Development and extension of an aggregated scale model: Part 2 – Extensions to ASMITA
Development and extension of an aggregated scale model: Part 2 – Extensions to ASMITA
Whilst much attention has been given to models that describe wave, tide and sediment transport processes in sufficient detail to determine the local changes in bed level over a relatively detailed representation of the bathymetry, far less attention has been given to models that consider the problem at a much larger scale (e.g. that of geomorphological elements such as a tidal flat and tidal channel). Such aggregated or lumped models tend not to represent the processes in detail but rather capture the behaviour at the scale of interest. One such model developed using the concept of an equilibrium concentration is the Aggregated Scale Morphological Interaction between Tidal basin and Adjacent coast (ASMITA). In a companion paper (Part 1), we detail the original model and provide some new insights into the concepts of equilibrium, and horizontal and vertical exchange that are key components of this modelling approach. In this paper, we summarise a range of developments that have been undertaken to extend the original model concept, to illustrate the flexibility and power of the conceptual framework. However, adding detail progressively moves the model in the direction of the more detailed process-based models and we give some consideration to the boundary between the two.
estuary, tidal inlet, morphology, tides, waves, sediment transport
651-670
Townend, Ian
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Wang, Zheng Bing
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Stive, Marcel
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Zhou, Zeng
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October 2016
Townend, Ian
f72e5186-cae8-41fd-8712-d5746f78328e
Wang, Zheng Bing
0bf73ba6-eed4-4ebe-8175-929d35912e3d
Stive, Marcel
0a2f8283-05bd-4557-9867-a9ba5d03922b
Zhou, Zeng
a167cd81-84c7-4e55-9e28-4529e26e7c01
Townend, Ian, Wang, Zheng Bing, Stive, Marcel and Zhou, Zeng
(2016)
Development and extension of an aggregated scale model: Part 2 – Extensions to ASMITA.
China Ocean Engineering, 30 (5), .
(doi:10.1007/s13344-016-0042-6).
Abstract
Whilst much attention has been given to models that describe wave, tide and sediment transport processes in sufficient detail to determine the local changes in bed level over a relatively detailed representation of the bathymetry, far less attention has been given to models that consider the problem at a much larger scale (e.g. that of geomorphological elements such as a tidal flat and tidal channel). Such aggregated or lumped models tend not to represent the processes in detail but rather capture the behaviour at the scale of interest. One such model developed using the concept of an equilibrium concentration is the Aggregated Scale Morphological Interaction between Tidal basin and Adjacent coast (ASMITA). In a companion paper (Part 1), we detail the original model and provide some new insights into the concepts of equilibrium, and horizontal and vertical exchange that are key components of this modelling approach. In this paper, we summarise a range of developments that have been undertaken to extend the original model concept, to illustrate the flexibility and power of the conceptual framework. However, adding detail progressively moves the model in the direction of the more detailed process-based models and we give some consideration to the boundary between the two.
Text
Ian paper_part2 Proof.pdf
- Accepted Manuscript
More information
Accepted/In Press date: 16 May 2016
e-pub ahead of print date: 9 October 2016
Published date: October 2016
Keywords:
estuary, tidal inlet, morphology, tides, waves, sediment transport
Organisations:
Coastal & Shelf Research
Identifiers
Local EPrints ID: 402915
URI: http://eprints.soton.ac.uk/id/eprint/402915
ISSN: 0890-5487
PURE UUID: b4b39bdb-cf37-44d4-a7c1-905a48d6bee5
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Date deposited: 05 Dec 2016 10:05
Last modified: 16 Mar 2024 03:24
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Contributors
Author:
Zheng Bing Wang
Author:
Marcel Stive
Author:
Zeng Zhou
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