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- W2175364896 abstract "While the boundary between the ocean and the atmosphere has been extensively studied it is still not well understood. Heat, mass and momentum cross this boundary at a rate determined by many features of not only the sea surface motion but also the properties of the atmosphere and the ocean boundary layers on each side of the interface. There are some simplifications that can be made because the sharp variations are predominantly in the vertical, but there is a hierarchy of scales and processes at play which cannot be ignored in many applications. Central to understanding the processes at the boundary is gaining knowledge about the flux of momentum between the water and the air. The flux, which is the rate of transport of momentum across unit area, can be in either direction. In a frame of reference fixed to the earth, flux is mostly from the wind to the ocean currents, but less frequently, the flux is from the wind-waves or currents to the atmosphere." @default.
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- W2175364896 date "2001-09-24" @default.
- W2175364896 modified "2023-09-26" @default.
- W2175364896 title "Overview" @default.
- W2175364896 doi "https://doi.org/10.1017/cbo9780511552076.002" @default.
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