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2-0.5 m s-1. Disturbances were mostly excited on the downslope side of the array where the internal waves from the Pacific Ocean broke initially and the turbulence oscillated between less then 1 km small-scale ridges. Such small-scale topography caused varying turbulence-induced signals due to localized waves breaking. Arrayed OBSs can provide complementary observations to characterize deep-sea turbulence.Cleft palate repair is a challenging procedure for cleft surgeons to teach, and in research, it can be difficult to evaluate differen
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