Interaction of the Solar Wind with Magnetized Asteroids

نویسندگان

  • X. Blanco-Cano
  • N. Omidi
  • C. T. Russell
چکیده

RESUME We use a 2-D hybrid code (fluid electrons, particle ions) to simulate the interaction of the solar wind with a magnetized asteroid. The asteroid field is taken as a dipole with different strengths. For a small magnetic moment a whistler wake is generated. Stronger dipoles generate a magnetosonic perturbation. We compare simulation results with the signatures observed by Galileo near Gaspra and Ida. When the IMF is 90° to the solar wind flow, the wake is downstream from the asteroid, and is formed by whistler and magnetosonic waves. When the IMF is ≈45° to the flow, part of the wake is upstream. From the discrepancies found between observations and simulations we conclude that signatures near Gaspra and Ida were not generated by the solar wind interaction with magnetized asteroids.

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تاریخ انتشار 2003