Magnetospheric Electron-Density Values Determined from Plasma Resonances Stimulated by the Radio Plasma Imager on the IMAGE Satellite R F Benson, Goddard Space Flight Center, Greenbelt, MD 20771, 301-286-4037, u2rfb@lepvax.gsfc.nasa.gov J F Fainberg, Goddard Space Flight Center, Greenbelt, MD 20771, 301-286-6940 V A Osherovich, RITSS/Goddard Space Flight Center, Greenbelt, MD 20771, 301-286-3649 J L Green, Goddard Space Flight Center, Greenbelt, MD 20771, 301-286-7354 S F Fung Goddard Space Flight Center, Greenbelt, MD 20771, 301-286-6301 B W Reinisch, University of Massachusetts Lowell, Lowell, MA 01854, 978-934-4903 The Radio Plasma Imager (RPI) on the Imager for Magnetopause-to-Aurora Global Exploration (IMAGE) satellite was designed for long-distance magnetospheric radio sounding. The RPI also stimulates local plasma resonances that can be used to accurately deduce both the ambient electron density and the magnetic field strength even in very tenuous plasmas where the former is difficult to measure. The information provided by these resonances is beneficial to the process of inversion of the magnetospheric reflection traces into electron-density profiles. When RPI is programmed to transmit short (3.2 ms) pulses, with a linear stepping size between frequency transmissions comparable to the RPI receiver bandwidth of 300 Hz over a limited portion of the sweep range, the plasma resonances at the harmonics of the electron cyclotron frequency fce are clearly identified. These resonances have been stimulated before by magnetospheric radio sounders but never at such great distances at high latitudes. Even at the high-latitude IMAGE apogee radial distance of 8 RE, resonances up to 18 fce are observed and the time duration of the lower harmonics can exceed 100 ms. Plasma resonances at the electron plasma frequency fpe and the upper-hybrid frequency fuh, where fuh2 = fpe2 + fce2 are also stimulated by RPI. These resonances have been used to identify the ambient electron density and the magnetic field strength along the IMAGE orbit and the results, and comparisons to existing models, will be presented. _______________ Presented at the Fall American Geophysical Union Meeting, San Francisco, CA., December 15-19, 2000