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dc.contributor.authorKranenburg, Wouter M.  Concept link
dc.contributor.authorGeyer, W. Rockwell  Concept link
dc.contributor.authorGarcia, Adrian Mikhail P.  Concept link
dc.contributor.authorRalston, David K.  Concept link
dc.date.accessioned2019-07-23T20:49:46Z
dc.date.available2019-07-23T20:49:46Z
dc.date.issued2019-06-13
dc.identifier.citationKranenburg, W. M., Geyer, W. R., Garcia, A. M. P., & Ralston, D. K. (2019). Reversed lateral circulation in a sharp estuarine bend with weak stratification. Journal of Physical Oceanography, 49(6), 1619-1637.en_US
dc.identifier.urihttps://hdl.handle.net/1912/24364
dc.descriptionAuthor Posting. © American Meteorological Society, 2019. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 49(6), (2019):1619-1637, doi:10.1175/JPO-D-18-0175.1.en_US
dc.description.abstractAlthough the hydrodynamics of river meanders are well studied, the influence of curvature on flow in estuaries, with alternating tidal flow and varying water levels and salinity gradients, is less well understood. This paper describes a field study on curvature effects in a narrow salt-marsh creek with sharp bends. The key observations, obtained during times of negligible stratification, are 1) distinct differences between secondary flow during ebb and flood, with helical circulation as in rivers during ebb and a reversed circulation during flood, and 2) maximum (ebb and flood) streamwise velocities near the inside of the bend, unlike typical river bend flow. The streamwise velocity structure is explained by the lack of a distinct point bar and the relatively deep cross section in the estuary, which means that curvature-induced inward momentum redistribution is not overcome by outward redistribution by frictional and topographic effects. Through differential advection of the along-estuary salinity gradient, the laterally sheared streamwise velocity generates lateral salinity differences, with the saltiest water near the inside during flood. The resulting lateral baroclinic pressure gradient force enhances the standard helical circulation during ebb but counteracts it during flood. This first leads to a reversed secondary circulation during flood in the outer part of the cross section, which triggers a positive feedback mechanism by bringing slower-moving water from the outside inward along the surface. This leads to a reversal of the vertical shear in the streamwise flow, and therefore in the centrifugal force, which further enhances the reversed secondary circulation.en_US
dc.description.sponsorshipThis project was funded by NSF Grant OCE-1634490. During this work W.M. Kranenburg was supported as USGS Postdoctoral Scholar at Woods Hole Oceanographic Institution. A.M.P. Garcia was supported by the Michael J. Kowalski Fellowship in Ocean Science and Engineering (AMPG), and the Diversity Fellowship of the MIT Office of the Dean of Graduate Education (AMPG). The authors thank Jay Sisson for the technical support and Peter Traykovski for providing the bathymetric data. Also, the suggestions for improvement by Dr. K. Blanckaert and an anonymous reviewer are thankfully acknowledged.en_US
dc.publisherAmerican Meteorological Societyen_US
dc.relation.urihttps://doi.org/10.1175/JPO-D-18-0175.1
dc.subjectEstuariesen_US
dc.subjectAdvectionen_US
dc.subjectBaroclinic flowsen_US
dc.subjectBarotropic flowsen_US
dc.titleReversed lateral circulation in a sharp estuarine bend with weak stratificationen_US
dc.typeArticleen_US
dc.identifier.doi10.1175/JPO-D-18-0175.1


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