Theoretical studies have shown the potential scientific value of multi-spac
ecraft: radio tomographic imaging of the magnetosphere. The < 10 R-E WIND p
erigee passes during August 2000 afforded a unique opportunity to test and
verify the capabilities of radio tomography by measuring interspacecraft el
ectromagnetic wave propagation parameters using the Radio Plasma Imager (RP
I) on IMAGE as the transmitter and the WAVES instrument on WIND as the rece
iver. The primary goal of this experiment was to measure Faraday rotation v
ariations in the RPI signal and interpret them in terms of the path-integra
ted magnetic field and electron density. A special 6 W linearly-polarized 8
28 kHz RPI signal was clearly detected by WAVES more than 6 R-E away and sh
owed a distinct signature of time-varying Faraday rotation. We show how cha
nges in the path-integrated electron density/magnetic field product can be
unambiguously measured from this continuous, low signal to noise ratio, sin
gle frequency measurement.