Hostname: page-component-848d4c4894-8kt4b Total loading time: 0 Render date: 2024-06-30T14:10:56.689Z Has data issue: false hasContentIssue false
  • English
  • Français

Tidal and Freshwater induced Circulation in the Tay Estuary.*

Published online by Cambridge University Press:  05 December 2011

J. A. Charlton ,
W. McNicoll  and
J. R. West
J. A. Charlton
Affiliation:
Department of Civil Engineering, University of Dundee
W. McNicoll
Affiliation:
Department of Civil Engineering, University of Dundee
J. R. West
Affiliation:
Department of Civil Engineering, University of Birmingham.
Get access

Extract

An understanding of the movement of a body of water can be considered a prerequisite to any other study whether it be physical or biological. This is particularly so in the case of an estuary where the water movements are complex. The movement of water in an estuary is primarily governed by the tidal and freshwater inputs, the resulting flow being modified by bed and channel configurations, salinity, and siltload variations. The tidal and freshwater inputs are themselves variables, the tidal range varying with the lunar cycle, and the freshwater input varying with the season or rainfall. The salinity variations within an estuary are interlinked with the tidal and freshwater fluctuating inputs. In addition the local and regional weather can modify the tidal response.

Type
Research Article
Information
Proceedings of the Royal Society of Edinburgh, Section B: Biological Sciences , Volume 75 , Issue 1-2: Physical and Biological Aspects of the Tay Estuary , 1975 , pp. 11 - 27
Copyright
Copyright © Royal Society of Edinburgh 1975

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Footnotes

*

This paper was assisted in publication by a grant from the Carnegie Trust for the Universities of Scotland.

References

Buller, A. T., Charlton, J. A. and McManus, J., 1972. Data from physical and chemical measurements in the Tay estuary for Neap and Spring tides June 1972. Tay Estuary Res. Rep., 2, 53 pp.Google Scholar
Buller, A. T., Charlton, J. A. and McManus, J., 1973. Chart of Upper Tay Estuary 1972–73. Dundee: Tay Estuary Research CentreGoogle Scholar
Craig, R. E., 1959. Hydrography of Scottish Coastal Waters. Mar. Res., 2.Google Scholar
Cunningham, D., 1895. Estuary of the Tay. Proc. Instn Civ. Engrs, 120, 299.Google Scholar
Davies, S. L., 1972. Undergraduate project thesis. Civil Eng. Dept., Dundee Univ.Google Scholar
Dronkers, J. J., 1964. Tidal Computations. North Holland.Google Scholar
Hydrographer, To The Navy, 1963. Pocket Tidal Stream Atlas. Flamborough Head-Pentland Firth (Chartlets 5198–5210), 1960. Chart No. 1481, River Tay.Google Scholar
Keers, J. R., 1966. Meteorological conditions leading to storm surges in the North Sea. Met. Mag. Lond., 95, 261–272.Google Scholar
Pontin, R. A., and Reid, J. A., 1975. The freshwater input to the Tay Estuary. Proc. Roy. Soc. Edinb. B, 75, 1–9.Google Scholar
Proudman, J. and Doodson, A. T., 1924. The principal constituents of the tides of the North Sea. Phil. Trans. Roy. Soc, A, 224, 185–219.Google Scholar
Rossiter, J. R., 1972. Sea level variations and their secular variation. Phil. Trans. Roy. Soc, A, 272, 131–140.Google Scholar
Silvester, R., 1974. Coastal Engineering, I. Elsevier.Google Scholar
West, J. R., 1973. On the salinity of the Tay Estuary. Ph.D. Thesis, Dundee Univ.Google Scholar