Open AccessDynamics of Rotating Shallow Gravity Currents Passing through a Channel. Part I: Observation of Transverse Structure
Author(s) -
Lars Umlauf,
Lars Arneborg
Publication year - 2009
Publication title -
journal of physical oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.706
H-Index - 143
eISSN - 1520-0485
pISSN - 0022-3670
DOI - 10.1175/2009jpo4159.1
Subject(s) - gravity current , geology , froude number , transverse plane , stratification (seeds) , turbulence , mechanics , internal wave , density contrast , entrainment (biomusicology) , geophysics , physics , flow (mathematics) , oceanography , structural engineering , astronomy , dormancy , engineering , biology , rhythm , acoustics , seed dormancy , germination , botany
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, synoptic, and highly resolved transects of stratification and turbulence parameters, as well as detailed velocity transects across the gravity current at different down-channel locations. The velocity data reveal a persistent transverse circulation, creating a characteristic wedge-shaped density structure in the interface. A strong asymmetry was also found in the interior of the gravity current, where the evolution of a dynamically significant transverse density gradient to the right of the down-channel flow was observed. Spectral analysis of the near-bottom velocities showed a surprisingly strong contribution to the bottom stress from low-frequency motions with periods up to 30 min that are possibly related to internal wave effects. Cross-channel transects of shear microstructure were used to investigate the transverse variation of local entrainment rates and bottom stresses. These data indicate that frictional control is essential for this class of gravity currents that are characterized by subcritical Froude numbers, small entrainment, strong rotational effects, and small thickness compared to the bottom Ekman layer.