The Location of the Reconnection line for Northward IMF

Mathematics – Probability

Scientific paper

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7835 Magnetic Reconnection

Scientific paper

The interconnection of magnetic fields through magnetic reconnection at the magnetopause is the dominant process for mass, energy and momentum transfer from the Earth's magnetosheath to the magnetosphere. Earlier studies on the location of the reconnection line during northward IMF conditions and high solar wind dynamic pressure revealed an approximately equal probability for anti-parallel and component reconnection between the interplanetary magnetic field (IMF) and the geomagnetic field. Using data from the Torodial Imaging Mass Angle Spectrograph (TIMAS) on the Polar spacecraft we have increased our survey over the entire cusp data base, selecting events with northward IMF but no restrictions on the solar wind dynamic pressure. The distance to the reconnection line are calculated by using the proven method of 3D cuts of the proton distribution function in the cusp to identify the low energy cut-off of precipitating ions. Anti-parallel or component reconnection is identified by tracing the distance to the reconnection line along the geomagnetic field line to the reconnection site.

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