Internal wave measurements on the Cycladic Plateau of the Aegean Sea

The internal wave climate in the southern Aegean Sea is examined with an array of two bottom‐mounted acoustic Doppler current profilers and three profiling moorings deployed on the northern continental slope of the Cretan Sea for 3 months. Frequency spectra indicate an extremely weak internal wave continuum, about 4–10 times weaker than the Garrett‐Munk and Levine reference levels. Spectra are instead dominated by semidiurnal internal tides and near‐inertial waves, which are examined in detail by bandpass filtering. In the semidiurnal band, a barotropic tidal flow of ≈2 cm s−1is observed, with a pronounced spring/neap modulation in phase with the lunar fortnightly cycle. One to two days following several of these spring tide periods, a distinct internal tide featuring 10–20 m vertical displacements and 15–20 cm s−1baroclinic velocities is detectable propagating upward and to the southeast. Time‐mean energy increases a factor of 2–5 within about 100 m from the bottom, implying generation and/or scattering from the bottom, whose slope is nearly critical to semidiurnal internal waves over much of the array. Several strong, downward propagating near‐inertial events are also seen, each of which occurs following a period of work done by the wind on the mixed layer as estimated from a nearby surface mooring. The high‐frequency internal wave continuum is more temporally constant but increases substantially toward the end of the deployment. Significant but unexplained differences in kinetic energy occur between successive spring tide periods in the case of the internal tides and between successive wind events in the case of the near‐inertial signals. Substantial variability is observed in the low‐frequency flows, which likely contributes to the time variability of the internal wave signals. We measured internal waves in the Aegean with profiling mooringsInternal tides and near‐inertial waves were dominantTheir levels were quite variable, suggesting that mesoscale flows are important