Ionospherically reflected echoes are received with a four-element mult
iplexed interferometer array and two phase-matched receivers in implem
entations of the National Oceanic and Atmospheric Administration dynas
onde. From these data, six phase parameters (Phi(0), Phi(x), Phi(y), P
hi(t), Phi(p) and Phi(f)) are obtained and used to derive echo locatio
n, Doppler velocity, wave polarization, and virtual range. Since 2 pi
aliasing is an inherent feature of interferometric spaced antenna phas
e measurements, the phase parameters cannot be derived directly from t
he measured phase values using the method of least squares. in this wo
rk, we introduce a general procedure for the derivation of these param
eters that (1) employs a ''zero-freedom'' technique to derive initial
estimates of the phase parameters, (2) derives shifted values of the m
easured phases from the six estimates, and (3) uses the method of leas
t squares in conjunction with the shifted phases to improve the phase
parameter estimates. This procedure minimizes the phase ambiguity inhe
rent in interferometric phase measurements and derives phase parameter
s that approach the ideal least squares result. Furthermore, the ionos
pheric echo ''quality'' is quantified by two error parameters, defined
as (s) over cap, the least squares of the measured phase errors, and
EP, the RMS phase error. It is also shown that the value of (s) over c
ap relative to the square of the standard deviation of measured phase
is equal to the number of degrees of freedom in the phase parameters.
Applying these techniques to data acquired with the Utah State Univers
ity dynasonde, we derive a standard deviation of <2 degrees in the mea
sured echo phase.