This paper presents laboratory and field testing of a pulse-to-purse cohere
nt acoustic Doppler profiler for the measurement of turbulence in the ocean
. In the laboratory, velocities and wavenumber spectra collected From Doppl
er and digital particle image velocimeter measurements compare very well. T
urbulent velocities are obtained by identifying and filtering out deep wate
r gravity waves in Fourier space and inverting the result. Spectra of the v
elocity profiles then reveal the presence of an inertial subrange in the tu
rbulence generated by unsteady breaking waves. In the field, comparison of
the profiler velocity records with a single-point current measurement is sa
tisfactory. Again wavenumber spectra are directly measured and exhibit an a
pproximate -5/3 slope. It is concluded that the instrument is capable of di
rectly resolving the wavenumber spectral levels in the inertial subrange un
der breaking waves, and therefore is capable of measuring dissipation and o
ther turbulence parameters in the upper mixed layer or surface-wave zone.