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global model of ocean tides.
The new Goce model of ocean circulation has been checked and integrated with the point measurements from drifting buoys.
A methodology is described for control of vertically profiling floats that uses an imperfect predictive model of ocean currents.
This control authority is combined with an imperfect model of ocean currents to attempt to force the floats to maintain position.
Jorge Sarmiento, a biogeochemist at Princeton University, and three colleagues coupled a sophisticated computer model of ocean currents to two simple biological models of proxies of phytoplankton and fish abundance.
Third are presented results from an April 2015 deployment in the Pacific Ocean that show that even with an imperfect model of ocean currents, model-based control can enhance float control performance.
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Such an increased flow of fresh water from Greenland could, according to the best available models of ocean circulation, change the way that currents flow in the North Atlantic, to the detriment of the Gulf Stream, the current that keeps north-west Europe warmer than its latitude suggests it should be.
Therefore, an advanced modeling of ocean parameters helps towards improving ocean and coastal engineering practices.
Numerical models of ocean circulation admit motions varying on a wide range of time scales.
This paper describes a numerical method with two time levels for solving partial differential equations that represent layered models of ocean circulation.
The motions seen in numerical models of ocean circulation typically include rapidly moving external gravity waves, which are essentially two-dimensional, and a variety of other motions which are much slower and generally three-dimensional.
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