Decadal-Scale Variations of Thalweg Morphology and Riffle–Pool Sequences in Response to Flow Regulation in the Lowermost Mississippi River

The lowermost Mississippi River (LMR) is one of the largest deltaic systems in North America and one of the heavily human-manipulated fluvial river systems. Historic hydrographic surveys from the mid-1900s to the early 2010s were used to document the thalweg morphology adjustments, as well as the ri...

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Main Authors: Chia-Yu Wu, Joann Mossa
Format: Article
Language:English
Published: MDPI AG 2019-06-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/11/6/1175
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spelling doaj-97496243b582432284d908ee7d1971232020-11-24T21:20:19ZengMDPI AGWater2073-44412019-06-01116117510.3390/w11061175w11061175Decadal-Scale Variations of Thalweg Morphology and Riffle–Pool Sequences in Response to Flow Regulation in the Lowermost Mississippi RiverChia-Yu Wu0Joann Mossa1Department of Geography, University of Florida, Gainesville, FL 32611, USADepartment of Geography, University of Florida, Gainesville, FL 32611, USAThe lowermost Mississippi River (LMR) is one of the largest deltaic systems in North America and one of the heavily human-manipulated fluvial river systems. Historic hydrographic surveys from the mid-1900s to the early 2010s were used to document the thalweg morphology adjustments, as well as the riffle&#8722;pool sequences. Extensive aggradation was observed during 1950s to 1960s, as the Atchafalaya River was enlarging before the completion of the Old River Control Structure (ORCS). Following the completion of the ORCS, reductions in sediment input to the LMR resulted in net degradation of the thalweg profile patterns since the mid-1960s except for the 1992&#8722;2004 period. Different flood events that supplied sediment might be the cause of upstream aggradation from 1963&#8722;1975 and net aggradation along the entire reach from 1992&#8722;2004. Furthermore, the change pattern of thalweg profiles appear to be controlled by backwater effects, as well as the Bonnet Carr&#233; spillway opening. Results from riffle&#8722;pool sequences reveal that the averaging W<sub>s</sub> ratios (length to channel width) are 6&#8722;7, similar to numerous previous studies. Temporal variations of the same riffles and pools reveal that aggradation and degradation might be heavily controlled by similar factors to the thalweg variations (i.e., sediment supply, backwater effects). In sum, this study examines decadal-scale geomorphic responses in a low-lying large river system subject to different human interventions, as well as natural flood events. Future management strategies of this and similar river systems should consider recent riverbed changes in dredging, sediment management, and river engineering.https://www.mdpi.com/2073-4441/11/6/1175thalwegriffle–pool sequencelowermost Mississippi River
collection DOAJ
language English
format Article
sources DOAJ
author Chia-Yu Wu
Joann Mossa
spellingShingle Chia-Yu Wu
Joann Mossa
Decadal-Scale Variations of Thalweg Morphology and Riffle–Pool Sequences in Response to Flow Regulation in the Lowermost Mississippi River
Water
thalweg
riffle–pool sequence
lowermost Mississippi River
author_facet Chia-Yu Wu
Joann Mossa
author_sort Chia-Yu Wu
title Decadal-Scale Variations of Thalweg Morphology and Riffle–Pool Sequences in Response to Flow Regulation in the Lowermost Mississippi River
title_short Decadal-Scale Variations of Thalweg Morphology and Riffle–Pool Sequences in Response to Flow Regulation in the Lowermost Mississippi River
title_full Decadal-Scale Variations of Thalweg Morphology and Riffle–Pool Sequences in Response to Flow Regulation in the Lowermost Mississippi River
title_fullStr Decadal-Scale Variations of Thalweg Morphology and Riffle–Pool Sequences in Response to Flow Regulation in the Lowermost Mississippi River
title_full_unstemmed Decadal-Scale Variations of Thalweg Morphology and Riffle–Pool Sequences in Response to Flow Regulation in the Lowermost Mississippi River
title_sort decadal-scale variations of thalweg morphology and riffle–pool sequences in response to flow regulation in the lowermost mississippi river
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2019-06-01
description The lowermost Mississippi River (LMR) is one of the largest deltaic systems in North America and one of the heavily human-manipulated fluvial river systems. Historic hydrographic surveys from the mid-1900s to the early 2010s were used to document the thalweg morphology adjustments, as well as the riffle&#8722;pool sequences. Extensive aggradation was observed during 1950s to 1960s, as the Atchafalaya River was enlarging before the completion of the Old River Control Structure (ORCS). Following the completion of the ORCS, reductions in sediment input to the LMR resulted in net degradation of the thalweg profile patterns since the mid-1960s except for the 1992&#8722;2004 period. Different flood events that supplied sediment might be the cause of upstream aggradation from 1963&#8722;1975 and net aggradation along the entire reach from 1992&#8722;2004. Furthermore, the change pattern of thalweg profiles appear to be controlled by backwater effects, as well as the Bonnet Carr&#233; spillway opening. Results from riffle&#8722;pool sequences reveal that the averaging W<sub>s</sub> ratios (length to channel width) are 6&#8722;7, similar to numerous previous studies. Temporal variations of the same riffles and pools reveal that aggradation and degradation might be heavily controlled by similar factors to the thalweg variations (i.e., sediment supply, backwater effects). In sum, this study examines decadal-scale geomorphic responses in a low-lying large river system subject to different human interventions, as well as natural flood events. Future management strategies of this and similar river systems should consider recent riverbed changes in dredging, sediment management, and river engineering.
topic thalweg
riffle–pool sequence
lowermost Mississippi River
url https://www.mdpi.com/2073-4441/11/6/1175
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