The underwater environment can be considered a system with time-varying impulse response, causing time-dependent spectral changes to a transmitted acoustic signal. This is the result of the interaction of the signal with the water column and ocean boundaries or the presence of fast moving object scatterers in the ocean. In underwater acoustic communications using mediumto-high frequencies (0.3-20 kHz), the nonstationary transformation on the transmitted signals can be modeled as multiple timedelay and Doppler-scaling paths. When estimating the channel, a higher processing performance is thus expected if the techniques used employ a matched channel model compared to those that only compensate for wideband effects. Following a matched linear time-varying wideband system representation, we propose two different methods for estimating the underwater acoustic communication environment. The first method follows a canonical timescale channel model and is based on estimating the coefficients of the discrete wideband spreading function. The second method follows a ray system model and is based on extracting timescale features for different ray paths using the matching pursuit decomposition algorithm. Both methods are validated and compared using communication data from actual underwater acoustic communication experiments. spreading function can provide a means for improving communication receiver performance [11, 12]. Characterizing acoustic signal propagation through water is essential for many applications, including underwater acoustic communications, active and passive sonar, underwater navigation and tracking, and ocean acoustic tomography. The highly time-varying nature of the underwater environment can cause many undesirable distortions to the propagating signal. Time-varying multipath distortions may be the result of dense reflections from rough surfaces, fluctuations in sound speed due to inhomogeneous mediums, relative motion between transmitters and receivers, or changes in the propagating medium [13]. Depending on the transmission frequency and ocean depth, the time-dependent spectral changes in the signal can be Doppler scaling (compression or expansion) or dispersive (nonlinear) transformations [3, 6, 14]. In particular, medium-to-high frequency (0.3-20 kHz) underwater acoustic signals are characterized by spreading caused by multiple time-delay paths and multiple Doppler-scaling