An examination of estuary stability in response to human interventions in the South Branch of the Yangtze (Changjiang) estuary, China
An examination of estuary stability in response to human interventions in the South Branch of the Yangtze (Changjiang) estuary, China
Estuary morphologies are dynamic systems, and their stabilities are dependent on various forcing conditions, including tides, waves, and fluvial inputs. However, during the past half century, massive anthropogenic interventions have occurred in many estuaries around the world, resulting in substantial changes in morphologies. Here, we examine such changes in the Yangtze estuary to study decadal morphological stability under anthropogenic disturbances using an entropy-based approach. Using a numerical model, the influence of bathymetric changes and sea-level rise on the variations in energy within the South Branch was examined. An analysis of the spatiotemporal bathymetric variations suggested that the South Branch can be subdivided into three segments of the lower, middle and upper reaches. The changes in these three segments relative to a theoretical equilibrium state were used to investigate and attribute the causes of change. It was found that (1) reclamation works in the South Branch during the last half century, primarily the Xuliujing reclamations (before 1980s) in the upper reach and the Changxing Island expansion (Qingcaosha Reservoir project, 2002–2007) in the lower reach, moved the system away from equilibrium by 2.5–3% in total, although the natural evolution between 1987 and 1997 restored some of the lost efficiency; (2) before large-scale reclamations, river flooding disturbed the system away from equilibrium by 3–6% in 1958, but this was mitigated by 1–2% due to the reclamation works that constrained the channel and deepened the subtidal area; (3) an entropy-based analysis suggested that the Xuliujing reclamation introduced a river constraint that influenced the reach ~20 km downstream, and by enclosing the Qingcaosha Reservoir, a tidal constraint was introduced that influenced the reach ~30 km upstream; and (4) morphological adjustment within the South Branch (a form of self-organization) has enabled the system to adjust to the imposed changes toward a new dynamic equilibrium, consistent with the prevailing constraints and forcing conditions. The results of this study demonstrate a method to determine estuary stability in the context of human interventions, and this method may be relevant to other estuaries subject to large-scale changes.
Energy, Reclamations, Stability, Yangtze (Changjiang) estuary
1-14
Zhang, Min
850608b2-ad0d-412a-a467-24dabdd0c1e4
Townend, Ian
f72e5186-cae8-41fd-8712-d5746f78328e
Zhou, Yunxuan
bc6ecb4c-5937-4580-950a-6997b7e5a903
Wang, Lihua
81a30ec6-a4df-4b47-96e5-2194cf0186ef
Dai, Zhijun
518bc4ef-716d-461d-a781-a3e5b4d04ba7
15 November 2019
Zhang, Min
850608b2-ad0d-412a-a467-24dabdd0c1e4
Townend, Ian
f72e5186-cae8-41fd-8712-d5746f78328e
Zhou, Yunxuan
bc6ecb4c-5937-4580-950a-6997b7e5a903
Wang, Lihua
81a30ec6-a4df-4b47-96e5-2194cf0186ef
Dai, Zhijun
518bc4ef-716d-461d-a781-a3e5b4d04ba7
Zhang, Min, Townend, Ian, Zhou, Yunxuan, Wang, Lihua and Dai, Zhijun
(2019)
An examination of estuary stability in response to human interventions in the South Branch of the Yangtze (Changjiang) estuary, China.
Estuarine, Coastal and Shelf Science, 228, , [106383].
(doi:10.1016/j.ecss.2019.106383).
Abstract
Estuary morphologies are dynamic systems, and their stabilities are dependent on various forcing conditions, including tides, waves, and fluvial inputs. However, during the past half century, massive anthropogenic interventions have occurred in many estuaries around the world, resulting in substantial changes in morphologies. Here, we examine such changes in the Yangtze estuary to study decadal morphological stability under anthropogenic disturbances using an entropy-based approach. Using a numerical model, the influence of bathymetric changes and sea-level rise on the variations in energy within the South Branch was examined. An analysis of the spatiotemporal bathymetric variations suggested that the South Branch can be subdivided into three segments of the lower, middle and upper reaches. The changes in these three segments relative to a theoretical equilibrium state were used to investigate and attribute the causes of change. It was found that (1) reclamation works in the South Branch during the last half century, primarily the Xuliujing reclamations (before 1980s) in the upper reach and the Changxing Island expansion (Qingcaosha Reservoir project, 2002–2007) in the lower reach, moved the system away from equilibrium by 2.5–3% in total, although the natural evolution between 1987 and 1997 restored some of the lost efficiency; (2) before large-scale reclamations, river flooding disturbed the system away from equilibrium by 3–6% in 1958, but this was mitigated by 1–2% due to the reclamation works that constrained the channel and deepened the subtidal area; (3) an entropy-based analysis suggested that the Xuliujing reclamation introduced a river constraint that influenced the reach ~20 km downstream, and by enclosing the Qingcaosha Reservoir, a tidal constraint was introduced that influenced the reach ~30 km upstream; and (4) morphological adjustment within the South Branch (a form of self-organization) has enabled the system to adjust to the imposed changes toward a new dynamic equilibrium, consistent with the prevailing constraints and forcing conditions. The results of this study demonstrate a method to determine estuary stability in the context of human interventions, and this method may be relevant to other estuaries subject to large-scale changes.
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Accepted/In Press date: 16 September 2019
e-pub ahead of print date: 16 September 2019
Published date: 15 November 2019
Keywords:
Energy, Reclamations, Stability, Yangtze (Changjiang) estuary
Identifiers
Local EPrints ID: 434945
URI: http://eprints.soton.ac.uk/id/eprint/434945
ISSN: 0272-7714
PURE UUID: c5c5c173-51d9-4ad1-b57c-2a55c7dedb05
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Date deposited: 16 Oct 2019 16:30
Last modified: 18 Mar 2024 05:25
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Author:
Min Zhang
Author:
Yunxuan Zhou
Author:
Lihua Wang
Author:
Zhijun Dai
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