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Are equilibrium multichannel networks predictable? The case of the regulated Indus River, Pakistan

Are equilibrium multichannel networks predictable? The case of the regulated Indus River, Pakistan
Are equilibrium multichannel networks predictable? The case of the regulated Indus River, Pakistan
Arguably, the current planform behaviour of the Indus River is broadly predictable. Between Chashma and Taunsa, Pakistan, the Indus is a 264-km-long multiple-channel reach. Remote sensing imagery, encompassing major floods in 2007 and 2010, shows that the Indus has a minimum of two and a maximum of nine channels, with on average four active channels during the dry season and five during the annual monsoon. Thus, the network structure, if not detailed planform, remains stable even for the record 2010 flood (27,100 m3 s− 1; recurrence interval > 100 years). Bankline recession is negligible for discharges less than a peak annual discharge of 6000 m3 s− 1 (~ 80% of mean annual flood). The Maximum Flow Efficiency (MFE) principle demonstrates that the channel network is insensitive to the monsoon floods, which typically peak at 13,200 m3 s− 1. Rather, the network is in near-equilibrium with the mean annual flood (7530 m3 s− 1). The MFE principle indicates that stable networks have three to four channels, thus the observed stability in the number of active channels accords with the presence of a near-equilibrium reach-scale channel network. Insensitivity to the annual hydrological cycle demonstrates that the timescale for network adjustment is much longer than the timescale of the monsoon hydrograph, with the annual excess water being stored on floodplains rather than being conveyed in an enlarged channel network. The analysis explains the lack of significant channel adjustment following the largest flood in 40 years and the extensive Indus flooding experienced on an annual basis, with its substantial impacts on the populace and agricultural production.
0169-555X
Carling, Paul
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Trieu, Hai, Quang
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Hornby, Duncan
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Huang, He Qing
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Darby, Stephen
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Sear, David
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Hutton, Craig
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Hill, C.
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Ali, Z
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Ahmed, A
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Iqbal, I
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Hussain, Z
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Carling, Paul
8d252dd9-3c88-4803-81cc-c2ec4c6fa687
Trieu, Hai, Quang
4d1ee5ca-e853-4526-874a-0a4a5f5bb8f5
Hornby, Duncan
75cfaf57-72c1-4392-a78c-89b4b1033dca
Huang, He Qing
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Darby, Stephen
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Sear, David
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Hutton, Craig
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Hill, C.
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Ali, Z
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Ahmed, A
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Iqbal, I
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Hussain, Z
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Carling, Paul, Trieu, Hai, Quang, Hornby, Duncan, Huang, He Qing, Darby, Stephen, Sear, David, Hutton, Craig, Hill, C., Ali, Z, Ahmed, A, Iqbal, I and Hussain, Z (2018) Are equilibrium multichannel networks predictable? The case of the regulated Indus River, Pakistan. Geomorphology. (doi:10.1016/j.geomorph.2017.09.021).

Record type: Article

Abstract

Arguably, the current planform behaviour of the Indus River is broadly predictable. Between Chashma and Taunsa, Pakistan, the Indus is a 264-km-long multiple-channel reach. Remote sensing imagery, encompassing major floods in 2007 and 2010, shows that the Indus has a minimum of two and a maximum of nine channels, with on average four active channels during the dry season and five during the annual monsoon. Thus, the network structure, if not detailed planform, remains stable even for the record 2010 flood (27,100 m3 s− 1; recurrence interval > 100 years). Bankline recession is negligible for discharges less than a peak annual discharge of 6000 m3 s− 1 (~ 80% of mean annual flood). The Maximum Flow Efficiency (MFE) principle demonstrates that the channel network is insensitive to the monsoon floods, which typically peak at 13,200 m3 s− 1. Rather, the network is in near-equilibrium with the mean annual flood (7530 m3 s− 1). The MFE principle indicates that stable networks have three to four channels, thus the observed stability in the number of active channels accords with the presence of a near-equilibrium reach-scale channel network. Insensitivity to the annual hydrological cycle demonstrates that the timescale for network adjustment is much longer than the timescale of the monsoon hydrograph, with the annual excess water being stored on floodplains rather than being conveyed in an enlarged channel network. The analysis explains the lack of significant channel adjustment following the largest flood in 40 years and the extensive Indus flooding experienced on an annual basis, with its substantial impacts on the populace and agricultural production.

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Accepted/In Press date: 19 September 2017
e-pub ahead of print date: 27 September 2017
Published date: 1 February 2018

Identifiers

Local EPrints ID: 414785
URI: http://eprints.soton.ac.uk/id/eprint/414785
ISSN: 0169-555X
PURE UUID: 27dca3ee-d537-4952-95ac-9681b8a72193
ORCID for Duncan Hornby: ORCID iD orcid.org/0000-0001-6295-1360
ORCID for Stephen Darby: ORCID iD orcid.org/0000-0001-8778-4394
ORCID for David Sear: ORCID iD orcid.org/0000-0003-0191-6179
ORCID for Craig Hutton: ORCID iD orcid.org/0000-0002-5896-756X

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Date deposited: 11 Oct 2017 16:31
Last modified: 16 Mar 2024 03:39

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Contributors

Author: Paul Carling
Author: Hai, Quang Trieu
Author: Duncan Hornby ORCID iD
Author: He Qing Huang
Author: Stephen Darby ORCID iD
Author: David Sear ORCID iD
Author: Craig Hutton ORCID iD
Author: C. Hill
Author: Z Ali
Author: A Ahmed
Author: I Iqbal
Author: Z Hussain

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