Gravitational circulation in straits and estuaries

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ID: 300023
2021
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Abstract
A coupled set of partial differential equations and associated boundary conditions is written to describe circulation and salt-flux processes for estuaries in which turbulent mixing results primarily from tidal currents. Similarity solutions, motivated by characteristic salinity distributions observed in estuaries, are obtained for this set of equations and are compared with observational data. The circulation is separated into modes analogous to the barotropic, baroclinic, and Ekman modes of oceanic circulation. The salinity distribution, although coupled to the velocity distribution, is found to vary independently of it as well. The theoretical results are discussed in regard to: (i) correlation between the vertical variations of mean velocity and salinity, (ii) the role of this correlation in maintaining the steady-state salinity distribution in estuaries, and (iii) some implications for computations of flushing and dispersion of contaminants.
Reference Key
openalex_W4205690301 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Donald V. Hansen, Maurice Rattray
Journal journal of marine research
Year 2021
DOI
10.1357/002224021834614399
URL
Keywords Keywords not found

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