skip to main content
US FlagAn official website of the United States government
dot gov icon
Official websites use .gov
A .gov website belongs to an official government organization in the United States.
https lock icon
Secure .gov websites use HTTPS
A lock ( lock ) or https:// means you've safely connected to the .gov website. Share sensitive information only on official, secure websites.


Title: Geospatial data for natural channel centerlines across the continental US
This data repository includes (1) the original observations for channel bank positions of 143 meandering reaches in 89 rivers across the continental US in the dataset of the National Cooperative Highway Research Program Project (NCHRP) 24-26 (Lagasse et al., 2004), and (2) the geospatial data for centerlines of 103 meandering reaches in 70 rivers recovered from the original NCHRP 24-26 dataset. Reference: Lagasse, P. F., Zevenbergen, L. W., Spitz, W. J., & Thorne, C. R., 2004. Methodology for predicting channel migration. Washington, DC: Transportation Research Board. https://doi.org/10.17226/23352  more » « less
Award ID(s):
1823530
PAR ID:
10585133
Author(s) / Creator(s):
;
Publisher / Repository:
University of Virginia Dataverse
Date Published:
Subject(s) / Keyword(s):
Earth and Environmental Sciences Geomorphology, meandering rivers, channel positions
Format(s):
Medium: X
Right(s):
Creative Commons Zero v1.0 Universal
Sponsoring Org:
National Science Foundation
More Like this
  1. NA (Ed.)
    Recent research has indicated that numerous lowland rivers in North America and Europe had multithread, anabranching channel patterns prior to widespread human modification of landscapes and that contemporary human activities have transformed many anabranching rivers into single-channel meandering rivers. Although lowland rivers in the upper midwestern United States are predominantly meandering, anabranching occurs locally. Whether anabranching of these river systems was uncommon in the past or intensive agriculture has resulted in near eradication of anabranching channel patterns remains uncertain. This article quantifies the prevalence of river anabranching within several watersheds in the upper midwestern United States prior to widespread European settlement in the early to mid-1800s based on General Land Office survey plat maps and field notes. It also compares this prevalence to the contemporary occurrence of river anabranching. Results show that anabranching reaches were somewhat more common historically (22 percent more reaches in the past compared to the present), but were still relatively rare, constituting only about 1 percent of the total length of streams in the study watersheds. Analysis of the geographic distribution of anabranching reaches reveals that historical spatial patterns generally are different than modern patterns. Thus, only a handful of historical anabranching reaches have persisted through time to the present. The findings place contemporary river anabranching in the upper midwestern United States within the context of past conditions and suggest that human modification of landscapes throughout this region has not substantially modified channel patterns of rivers. 
    more » « less
  2. This is the archive of the numerical model and river centerline data used for analyzing the timescale related to meandering channel migration, which is tied to the manuscript submitted to Journal of Geophysical Research: Earth Surface: Li, Y., and Limaye, A. B., Timescale of the morphodynamic feedback between planform geometry and lateral migration of meandering rivers. 
    more » « less
  3. Abstract Source‐to‐sink transfer of sediment and organic carbon (OC) is regulated by river mobility. Quantifying trends in river mobility is, however, challenging due to diverse planform morphologies (e.g., meandering, braided) and measurement methods. Here, we utilize a remote‐sensing method applicable to all planform morphologies to quantify the mobility timescales of 80 rivers worldwide. Results show that, across the continuum from meandering to braided rivers, there is a systematic reduction in the timescales of channel mobility and—to a lesser extent—floodplain reworking. This leads to a decrease in the efficiency with which braided rivers rework old floodplain material compared to their meandering counterparts. Reduced floodplain reworking efficiency of braided rivers leads to smaller channel‐belt areas relative to their size. Results suggest that river‐mobility timescales derived from remote sensing can aid in the characterization of sediment and OC storage and transit times at a global scale. 
    more » « less
  4. Abstract In meandering rivers, interactions between flow, sediment transport, and bed topography affect diverse processes, including bedform development and channel migration. Predicting how these interactions affect the spatial patterns and magnitudes of bed deformation in meandering rivers is essential for various river engineering and geoscience problems. Computational fluid dynamics simulations can predict river morphodynamics at fine temporal and spatial scales but have traditionally been challenged by the large scale of natural rivers. We conducted coupled large‐eddy simulation and bed morphodynamics simulations to create a unique database of hydro‐morphodynamic data sets for 42 meandering rivers with a variety of planform shapes and large‐scale geometrical features that mimic natural meanders. For each simulated river, the database includes (a) bed morphology, (b) three‐dimensional mean velocity field, and (c) bed shear stress distribution under bankfull flow conditions. The calculated morphodynamics results at dynamic equilibrium revealed the formation of scour and deposition patterns near the outer and inner banks, respectively, while the location of point bars and scour regions around the apexes of the meander bends is found to vary as a function of the radius of curvature of the bends to the width ratio. A new mechanism is proposed that explains this seemingly paradoxical finding. The high‐fidelity simulation results generated in this work provide researchers and scientists with a rich numerical database for morphodynamics and bed shear stress distributions in large‐scale meandering rivers to enable systematic investigation of the underlying phenomena and support a range of river engineering applications. 
    more » « less
  5. Abstract Mutual adjustment between process and form shapes the morphology of alluvial river channels, including channel banks. The tops of banks define the transition between the channel and adjacent floodplain, which corresponds to the level of incipient flooding. Despite the geomorphological and hydrological importance of this transition, few, if any, studies have extensively examined spatial variability in bank elevations and its influence on bankfull stage. This study uses an objective method to explore this variability at two spatial resolutions along three alluvial lowland meandering rivers. Results show that variability in bankfull stage is inherent to all three rivers. The mean variability of bankfull stage about the average downstream gradient in this stage is 10% to 20% of mean bankfull depth. Elevations of channel banks exhibit similar variability, even after accounting for systematic variations in heights of inner and outer banks associated with river meandering. Two‐dimensional hydraulic simulations show that the elevation range of mean variability in bankfull stage overlaps considerably with the elevation range of high curvature on rating curves, confirming that variability in bankfull stage influences the shape of these curves. The simulations verify that breaks in channel banks allow flow to extend onto the floodplain at stages below the average bankfull stage. The findings provide fundamental insight into the variable nature of bankfull conditions along meandering rivers and the role of this variability in channel‐floodplain connectivity. The results also inform river‐restoration efforts that seek to re‐establish the natural configuration of channel banks. 
    more » « less