On August 27, 1998 we observed auroral E-region irregularities using the Ma
nastash Ridge Radar system. These are the first radio science results from
passive radar observations of commercial FM broadcasts near 100 MHz. These
are also the first reported observations of 1.5 m irregularities in 15 year
s. The data show scatter most consistent with type-1 and type-3 ion-acousti
c turbulence as observed by 50 MHz and 140 MHz radars. The instrument is ex
traordinarily low in cost and provides data free of range and doppler veloc
ity aliasing problems. The range and velocity resolution achieved by this r
adar is substantially superior to that of other comparable coherent scatter
radars, and the time resolution is similar.