Two Dimensional Aspects Of Salinity Intrusion In Estuaries
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Two dimensional Aspects of Salinity Intrusion in Estuaries
Author | : Donald R. F. Harleman,Arthur T. Ippen |
Publsiher | : Unknown |
Total Pages | : 72 |
Release | : 1967 |
Genre | : Estuaries |
ISBN | : UCR:31210024969725 |
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Unsteady Salinity Intrusion in Estuaries
Author | : Donald R. F. Harleman,John J. Fisher,M. Llewellyn Thatcher |
Publsiher | : Unknown |
Total Pages | : 54 |
Release | : 1974 |
Genre | : River Mouth and estuaries |
ISBN | : UCR:31210025034941 |
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Application of Boundary layer Theory to Dispersion in Nonstratified Two dimensional Esturaries
Author | : Jack Norman Nielsen,Gary D. Kuhn |
Publsiher | : Unknown |
Total Pages | : 126 |
Release | : 1973 |
Genre | : Estuaries |
ISBN | : UCR:31210024979484 |
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Technical Bulletin
Author | : Anonim |
Publsiher | : Unknown |
Total Pages | : 418 |
Release | : 1954 |
Genre | : Hydraulics |
ISBN | : UCSD:31822009437187 |
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Committee on Tidal Hydraulics Report
Author | : Anonim |
Publsiher | : Unknown |
Total Pages | : 582 |
Release | : 1968 |
Genre | : Coast changes |
ISBN | : UCSD:31822009379397 |
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Bibliography on Tidal Hydraulics
Author | : Virginia Dale |
Publsiher | : Unknown |
Total Pages | : 306 |
Release | : 1980 |
Genre | : Hydraulics |
ISBN | : UFL:31262085115318 |
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Evaluation of Numerical Storm Surge Models
Author | : United States. Army. Corps of Engineers. Committee on Tidal Hydraulics |
Publsiher | : Unknown |
Total Pages | : 98 |
Release | : 1980 |
Genre | : Hurricanes |
ISBN | : UOM:39015095027697 |
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One dimensional Analysis of Salinity Intrusion in Estuaries
Author | : Arthur T. Ippen,Donald R. F. Harleman,United States. Army. Corps of Engineers. Committee on Tidal Hydraulics |
Publsiher | : Unknown |
Total Pages | : 130 |
Release | : 1961 |
Genre | : Estuaries |
ISBN | : UFL:31262077187804 |
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An experimental and analytical study of the basic factors which determine the instantaneous longitudinal distribution of salinity in a partially mixed estuary of constant section is presented. The mass-transfer equation is solved in two parts: (a) the quasi-steady-state convective-diffusion problem for an observer moving with the tidal velocity, and (b) the cyclic translation of saline water due to the tidal velocity. In the steady-state portion the apparent longitudinal diffusion coefficient is a function of the turbulence induced by the tide and of the internal circulations induced by the density difference. An expression is developed for the intrusion length as a function of the estuary length, mean depth, tidal amplitude and period, fresh-water discharge, ocean salinity, and estuary roughness. A stratification number is defined which expresses the degree of stratification or mixing in an estuary. (Author).