Tidal amplification and river capture in response to land reclamation in the Ganges-Brahmaputra delta
At a global scale, intertidal areas are being reclaimed for agriculture as well as urban expansion, imposing high human pressure on the coastal zone. The Ganges-Brahmaputra Delta (GBD) is an exponent of this development. In this delta, land reclamation accelerated in the 1960's to 1980's, when polders were constructed in areas subject to regular marine flooding. A comprehensive analysis of tidal channel evolution in the southwest GBD reveals how land reclamation leads to tidal amplification, channel shoaling, bank erosion, and interaction between channels in which one tidal river captures the storage area of a neighbouring river. We identify-two positive feedback mechanisms that govern these morphological changes. First, reclaiming intertidal areas results in immediate loss of tidal storage, which leads to amplification and faster propagation of the tides. In systems with abundant sediment supply, the blind tidal channels progressively fill in with sediment, leading to a continued loss of tidal storage and therefore further distorting the tides. Secondly, when intertidal areas of parallel (and inter-connected) river delta distributaries are asynchronously or unevenly reclaimed, one channel distributary may expand its intertidal area at the expense of the other. This is initiated by an increasing propagation speed of the tidal wave in the partially reclaimed distributary, travelling into the non-reclaimed distributary through connecting channels. These connecting channels progressively expand while the pristine channel shoals, and potentially degenerates. Both positive feedback loops are very stable and are responsible for pluvial flooding of polders, large-scale bank erosion, and poorly navigable primary waterways, including the navigation channel accessing Bangladesh's second-largest port. Interventions aiming to solve these problems have to account for the complex positive feedback mechanisms identified in this paper and be nature-based and holistic.
Main Authors: | , , , , , |
---|---|
Format: | Article/Letter to editor biblioteca |
Language: | English |
Subjects: | Estuary, Fine sediments, Ganges-Brahmaputra delta, Human impacts, Land reclamations, Tidal amplification, |
Online Access: | https://research.wur.nl/en/publications/tidal-amplification-and-river-capture-in-response-to-land-reclama |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
id |
dig-wur-nl-wurpubs-603286 |
---|---|
record_format |
koha |
spelling |
dig-wur-nl-wurpubs-6032862024-12-04 van Maren, D.S. Beemster, J.G.W. Wang, Z.B. Khan, Z.H. Schrijvershof, R.A. Hoitink, A.J.F. Article/Letter to editor Catena 220 (2023) ISSN: 0341-8162 Tidal amplification and river capture in response to land reclamation in the Ganges-Brahmaputra delta 2023 At a global scale, intertidal areas are being reclaimed for agriculture as well as urban expansion, imposing high human pressure on the coastal zone. The Ganges-Brahmaputra Delta (GBD) is an exponent of this development. In this delta, land reclamation accelerated in the 1960's to 1980's, when polders were constructed in areas subject to regular marine flooding. A comprehensive analysis of tidal channel evolution in the southwest GBD reveals how land reclamation leads to tidal amplification, channel shoaling, bank erosion, and interaction between channels in which one tidal river captures the storage area of a neighbouring river. We identify-two positive feedback mechanisms that govern these morphological changes. First, reclaiming intertidal areas results in immediate loss of tidal storage, which leads to amplification and faster propagation of the tides. In systems with abundant sediment supply, the blind tidal channels progressively fill in with sediment, leading to a continued loss of tidal storage and therefore further distorting the tides. Secondly, when intertidal areas of parallel (and inter-connected) river delta distributaries are asynchronously or unevenly reclaimed, one channel distributary may expand its intertidal area at the expense of the other. This is initiated by an increasing propagation speed of the tidal wave in the partially reclaimed distributary, travelling into the non-reclaimed distributary through connecting channels. These connecting channels progressively expand while the pristine channel shoals, and potentially degenerates. Both positive feedback loops are very stable and are responsible for pluvial flooding of polders, large-scale bank erosion, and poorly navigable primary waterways, including the navigation channel accessing Bangladesh's second-largest port. Interventions aiming to solve these problems have to account for the complex positive feedback mechanisms identified in this paper and be nature-based and holistic. en application/pdf https://research.wur.nl/en/publications/tidal-amplification-and-river-capture-in-response-to-land-reclama 10.1016/j.catena.2022.106651 https://edepot.wur.nl/579277 Estuary Fine sediments Ganges-Brahmaputra delta Human impacts Land reclamations Tidal amplification https://creativecommons.org/licenses/by/4.0/ https://creativecommons.org/licenses/by/4.0/ Wageningen University & Research |
institution |
WUR NL |
collection |
DSpace |
country |
Países bajos |
countrycode |
NL |
component |
Bibliográfico |
access |
En linea |
databasecode |
dig-wur-nl |
tag |
biblioteca |
region |
Europa del Oeste |
libraryname |
WUR Library Netherlands |
language |
English |
topic |
Estuary Fine sediments Ganges-Brahmaputra delta Human impacts Land reclamations Tidal amplification Estuary Fine sediments Ganges-Brahmaputra delta Human impacts Land reclamations Tidal amplification |
spellingShingle |
Estuary Fine sediments Ganges-Brahmaputra delta Human impacts Land reclamations Tidal amplification Estuary Fine sediments Ganges-Brahmaputra delta Human impacts Land reclamations Tidal amplification van Maren, D.S. Beemster, J.G.W. Wang, Z.B. Khan, Z.H. Schrijvershof, R.A. Hoitink, A.J.F. Tidal amplification and river capture in response to land reclamation in the Ganges-Brahmaputra delta |
description |
At a global scale, intertidal areas are being reclaimed for agriculture as well as urban expansion, imposing high human pressure on the coastal zone. The Ganges-Brahmaputra Delta (GBD) is an exponent of this development. In this delta, land reclamation accelerated in the 1960's to 1980's, when polders were constructed in areas subject to regular marine flooding. A comprehensive analysis of tidal channel evolution in the southwest GBD reveals how land reclamation leads to tidal amplification, channel shoaling, bank erosion, and interaction between channels in which one tidal river captures the storage area of a neighbouring river. We identify-two positive feedback mechanisms that govern these morphological changes. First, reclaiming intertidal areas results in immediate loss of tidal storage, which leads to amplification and faster propagation of the tides. In systems with abundant sediment supply, the blind tidal channels progressively fill in with sediment, leading to a continued loss of tidal storage and therefore further distorting the tides. Secondly, when intertidal areas of parallel (and inter-connected) river delta distributaries are asynchronously or unevenly reclaimed, one channel distributary may expand its intertidal area at the expense of the other. This is initiated by an increasing propagation speed of the tidal wave in the partially reclaimed distributary, travelling into the non-reclaimed distributary through connecting channels. These connecting channels progressively expand while the pristine channel shoals, and potentially degenerates. Both positive feedback loops are very stable and are responsible for pluvial flooding of polders, large-scale bank erosion, and poorly navigable primary waterways, including the navigation channel accessing Bangladesh's second-largest port. Interventions aiming to solve these problems have to account for the complex positive feedback mechanisms identified in this paper and be nature-based and holistic. |
format |
Article/Letter to editor |
topic_facet |
Estuary Fine sediments Ganges-Brahmaputra delta Human impacts Land reclamations Tidal amplification |
author |
van Maren, D.S. Beemster, J.G.W. Wang, Z.B. Khan, Z.H. Schrijvershof, R.A. Hoitink, A.J.F. |
author_facet |
van Maren, D.S. Beemster, J.G.W. Wang, Z.B. Khan, Z.H. Schrijvershof, R.A. Hoitink, A.J.F. |
author_sort |
van Maren, D.S. |
title |
Tidal amplification and river capture in response to land reclamation in the Ganges-Brahmaputra delta |
title_short |
Tidal amplification and river capture in response to land reclamation in the Ganges-Brahmaputra delta |
title_full |
Tidal amplification and river capture in response to land reclamation in the Ganges-Brahmaputra delta |
title_fullStr |
Tidal amplification and river capture in response to land reclamation in the Ganges-Brahmaputra delta |
title_full_unstemmed |
Tidal amplification and river capture in response to land reclamation in the Ganges-Brahmaputra delta |
title_sort |
tidal amplification and river capture in response to land reclamation in the ganges-brahmaputra delta |
url |
https://research.wur.nl/en/publications/tidal-amplification-and-river-capture-in-response-to-land-reclama |
work_keys_str_mv |
AT vanmarends tidalamplificationandrivercaptureinresponsetolandreclamationinthegangesbrahmaputradelta AT beemsterjgw tidalamplificationandrivercaptureinresponsetolandreclamationinthegangesbrahmaputradelta AT wangzb tidalamplificationandrivercaptureinresponsetolandreclamationinthegangesbrahmaputradelta AT khanzh tidalamplificationandrivercaptureinresponsetolandreclamationinthegangesbrahmaputradelta AT schrijvershofra tidalamplificationandrivercaptureinresponsetolandreclamationinthegangesbrahmaputradelta AT hoitinkajf tidalamplificationandrivercaptureinresponsetolandreclamationinthegangesbrahmaputradelta |
_version_ |
1819142033407737856 |