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    Eulerian Volume Transport Induced by Spatially Damped Internal Equatorial Kelvin Waves 

    Source: Journal of Physical Oceanography:;2015:;Volume( 045 ):;issue: 007:;page 1794
    Author(s): Weber, Jan Erik H.
    Publisher: American Meteorological Society
    Abstract: he Eulerian volume transport in internal equatorial Kelvin waves subject to viscous attenuation is investigated theoretically by integrating the horizontal momentum equations in the vertical. In terms of small perturbations, ...
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    Ekman Currents and Mixing due to Surface Gravity Waves 

    Source: Journal of Physical Oceanography:;1981:;Volume( 011 ):;issue: 010:;page 1431
    Author(s): Weber, Jan Erik
    Publisher: American Meteorological Society
    Abstract: The steady Ekman boundary-layer current is studied theoretically for the case when the eddy viscosity is proportional to the shear of the wave orbital velocity in a turbulent wave, times the square of a mixing length ...
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    Wave Attenuation and Wave Drift in the Marginal Ice Zone 

    Source: Journal of Physical Oceanography:;1987:;Volume( 017 ):;issue: 012:;page 2351
    Author(s): Weber, Jan Erik
    Publisher: American Meteorological Society
    Abstract: 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 formulation, and the brash is ...
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    Wave-Induced Mass Transport in the Oceanic Surface Layer 

    Source: Journal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 012:;page 2527
    Author(s): Weber, Jan Erik
    Publisher: American Meteorological Society
    Abstract: The mean mass transport induced by surface gravity waves is investigated theoretically for a deep, rotating ocean with a constant eddy viscosity. The waves are periodic in time and have amplitudes that grow or decay slowly ...
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    Friction-Induced Roll Motion in Short-Crested Surface Gravity Waves 

    Source: Journal of Physical Oceanography:;1985:;Volume( 015 ):;issue: 007:;page 936
    Author(s): Weber, Jan Erik
    Publisher: American Meteorological Society
    Abstract: Induced streaming due to deep water surface gravity waves propagating at oblique angles to each other is studied theoretically on the basis of a Lagrangian description. The ocean is slightly viscous, and the primary waves ...
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    Steady Wind- and Wave-Induced Currents in the Open Ocean 

    Source: Journal of Physical Oceanography:;1983:;Volume( 013 ):;issue: 003:;page 524
    Author(s): Weber, Jan Erik
    Publisher: American Meteorological Society
    Abstract: Steady wind-drift currents in a deep viscous rotating ocean are studied theoretically. The analysis is based on the Lagrangian description of motion. A mean wind-stress at the surface yields the traditional Ekman current. ...
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    Transient Ocean Currents Induced by Wind and Growing Waves 

    Source: Journal of Physical Oceanography:;1993:;Volume( 023 ):;issue: 002:;page 193
    Author(s): Weber, Jan Erik; Melsom, Arne
    Publisher: American Meteorological Society
    Abstract: A theoretical nonlinear model for wind- and wave-induced currents in a viscous, rotating ocean is developed. The analysis is based on a Lagrangian description of motion. The nonlinear drift problem is formulated such that ...
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    Mass Transport Velocity in Free Barotropic Poincaré Waves 

    Source: Journal of Physical Oceanography:;2003:;Volume( 033 ):;issue: 009:;page 2000
    Author(s): Høydalsvik, Frode; Weber, Jan Erik
    Publisher: American Meteorological Society
    Abstract: The mass transport velocity induced by long surface waves in a shallow, rotating viscous ocean is studied theoretically by using a Lagrangian description of motion. The depth is constant, and the water is homogeneous. Such ...
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    Effect of an Insoluble Surface Film on the Drift Velocity of Capillary–Gravity Waves 

    Source: Journal of Physical Oceanography:;1989:;Volume( 019 ):;issue: 007:;page 952
    Author(s): Weber, Jan Erik; Førland, Even
    Publisher: American Meteorological Society
    Abstract: 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 description of motion. ...
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    Mass Transport in the Stokes Edge Wave for Constant Arbitrary Bottom Slope in a Rotating Ocean 

    Source: Journal of Physical Oceanography:;2014:;Volume( 044 ):;issue: 004:;page 1161
    Author(s): Ghaffari, Peygham; Weber, Jan Erik H.
    Publisher: American Meteorological Society
    Abstract: he Lagrangian mass transport in the Stokes surface edge wave is obtained from the vertically integrated equations of momentum and mass in a viscous rotating ocean, correct to the second order in wave steepness. The analysis ...
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