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Volume 50 Supplement 3

Special Issue: The PLANET-B Misson and Related Science

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Low Frequency plasma wave Analyzer (LFA) onboard the PLANET-B spacecraft

Abstract

The Low Frequency plasma wave Analyzer, LFA, on board the PLANET-B spacecraft has been developed to measure the Martian plasma waves. Two orthogonal electric dipole wire antennas, 50 m tip-to-tip, in the spacecraft spin plane are used to measure plasma waves, dc electric fields, and the spacecraft potential relative to the ambient plasma. The LFA has capability to measure the wave spectrum in the band from 10 Hz to 32 kHz, and to capture the signal waveform in the band from dc to 32 kHz by using a 4 MByte memory. The LFA scientific objectives are to explore the following: (1) Macroscopic plasma environment and boundaries from the solar wind to the ionosphere, (2) Microscopic plasma phenomena induced by the interaction between the solar wind and the Martian atmosphere and the moon Phobos, (3) Generation and propagation of electromagnetic waves, (4) Plasma densities and waves in the nightside ionosphere and tail, and (5) Comparison of Martian plasma waves with those of other planets such as non-magnetized Venus and magnetized Earth.

References

  • Crawford, G. K. et al., VLF imaging of the Venus foreshock, Geophys. Res. Lett., 20, 2801–2804, 1993.

    Article  Google Scholar 

  • Dubinin, E. et al., Comparison of observed plasma and magnetic field structures in the wakes of Mars and Venus, J. Geophys. Res., 96, 11189–11197, 1991.

    Article  Google Scholar 

  • Grard, R. et al., First measurements of plasma waves near Mars, Nature, 341, 607–609, 1989.

    Article  Google Scholar 

  • Grard, R. et al., Plasma and waves around Mars, Planet. Space Sci., 39, 89–98, 1991.

    Article  Google Scholar 

  • Grebowsky, J. M. et al., Venus nighttime ionospheric holes: the signatures of parallel electric field acceleration regions?, Geophys. Res. Lett., 8, 1273–1276, 1981.

    Article  Google Scholar 

  • Greenstadt, E. W. et al., Spatial distribution of electron plasma oscillations in the Earth’s foreshock at ISEE 3, J. Geophys. Res., 100, 19933–19939, 1995.

    Article  Google Scholar 

  • Gurnett, D. A., The polar plasma wave instrument, Space Sci. Rev., 71, 597–22, 1995.

    Article  Google Scholar 

  • Huba, J. D., Generation of waves in the Venus mantle by the ion acoustic beam instability, Geophys. Res. Lett., 20, 1751–1754, 1993.

    Article  Google Scholar 

  • Johnson, F. S. et al., Viking 1 electron observations at Mars, J. Geophys. Res., 96, 11097–11118, 1991.

    Article  Google Scholar 

  • Kasaba et al., GEOTAIL observation of 2fp emission around the terrestrial electron foreshock, Adv. Space Res., 20, 699–702, 1997.

    Article  Google Scholar 

  • Krymskii, A. M. et al., The electromagnetic effects of the solar wind interaction with the Phobos neutral gas halo and dust torus, Planet. Space Sci., 40, 1033–1041, 1992.

    Article  Google Scholar 

  • Lundin, R. et al., ASPERA/PHOBOS measurements of the ion outflow from the Martian ionosphere, Geophys. Res. Lett., 17, 873–876, 1990.

    Article  Google Scholar 

  • Matsumoto, H. et al., Plasma wave observations with GEOTAIL spacecraft, J. Geomag. Geoelectr., 46, 59–95, 1994.

    Article  Google Scholar 

  • Moses, S. L. et al., Characteristics of spectra from the Martian bow shock and comparison with Venus, Earth, AMPTE, Jupiter, and Saturn, J. Geophys. Res., 96, 11221–11226, 1991.

    Article  Google Scholar 

  • Nairn, C. M. C. et al., Plasma wave observations in the night sector of Mars, J. Geophys. Res., 96, 11227–11233, 1991.

    Article  Google Scholar 

  • Pedersen, A. et al., Deviation of electron densities from differential potential measurements upstream and down stream of the bow shock and in the magnetosphere of Mars, J. Geophys. Res., 96, 11243–11252, 1991.

    Article  Google Scholar 

  • Sagdeev, R. Z. et al., Wave activity in the neighborhood of the bow shock of Mars, Geophys. Res. Lett., 17, 893–896, 1990.

    Article  Google Scholar 

  • Scarf, F. L. et al., Pioneer Venus plasma wave observations: The solar wind-Venus interaction, J. Geophys. Res., 85, 7599–7612, 1980.

    Article  Google Scholar 

  • Showstack, R., Mars has crustal, complex magnetic field, EOS, 78, 40, 429, 1997.

    Article  Google Scholar 

  • Slavin, J. A. et al., The solar wind interaction with Mars: Mariner 4, Mars2, Mars3, Mars5, and Phobos 2 observations of bow shock position and shape, J. Geophys. Res., 96, 11235–11241, 1991.

    Article  Google Scholar 

  • Strangeway, R. J., Plasma waves at Venus, Space Sci. Rev., 55, 275–316, 1991.

    Article  Google Scholar 

  • Szegö, K. et al., Electron acceleration above the dayside ionopause of non magnetized bodies, Pros. 4th COSPER Colloquium, edited by T. I. Gombosi, pp. 247–252, Pergamon Press, 1986.

  • Taylor, H. A. et al., Venus nightside ionospheric troughs: Implications for evidence of lightning and volcanism, J. Geophys. Res., 90, 7415–7426, 1985.

    Article  Google Scholar 

  • Trotignon, G. et al., Plasma wave system measurements of the Martian bow shock from the Phobos 2 spacecraft, J. Geophys. Res., 96, 11253–11264, 1991.

    Article  Google Scholar 

  • Woo, R. and A. J. Kilore, Magnetization of the ionospheres of Venus and Mars: results from radio occultation measurements, J. Geophys. Res., 96, 11073–11081, 1991.

    Article  Google Scholar 

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Matsumoto, H., Okada, T., Hashimoto, K. et al. Low Frequency plasma wave Analyzer (LFA) onboard the PLANET-B spacecraft. Earth Planet Sp 50, 223–228 (1998). https://doi.org/10.1186/BF03352107

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  • DOI: https://doi.org/10.1186/BF03352107

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