Vertical mixing caused by breaking of internal tides plays a major role in maintaining the deep-ocean stratification. This study compares observations of dissipation from microstructure measurements to calculations of the vertical energy flux from barotropic to internal tides. taking into account the temporal variation due to the spring-neap tidal cycle. The dissipation data originate... https://countryscenesaddleryandpetsuppliers.shop/product-category/hidez-hoods/