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Thus, a better understanding of the aforementioned processes in the upper ocean requires accurate numerical predictions and careful measurements of turbulent mixing, especially in the presence of substantial wave-induced motions. High-quality turbulence measurements in the surface layer have been made by ...
weak upwelling vs strong upwelling) that influences their tolerance and responses to climate change27. The coastal area of Central Chile (~ 33°S) is characterized by seasonal, wind-driven upwelling that brings cold nutrient-rich waters to the surface in austral spring and early...
ocean waves are tsunamis from e.g. earthquakes and landslides. Because ocean waves can travel far and can contain high energy it is important to measure ocean waves to understand their impact on shipping fishing, tourism, constructions, shorelines, water mixing, sediment resuspension, gas exchange...
wind forcing, surface currents, Ekman pumping, and vertical mixing). The oligotrophic waters of the North Pacific and North Atlantic gyres are observed to be expanding over this period, while those of the South Pacific, South Atlantic, and South Indian Ocean gyres show much weaker and less ...
wave-induced turbulence[1] Field observations of water temperature on the Australian North-West Shelf (Eastern Indian Ocean) with the support of numerical simulations are used to demonstrate that the injection of turbulence generated by the wave orbital motion substantially contributes to the mixing of...
This ???Surface Wave Mixing??? (SWM) is represented by a novel parameterization, in which the wave orbital motion contributes directly to the production of turbulent kinetic energy. The parameterization is implemented here as a modification to the k??? turbulence scheme, used within an ocean mo...
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