energetic particle streams and ground-based observations of a disconnection event. A broad minimum of the wave activity during the inbound phase of both encounters occurs in the same region where a substantial change of the slope of the total magnetic field and of the plasma velocity takes place and where the observed neutral gas density has a discontinuity. The VEGA-1 and -2 magnetic field observations are compared with the results of 3-D MHD computer simulations. It is concluded that most of the measured variability is the result of IMF variations.

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