The standard technique for computing ocean wave - radar modulation tra
nsfer functions (MTFs) depends on nonparametric fast Fourier transform
(FFT) methods. In this paper we suggest a new approach applying an au
toregressive (AR) parametric spectral estimator. The analysis shows th
at the two-channel autoregressive model produces smooth estimates of t
he MTF and permits better frequency resolution than FFT techniques. Th
e feed-across effect inherent in the methods developed to evaluate the
multichannel AR coefficients causes a negligible effect on MTF. The A
R-based MTF depends weakly on the record length; for steady meteorolog
ical conditions the AR model of the MTF for a 2-min data run is compar
able with ones calculated using 10 min or more of data. In the same si
tuation the FFT technique is unreliable for records of less than 10 mi
n. The appropriate order of the multichannel AR model can vary without
causing significant change in the MTF. In most cases any order betwee
n 8 and 16, depending on radar system parameters and meteorological co
nditions, will give acceptable results.