Neutral Hydrogen Density Profiles Derived from Geocoronal Imaging Ostgaard, N., S. B. Mende, H. U. Frey, G. R. Gladstone, The geocorona is produced when solar Ly-a radiation is resonance scattered by neutral hydrogen in the exosphere and measurements of the geocoronal intensity from space can therefore be used to derive the density profile of neutral hydrogen surrounding the Earth. The Geocorononal Imager (GEO) instrument, which is part of the FUV imaging system onboard the IMAGE satellite, is designed to measure the geocoronal Ly-a emissions. Three imagers, HENA, MENA and LENA onboard the IMAGE satellite are imaging the energetic neutral atoms (ENA). ENA are produced by charge exchange between energetic magnetospheric ions and the cold neutral hydrogen background. In order to convert the measurements of ENA to magnetospheric ion distribution, information about the instantaneous neutral hydrogen density distribution is needed. In this paper we present how we can develop an inversion scheme using the GEO data of Ly-a column density to obtain the radial density profile of the neutral hydrogen in the magnetosphere. _______________ To be presented at the Magnetospheric Imaging Workshop, Yosemite National Park, California, U.S.A., Feb. 5-8, 2002.