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    The Description of Mixing in Stratified Layers without Shear in Large-Scale Ocean Models 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 011:;page 3032
    Author(s): Umlauf, Lars
    Publisher: American Meteorological Society
    Abstract: Large-scale geophysical flows often exhibit layers with negligible vertical shear and infinite gradient Richardson number Ri. It is well known that these layers may be regions of active mixing, even in the absence of local ...
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    Dynamics of Rotating Shallow Gravity Currents Passing through a Channel. Part II: Analysis 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 010:;page 2402
    Author(s): Umlauf, Lars; Arneborg, Lars
    Publisher: American Meteorological Society
    Abstract: The physics of frictional control for channelized rotating gravity currents are analyzed using an extensive dataset including hydrographic, current, and microstructure measurements from the western Baltic Sea. Rotational ...
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    Dynamics of Rotating Shallow Gravity Currents Passing through a Channel. Part I: Observation of Transverse Structure 

    Source: Journal of Physical Oceanography:;2009:;Volume( 039 ):;issue: 010:;page 2385
    Author(s): Umlauf, Lars; Arneborg, Lars
    Publisher: American Meteorological Society
    Abstract: A detailed dataset describing a quasi-stationary bottom gravity current, approximately 10 m thick and 10 km wide, passing through a channel-like constriction in the western Baltic Sea is presented. The data include full-depth, ...
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    Residual Transport of Suspended Material by Tidal Straining near Sloping Topography 

    Source: Journal of Physical Oceanography:;2016:;Volume( 046 ):;issue: 007:;page 2083
    Author(s): Schulz, Kirstin; Umlauf, Lars
    Publisher: American Meteorological Society
    Abstract: idal straining is known to have an important impact on the generation of residual currents and the transport of suspended material in estuaries and the coastal ocean. Essential for this process is an externally imposed ...
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    Diapycnal Transport and Mixing Efficiency in Stratified Boundary Layers near Sloping Topography 

    Source: Journal of Physical Oceanography:;2010:;Volume( 041 ):;issue: 002:;page 329
    Author(s): Umlauf, Lars; Burchard, Hans
    Publisher: American Meteorological Society
    Abstract: The interaction of shear, stratification, and turbulence in boundary layers on sloping topography is investigated with the help of an idealized theoretical model, assuming uniform bottom slope and homogeneity in the upslope ...
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    Frontal Instability and Energy Dissipation in a Submesoscale Upwelling Filament 

    Source: Journal of Physical Oceanography:;2020:;volume( 50 ):;issue: 007:;page 2017
    Author(s): Peng, Jen-Ping;Holtermann, Peter;Umlauf, Lars
    Publisher: American Meteorological Society
    Abstract: Based on high-resolution turbulence microstructure and near-surface velocity data, frontal instability and its relation to turbulence are investigated inside a transient upwelling filament in the Benguela upwelling system ...
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    Gravity Current Dynamics and Entrainment—A Process Study Based on Observations in the Arkona Basin 

    Source: Journal of Physical Oceanography:;2007:;Volume( 037 ):;issue: 008:;page 2094
    Author(s): Arneborg, Lars; Fiekas, Volker; Umlauf, Lars; Burchard, Hans
    Publisher: American Meteorological Society
    Abstract: A 19-h time series of dissipation, stratification, and horizontal velocities has been obtained for a dense gravity current flowing into the Arkona Basin in the western Baltic Sea. The observations are compared with ...
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    Energetics of Bottom Ekman Layers during Buoyancy Arrest 

    Source: Journal of Physical Oceanography:;2015:;Volume( 045 ):;issue: 012:;page 3099
    Author(s): Umlauf, Lars; Smyth, William D.; Moum, James N.
    Publisher: American Meteorological Society
    Abstract: urbulent bottom Ekman layers are among the most important energy conversion sites in the ocean. Their energetics are notoriously complex, in particular near sloping topography, where the feedback between cross-slope Ekman ...
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    Lateral Circulation Generates Flood Tide Stratification and Estuarine Exchange Flow in a Curved Tidal Inlet 

    Source: Journal of Physical Oceanography:;2014:;Volume( 045 ):;issue: 003:;page 638
    Author(s): Becherer, Johannes; Stacey, Mark T.; Umlauf, Lars; Burchard, Hans
    Publisher: American Meteorological Society
    Abstract: ross-channel transect measurements of microstructure and velocity in a well-mixed and curved tidal inlet in the German Wadden Sea show the occurrence of significant late flood stratification. This stratification is found ...
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    Entrainment in Shallow Rotating Gravity Currents: A Modeling Study 

    Source: Journal of Physical Oceanography:;2010:;Volume( 040 ):;issue: 008:;page 1819
    Author(s): Umlauf, Lars; Arneborg, Lars; Hofmeister, Richard; Burchard, Hans
    Publisher: American Meteorological Society
    Abstract: The physics of shallow gravity currents passing through a rotating channel at subcritical Froude number is investigated here with a series of idealized numerical experiments. It is found that the combined effects of friction ...
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