Other
Scientific paper
May 1990
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990sci...248..835p&link_type=abstract
Science (ISSN 0036-8075), vol. 248, May 18, 1990, p. 835-838. Research supported by NASA and U.S. National Research Council.
Other
83
D Lines, Emission Spectra, Mercury Atmosphere, Planetary Magnetospheres, Sodium Vapor, Deuterium, Monochromatic Radiation, Sputtering, Temporal Distribution, Mercury (Planet), Atmosphere, Sodium, Magnetosphere, Emissions, Latitude, Magnetic Effects, Distribution, Sputtering, Polar Regions, Transport, Vapor, Diurnal Variations, Magnetic Fields, Exosphere, Solar Effects, Earth-Based Observations, Techniques, Procedure, Ccd Methods
Scientific paper
Monochromatic images of Mercury at the sodium D2 emission line showed excess sodium emission in localized regions at high northern and southern latitudes and day-to-day global variations in the distribution of sodium emission. These phenomena support the suggestion that magnetospheric effects could be the cause. Sputtering of surface minerals could produce sodium vapor in polar regions during magnetic substorms, when magnetospheric ions directly impact the surface. Another important process may be the transport of sodium ions along magnetic field lines toward polar regions, where they impact directly on the surface of Mercury and are neutralized to regenerate neutral sodium atoms. Day-to-day variations in planetary sodium distributions could result from changing solar activity, which can change the magnetosphere in time scales of a few hours. Observations of the sodium exosphere may provide a tool for remote monitoring of the magnetosphere of Mercury.
Morgan Thomas H.
Potter Andrew E.
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