Geomorphic adjustment to hydrologic modifications along a meandering river: Implications for surface flooding on a floodplain

Geomorphic adjustment to hydrologic modifications along a meandering river: Implications for surface flooding on a floodplain

Responses of large regulated rivers to contemporary changes in base level are not well understood. We used field measurements and historical analysis of air photos and topographic maps to identify geomorphic trends of the lower White River, Arkansas, USA, in the 70years following base-level lowering...

Full description

Saved in:
Bibliographic Details
Published in:Geomorphology (Amsterdam, Netherlands) Vol. 269; pp. 149 - 159
Main Authors: Edwards, Brandon L., Keim, Richard F., Johnson, Erin L., Hupp, Cliff R., Marre, Saraline, King, Sammy L.
Format: Journal Article
Language:English
Published: Elsevier B.V 15-09-2016
Subjects:
Adjustment
Anthropogenic modification
Channel incision
Flood control
Flood modeling
Flooding
Floodplain geomorphology
Floods
Freshwater
Geomorphology
Hydrology
Mississippi River (US)
Rivers
USA, Arkansas
USA, Arkansas, White R
North America, Mississippi R
Channel incision
Anthropogenic modification
Floodplain geomorphology
Flood modeling
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:Responses of large regulated rivers to contemporary changes in base level are not well understood. We used field measurements and historical analysis of air photos and topographic maps to identify geomorphic trends of the lower White River, Arkansas, USA, in the 70years following base-level lowering at its confluence with the Mississippi River and concurrent with flood control by dams. Incision was identified below a knickpoint area upstream of St. Charles, AR, and increases over the lowermost ~90km of the study site to ~2m near the confluence with the Mississippi River. Mean bankfull width increased by 30m (21%) from 1930 to 2010. Bank widening appears to be the result of flow regulation above the incision knickpoint and concomitant with incision below the knickpoint. Hydraulic modeling indicated that geomorphic adjustments likely reduced flooding by 58% during frequent floods in the incised, lowermost floodplain affected by backwater flooding from the Mississippi River and by 22% above the knickpoint area. Dominance of backwater flooding in the incised reach indicates that incision is more important than flood control on the lower White River in altering flooding and also suggests that the Mississippi River may be the dominant control in shaping the lower floodplain. Overall, results highlight the complex geomorphic adjustment in large river-floodplain systems in response to anthropogenic modifications and their implications, including reduced river-floodplain connectivity. •Response of a large river to dam closure and lowered base level is documented.•Bank widening in response to dam closure occurred rapidly in upper channel.•Bank widening and incision in lower channel in response to main stem modification.•Flood modeling shows significant impact of geomorphic adjustment on flood extent.•Results highlight transition from watershed to main stem backwater dominance.
Bibliography:ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0169-555X
1872-695X
DOI:10.1016/j.geomorph.2016.06.037