New techniques are applied to measured Doppler velocity and angle of a
rrival to estimate horizontal wind vectors, variances; and momentum fl
uxes, from MF radar data. The approach used to estimate mean winds was
first introduced as ''time domain interferometry'' (TDI) by Vandepeer
and Reid [1995]. In the present paper, the algorithm is refined and u
sed with data from the Urbana MF radar, which employs a single vertica
l antenna beam, to obtain a monthly mean wind climatology which is com
pared with the results from conventional spaced antenna full correlati
on analysis. The comparison validates the scattering model used in the
development of the TDI technique and highlights instrumental and proc
essing biases that differ between the two techniques. An extension of
the TDI method that can provide estimates of the Reynolds stress tenso
r associated with propagating gravity waves is also proposed, and some
preliminary results are presented.