Experimental data on the plasma envelopes of Mars, Venus, and Halley's and Giacobini-Zinner's comets: comparison of loading effects.

Mathematics – Logic

Scientific paper

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Cometary Plasma

Scientific paper

Results of research on the interaction of the solar wind with gaseous obstacles, which are the atmospheres of planets and comets, are described from a unique point of view. It is shown that with such interaction there results a specific plasma formation - a mantle, the boundary between which and the solar wind is distinctly marked. Possible physical mechanisms leading to the formation of an abrupt boundary between a mantle and the external flux are discussed. The mantle formed on the day side is topologically connected to the plasma tail.

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