Geometry and topology of estuary and braided river channel networks automatically extracted from topographic data

Matthew Hiatt (Corresponding author), Willem M. Sonke, Elisabeth Addink, Wout van Dijk, Marc J. van Kreveld, Tim A.E. Ophelders, Kevin A.B. Verbeek, Joyce Vlaming, Bettina Speckmann, Maarten G. Kleinhans

Research output: Contribution to journalArticleAcademicpeer-review

Abstract

Automatic extraction of channel networks from topography in systems with multiple interconnected channels, like braided rivers and estuaries, remains a major challenge in hydrology and geomorphology. Representing channelized systems as networks provides a mathematical framework for analyzing transport and geomorphology. In this paper, we introduce a mathematically rigorous methodology and software for extracting channel network topology and geometry from digital elevation models (DEMs) and analyze such channel networks in estuaries and braided rivers. Channels are represented as network links, while channel confluences and bifurcations are represented as network nodes. We analyze and compare DEMs from the field and those generated by numerical modeling. We use a metric called the volume parameter that characterizes the volume of deposited material separating channels to quantify the volume of reworkable sediment deposited between links, which is a measure for the spatial scale associated with each network link. Scale asymmetry is observed in most links downstream of bifurcations, indicating geometric asymmetry and bifurcation stability. The length of links relative to system size scales with volume parameter value to the power of 0.24–0.35, while the number of links decreases and does not exhibit power law behavior. Link depth distributions indicate that the estuaries studied tend to organize around a deep main channel that exists at the largest scale while braided rivers have channel depths that are more evenly distributed across scales. The methods and results presented establish a benchmark for quantifying the topology and geometry of multichannel networks from DEMs with a new automatic extraction tool.
Original languageEnglish
Article numbere2019JF005206
Number of pages19
JournalJournal of Geophysical Research: Earth Surface
Volume125
Issue number1
DOIs
Publication statusPublished - 5 Jan 2020

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braided river
river channel
topology
estuary
geometry
bifurcation
digital elevation model
geomorphology
asymmetry
confluence
vertical distribution
power law
hydrology
topography
software
methodology

Cite this

@article{27504b3f6202409b913d3388d7b0fc6f,
title = "Geometry and topology of estuary and braided river channel networks automatically extracted from topographic data",
abstract = "Automatic extraction of channel networks from topography in systems with multiple interconnected channels, like braided rivers and estuaries, remains a major challenge in hydrology and geomorphology. Representing channelized systems as networks provides a mathematical framework for analyzing transport and geomorphology. In this paper, we introduce a mathematically rigorous methodology and software for extracting channel network topology and geometry from digital elevation models (DEMs) and analyze such channel networks in estuaries and braided rivers. Channels are represented as network links, while channel confluences and bifurcations are represented as network nodes. We analyze and compare DEMs from the field and those generated by numerical modeling. We use a metric called the volume parameter that characterizes the volume of deposited material separating channels to quantify the volume of reworkable sediment deposited between links, which is a measure for the spatial scale associated with each network link. Scale asymmetry is observed in most links downstream of bifurcations, indicating geometric asymmetry and bifurcation stability. The length of links relative to system size scales with volume parameter value to the power of 0.24–0.35, while the number of links decreases and does not exhibit power law behavior. Link depth distributions indicate that the estuaries studied tend to organize around a deep main channel that exists at the largest scale while braided rivers have channel depths that are more evenly distributed across scales. The methods and results presented establish a benchmark for quantifying the topology and geometry of multichannel networks from DEMs with a new automatic extraction tool.",
author = "Matthew Hiatt and Sonke, {Willem M.} and Elisabeth Addink and {van Dijk}, Wout and {van Kreveld}, {Marc J.} and Ophelders, {Tim A.E.} and Verbeek, {Kevin A.B.} and Joyce Vlaming and Bettina Speckmann and Kleinhans, {Maarten G.}",
year = "2020",
month = "1",
day = "5",
doi = "10.1029/2019JF005206",
language = "English",
volume = "125",
journal = "Journal of Geophysical Research: Earth Surface",
issn = "0148-0227",
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Geometry and topology of estuary and braided river channel networks automatically extracted from topographic data. / Hiatt, Matthew (Corresponding author); Sonke, Willem M.; Addink, Elisabeth; van Dijk, Wout; van Kreveld, Marc J.; Ophelders, Tim A.E.; Verbeek, Kevin A.B.; Vlaming, Joyce; Speckmann, Bettina; Kleinhans, Maarten G.

In: Journal of Geophysical Research: Earth Surface, Vol. 125, No. 1, e2019JF005206, 05.01.2020.

Research output: Contribution to journalArticleAcademicpeer-review

TY - JOUR

T1 - Geometry and topology of estuary and braided river channel networks automatically extracted from topographic data

AU - Hiatt, Matthew

AU - Sonke, Willem M.

AU - Addink, Elisabeth

AU - van Dijk, Wout

AU - van Kreveld, Marc J.

AU - Ophelders, Tim A.E.

AU - Verbeek, Kevin A.B.

AU - Vlaming, Joyce

AU - Speckmann, Bettina

AU - Kleinhans, Maarten G.

PY - 2020/1/5

Y1 - 2020/1/5

N2 - Automatic extraction of channel networks from topography in systems with multiple interconnected channels, like braided rivers and estuaries, remains a major challenge in hydrology and geomorphology. Representing channelized systems as networks provides a mathematical framework for analyzing transport and geomorphology. In this paper, we introduce a mathematically rigorous methodology and software for extracting channel network topology and geometry from digital elevation models (DEMs) and analyze such channel networks in estuaries and braided rivers. Channels are represented as network links, while channel confluences and bifurcations are represented as network nodes. We analyze and compare DEMs from the field and those generated by numerical modeling. We use a metric called the volume parameter that characterizes the volume of deposited material separating channels to quantify the volume of reworkable sediment deposited between links, which is a measure for the spatial scale associated with each network link. Scale asymmetry is observed in most links downstream of bifurcations, indicating geometric asymmetry and bifurcation stability. The length of links relative to system size scales with volume parameter value to the power of 0.24–0.35, while the number of links decreases and does not exhibit power law behavior. Link depth distributions indicate that the estuaries studied tend to organize around a deep main channel that exists at the largest scale while braided rivers have channel depths that are more evenly distributed across scales. The methods and results presented establish a benchmark for quantifying the topology and geometry of multichannel networks from DEMs with a new automatic extraction tool.

AB - Automatic extraction of channel networks from topography in systems with multiple interconnected channels, like braided rivers and estuaries, remains a major challenge in hydrology and geomorphology. Representing channelized systems as networks provides a mathematical framework for analyzing transport and geomorphology. In this paper, we introduce a mathematically rigorous methodology and software for extracting channel network topology and geometry from digital elevation models (DEMs) and analyze such channel networks in estuaries and braided rivers. Channels are represented as network links, while channel confluences and bifurcations are represented as network nodes. We analyze and compare DEMs from the field and those generated by numerical modeling. We use a metric called the volume parameter that characterizes the volume of deposited material separating channels to quantify the volume of reworkable sediment deposited between links, which is a measure for the spatial scale associated with each network link. Scale asymmetry is observed in most links downstream of bifurcations, indicating geometric asymmetry and bifurcation stability. The length of links relative to system size scales with volume parameter value to the power of 0.24–0.35, while the number of links decreases and does not exhibit power law behavior. Link depth distributions indicate that the estuaries studied tend to organize around a deep main channel that exists at the largest scale while braided rivers have channel depths that are more evenly distributed across scales. The methods and results presented establish a benchmark for quantifying the topology and geometry of multichannel networks from DEMs with a new automatic extraction tool.

U2 - 10.1029/2019JF005206

DO - 10.1029/2019JF005206

M3 - Article

VL - 125

JO - Journal of Geophysical Research: Earth Surface

JF - Journal of Geophysical Research: Earth Surface

SN - 0148-0227

IS - 1

M1 - e2019JF005206

ER -