3.8 Article Book Chapter

Birth of a Magnetosphere

期刊

MAGNETOSPHERES IN THE SOLAR SYSTEM
卷 259, 期 -, 页码 427-439

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1002/9781119815624.ch27

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资金

  1. SNSA [95/15, 112/13, 108/12]
  2. VR [2015-04187]
  3. STFC of UK [ST/N000692/1]
  4. International Space Science Institute (ISSI) [2017-402]
  5. ESEP
  6. ANR [ANR-15-CE31-0009-01]
  7. CNRS
  8. Observatoire de Paris
  9. Universite Paul Sabatier, Toulouse
  10. Imperial College London - UK Science and Technology Facilities Council
  11. CNES
  12. Swedish Research Council [2015-04187] Funding Source: Swedish Research Council

向作者/读者索取更多资源

A magnetosphere can form around an object in a stellar wind either due to the intrinsic magnetic field of the object or stellar wind interaction with the ionosphere of the object. Through the study of the birth and evolution of a comet magnetosphere as the comet nucleus approached the Sun, we gain insights into the characteristics of comet magnetospheres and the changes in solar wind-atmosphere interaction.
A magnetosphere may form around an object in a stellar wind either due to the intrinsic magnetic field of the object or stellar wind interaction with the ionosphere of the object. Comets represent the most variable magnetospheres in our solar system, and through the Rosetta mission we have had the chance to study the birth and evolution of a comet magnetosphere as the comet nucleus approached the Sun. We review the birth of the comet magnetosphere as observed at comet 67P Churyumov-Gerasimenko, the formation of plasma boundaries and how the solar wind-atmosphere interaction changes character as the cometary gas cloud and magnetosphere grow in size. Mass loading of the solar wind leads to an asymmetric deflection of the solar wind for low outgassing rates. With increasing activity a solar wind ion cavity forms. Intermittent shock-like features were also observed. For intermediate outgassing rate a diamagnetic cavity is formed inside the solar wind ion cavity, thus well separated from the solar wind. The cometary plasma was typically very structured and variable. The region of the coma dense enough to have significant collisions forms a special region with different ion chemistry and plasma dynamics as compared to the outer collision-free region.

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