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AGU: Geophysical Research Letters

 

Keywords

  • Mercury
  • exosphere
  • magnetosphere

Index Terms

  • Magnetospheric Physics: Planetary magnetospheres
  • Planetary Sciences: Solar System Objects: Mercury
  • Atmospheric Composition and Structure: Exosphere
  • Magnetospheric Physics: Numerical modeling
  • Magnetospheric Physics: Solar wind/magnetosphere interactions

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 36, L04106, 5 PP., 2009
doi:10.1029/2008GL036207

Sodium-ion pickup observed above the magnetopause during MESSENGER's first Mercury flyby: Constraints on neutral exospheric models

Menelaos Sarantos

Heliophysics Science Division, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

James A. Slavin

Heliophysics Science Division, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

Mehdi Benna

Solar System Exploration Division, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

Scott A. Boardsen

Heliophysics Science Division, NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

Goddard Earth Sciences and Technology Center, University of Maryland, Baltimore County, Baltimore, Maryland, USA

Rosemary M. Killen

Department of Astronomy, University of Maryland, College Park, Maryland, USA

David Schriver

Institute of Geophysics and Planetary Physics, University of California, Los Angeles, California, USA

Pavel Trávníček

Institute of Geophysics and Planetary Physics, University of California, Los Angeles, California, USA

Single-particle tracings of sodium pickup ions launched upstream of Mercury's magnetopause are used to investigate the access of these ions to the magnetosphere and set limits on the distribution of neutral sodium about the planet during the first MESSENGER flyby. The transport of pickup ions is modeled using flow velocity and magnetic fields from a three-dimensional magnetohydrodynamic simulation. Extensive penetration of pickup ions into the magnetosphere is found in the post-noon and dusk local time sectors due to the northward interplanetary magnetic field at the time of MESSENGER's first flyby. It is concluded that: (1) pickup of magnetosheath photoions may be an important source of hot planetary ions within the magnetosphere; and (2) the sodium ions in the magnetosheath observed by MESSENGER must originate from an extended neutral exosphere due to ion sputtering and/or to a partially escaping distribution generated by photon-stimulated desorption with yields modified by regolith trapping.

Received 2 October 2008; accepted 21 January 2009; published 25 February 2009.

Citation: Sarantos, M., J. A. Slavin, M. Benna, S. A. Boardsen, R. M. Killen, D. Schriver, and P. Trávníček (2009), Sodium-ion pickup observed above the magnetopause during MESSENGER's first Mercury flyby: Constraints on neutral exospheric models, Geophys. Res. Lett., 36, L04106, doi:10.1029/2008GL036207.

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