A passive source ranging method based on the frequency warping transform of the vertical intensity flux in shallow water
Qi Yu-Bo1, †, Zhou Shi-Hong1, Yu Meng-Xiao1, Du Shu-Yuan1, Sun Mei2, Zhang Ren-He1
       

The received signals and their time–frequency representations. (a) Normalized waveform of the received pressure, (b) normalized waveform of the received vertical velocity, (c) spectrogram of the received pressure, and (d) spectrogram of the received vertical velocity. In every subfigure, the mode numbers are labeled in white. The spectrogram color scale is linear and arbitrary.