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A raft drifting on the ocean is at the mercy of the elements. When a sailor describes this experience, one begins to understand the meaning of "in situ," of being in touch with the water. The senses f...
Analysis of The Surface Drift Currents in the Bothnian Sea.
It is generally known that surface currents off Oregon flow equatorward in summer when winds are from the northwest and poleward in the winter when winds are from the south. A detailed pattern of surf...
The drift responses of monomolecular slicks to wind and wave action have been investigated in a laboratory wind-wave tunnel and in the field. The wind-wave tunnel was fitted with a mechanical wave gen...
A study has been carried out of the surface drift on open water due to the combined action of currents, winds and wind-generated waves for cocurrent and countercurrent air flow. It has been shown theo...
Drifting buoys and dynamic topography over the continental shelf in the northern Gulf of Alaska are used to describe the coastal circulation and flow in the offshelf Alaska Current. One permanent anti...
Smoothed records of ice drift, surface wind and upper ocean currents at four manned stations of the 1975–76 AIDJEX experiment in the central Arctic have been analyzed to provide a statistical relation...
Wind-induced shell currents and wave-induced mass transports at various fetches of both clean and slick sea surfaces are separately estimated. At the clean surface, the ratio between wind-induced curr...
Surface gravity waves in a viscous rotating ocean are studied theoretically when they penetrate an area covered by highly concentrated brashlike ice. The motion is described by a Lagrangian formulatio...
The drift velocity due to capillary-gravity waves in a deep ocean is investigated theoretically. The surface is covered by an insoluble, inextensible film, and the analysis is based an a Lagrangian de...
The paper proposes a theory of the stationary turbulent drift friction layer that, under the conditions of stable stratification, can appear as the upper mixed layer (UML) of the ocean or as one mixed...
Wind waves are commonly ignored when modeling the ice motion in the marginal ice zone. In order to estimate the importance of the wave forcing, an expression for the second-order wave-induced drift fo...
The migration of nonlinear frontal jets is examined using an inviscid “reduced gravity” model. Two cases are considered in detail. The first involves the drift of deep jets situated above a sloping bo...
A global version of the GFDL modular ocean model is forced using conventional restoring boundary conditions (BCs), mixed BCs (i.e., restoring the upper-level temperature but specifying a fixed salt fl...
A model was constructed to estimate ice floe trajectories. The model considers the balance of atmosphere and ocean drag forces on ice floes, including skin and body drag forces from wind, waves, and c...

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