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Published on: February 12, 2013
Plasma observations at venus with galileo.
Summary
Galileo spacecraft data revealed low electron heating (=20%) at Venus's bow shock. Solar wind densities and speeds were measured, with limited detection of pickup ions from Venus's corona.
Area of Science:
- Planetary Science
- Space Physics
- Plasma Physics
Background:
- Galileo spacecraft provided in-situ plasma measurements near Venus on February 10, 1990.
- The study focused on the Venusian bow shock and upstream solar wind environment.
- Instrument limitations (sunshade) affected ion observations in the magnetosheath.
Purpose of the Study:
- To analyze plasma conditions in the vicinity of Venus, including the bow shock and solar wind.
- To determine solar wind densities and bulk speeds using electron velocity distributions.
- To investigate the presence and density of pickup ions originating from Venus's planetary coronas.
Main Methods:
- Utilized plasma measurements from the Galileo spacecraft.
- Analyzed electron velocity distributions to derive solar wind parameters.
- Detected ions streaming from the bow shock and searched for pickup ions.
Main Results:
- Observed multiple crossings of the Venusian bow shock in the dawn sector.
- Determined solar wind densities and bulk speeds from electron data.
- Measured electron heating at the bow shock as less than or equal to 20%.
- Observed significant density increases (2-3x) at the dayside of the shock.
- Established an upper limit for pickup ion densities (10^-3 ion/cm^3).
Conclusions:
- Electron heating at the Venusian bow shock is minimal.
- Observed plasma density enhancements are consistent with bow shock dynamics.
- The upper limit for pickup ions aligns with theoretical models of Venus's neutral gas density.
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