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Influence of the nodal tide on the morphological response of estuaries

Influence of the nodal tide on the morphological response of estuaries
Influence of the nodal tide on the morphological response of estuaries

The nodal tide causes a periodic variation in the mean tidal range, with a period of 18.6. years and amplitude of about 4% of the mean range. As the cross-sectional area of the channel in an estuary has been observed to be related to the tidal prism, such a variation of the tidal range can significantly influence the morphological development of tide-dominated estuaries. Field observations from the Humber Estuary in England confirm that there is indeed an 18.6. year cycle in the total water volume of the estuary. In this estuary, with a relatively small morphological time scale, the response to the nodal tide variation appears to dominate the long-term large-scale sediment budget changes of the estuary. The semi-empirical model ESTMORF was able to reproduce these observations, in terms of the observed amplitude and phase lag (relative to the variation of the tidal amplitude) of the morphological response. It also showed good agreement with the along estuary variation in both the magnitude and phase of the response. To examine the character of the response in more detail, a simplified analytical solution has been derived from the governing non-linear equations. This has been investigated in terms of the sensitivity of the model to the various model parameters and by comparison with the historic data. The results demonstrate how the system response is strongly dependent on the morphological time scale of the estuary. Furthermore, the response is not uniform but varies along the length of the estuary, being most marked at the mouth and decaying up estuary. When examining changes in geomorphological features, such as the intertidal area, an appreciation of the role of the nodal tide is shown to be essential if historic data are to be properly interpreted.

Field observations, Humber Estuary, Modelling, Nodal tides, Sediment budget
0025-3227
73-82
Wang, Z. B.
701b3877-0155-4fd7-beab-a8661eb70b88
Townend, I. H.
f72e5186-cae8-41fd-8712-d5746f78328e
Wang, Z. B.
701b3877-0155-4fd7-beab-a8661eb70b88
Townend, I. H.
f72e5186-cae8-41fd-8712-d5746f78328e

Wang, Z. B. and Townend, I. H. (2012) Influence of the nodal tide on the morphological response of estuaries. Marine Geology, 291-294, 73-82. (doi:10.1016/j.margeo.2011.11.007).

Record type: Article

Abstract

The nodal tide causes a periodic variation in the mean tidal range, with a period of 18.6. years and amplitude of about 4% of the mean range. As the cross-sectional area of the channel in an estuary has been observed to be related to the tidal prism, such a variation of the tidal range can significantly influence the morphological development of tide-dominated estuaries. Field observations from the Humber Estuary in England confirm that there is indeed an 18.6. year cycle in the total water volume of the estuary. In this estuary, with a relatively small morphological time scale, the response to the nodal tide variation appears to dominate the long-term large-scale sediment budget changes of the estuary. The semi-empirical model ESTMORF was able to reproduce these observations, in terms of the observed amplitude and phase lag (relative to the variation of the tidal amplitude) of the morphological response. It also showed good agreement with the along estuary variation in both the magnitude and phase of the response. To examine the character of the response in more detail, a simplified analytical solution has been derived from the governing non-linear equations. This has been investigated in terms of the sensitivity of the model to the various model parameters and by comparison with the historic data. The results demonstrate how the system response is strongly dependent on the morphological time scale of the estuary. Furthermore, the response is not uniform but varies along the length of the estuary, being most marked at the mouth and decaying up estuary. When examining changes in geomorphological features, such as the intertidal area, an appreciation of the role of the nodal tide is shown to be essential if historic data are to be properly interpreted.

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More information

Published date: 1 January 2012
Keywords: Field observations, Humber Estuary, Modelling, Nodal tides, Sediment budget

Identifiers

Local EPrints ID: 469412
URI: http://eprints.soton.ac.uk/id/eprint/469412
ISSN: 0025-3227
PURE UUID: 7aa2be9d-ab49-4a41-9e16-60f1fce22137
ORCID for I. H. Townend: ORCID iD orcid.org/0000-0003-2101-3858

Catalogue record

Date deposited: 14 Sep 2022 16:46
Last modified: 18 Mar 2024 02:55

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Contributors

Author: Z. B. Wang
Author: I. H. Townend ORCID iD

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