John Shaw Data-verified
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Associate Professor
faculty
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Biography and Research Information
OverviewAI-generated summary
John Shaw, an Associate Professor at the University of Arkansas at Fayetteville, researches the morphodynamics of river- and deltaic systems. His work investigates the interplay of river and tidal forcings in shaping coastal channel networks and explores influences on discharge partitioning in large river deltas. Shaw has also examined ancient channel-mouth bifurcation angles on Earth and Mars, and the response of coastal environments to global warming during the Paleocene-Eocene Thermal Maximum. His research considers how marsh sedimentation controls delta morphology, slope, and mass balance, and the dynamic constraints on loop formation in transport networks.
Shaw's scholarship metrics include an h-index of 19, 120 total publications, and 1,642 total citations. He has collaborated with several University of Arkansas faculty members, including José Silvestre (7 shared publications), Glenn R. Sharman (5 shared publications), C. M. Hughes (3 shared publications), and Barry Shaulis (2 shared publications).
Metrics
- h-index: 19
- Publications: 120
- Citations: 1,670
Selected Publications
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Variable Flood Discharge Constrains Autochthonous Organic Carbon Preservation in Deltas: Insights From Physical Experiments (2026)
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Basin confinement influences river delta elevation profiles (2025)
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Stratigraphic Evidence of Backwater Morphodynamics and Lowland River Deltas in the Northern Hemisphere of Mars (2025)
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Ancient Channel-Mouth Bifurcation Angles on Earth and Mars (2024)
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Goldilocks Fluctuations: Dynamic Constraints on Loop Formation in Scale-Free Transport Networks (2024)
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Sediment Compaction in Experimental Deltas: Toward a Meso‐Scale Understanding of Coastal Subsidence Patterns (2023)
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Marsh-induced backwater: the influence of non-fluvial sedimentation on a delta's channel morphology and kinematics (2023)
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Comment on egusphere-2023-545 (2023)
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General comment on egusphere-2023-545 (2023)
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Coastal response to global warming during the Paleocene-Eocene Thermal Maximum (2023)
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Marsh induced backwater: the influence of non-fluvial sedimentation on a delta's channel morphology and kinematics (2023)
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Supplementary Data for "Interplay of river and tidal forcings promotes loops in coastal channel networks" (2022)
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Supplementary Data for "Interplay of river and tidal forcings promotes loops in coastal channel networks" (2022)
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Significant Human Modification of the Lower Arkansas River Sediment Budget (2022)
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Marsh Sedimentation Controls Delta Top Morphology, Slope, and Mass Balance (2022)
Collaboration Network
Top Collaborators
- Marsh Sedimentation Controls Delta Top Morphology, Slope, and Mass Balance
- Marsh-induced backwater: the influence of non-fluvial sedimentation on a delta's channel morphology and kinematics
- Sediment Compaction in Experimental Deltas: Toward a Meso‐Scale Understanding of Coastal Subsidence Patterns
- Basin confinement influences river delta elevation profiles
- Marsh sedimentation controls delta top morphology, slope, and mass balance
Showing 5 of 9 shared publications
- Marsh Sedimentation Controls Delta Top Morphology, Slope, and Mass Balance
- Marsh-induced backwater: the influence of non-fluvial sedimentation on a delta's channel morphology and kinematics
- Sediment Compaction in Experimental Deltas: Toward a Meso‐Scale Understanding of Coastal Subsidence Patterns
- Marsh sedimentation controls delta top morphology, slope, and mass balance
- Marsh-Delta Interactions: The strong influence of marsh deposition on delta slopes and mass partitioning
Showing 5 of 9 shared publications
- Marsh Sedimentation Controls Delta Top Morphology, Slope, and Mass Balance
- Marsh-induced backwater: the influence of non-fluvial sedimentation on a delta's channel morphology and kinematics
- Sediment Compaction in Experimental Deltas: Toward a Meso‐Scale Understanding of Coastal Subsidence Patterns
- Marsh sedimentation controls delta top morphology, slope, and mass balance
- Marsh induced backwater: the influence of non-fluvial sedimentation on a delta's channel morphology and kinematics
Showing 5 of 8 shared publications
- Marsh Sedimentation Controls Delta Top Morphology, Slope, and Mass Balance
- Marsh-induced backwater: the influence of non-fluvial sedimentation on a delta's channel morphology and kinematics
- Sediment Compaction in Experimental Deltas: Toward a Meso‐Scale Understanding of Coastal Subsidence Patterns
- Marsh sedimentation controls delta top morphology, slope, and mass balance
- Marsh-Delta Interactions: The strong influence of marsh deposition on delta slopes and mass partitioning
Showing 5 of 8 shared publications
- Marsh Sedimentation Controls Delta Top Morphology, Slope, and Mass Balance
- Marsh-induced backwater: the influence of non-fluvial sedimentation on a delta's channel morphology and kinematics
- Sediment Compaction in Experimental Deltas: Toward a Meso‐Scale Understanding of Coastal Subsidence Patterns
- Marsh sedimentation controls delta top morphology, slope, and mass balance
- Marsh-Delta Interactions: The strong influence of marsh deposition on delta slopes and mass partitioning
Showing 5 of 7 shared publications
- Coastal response to global warming during the Paleocene-Eocene Thermal Maximum
- Significant Human Modification of the Lower Arkansas River Sediment Budget
- Significant Human Modification of the Lower Arkansas River Sediment Budget
- Significant Human Modification of the Lower Arkansas River Sediment Budget
- Coastal Response to Global Warming During the Paleocene-Eocene Thermal Maximum
- Significant Human Modification of the Lower Arkansas River Sediment Budget
- Significant Human Modification of the Lower Arkansas River Sediment Budget
- Ancient Channel-Mouth Bifurcation Angles on Earth and Mars
- Significant Human Modification of the Lower Arkansas River Sediment Budget
- Interplay of River and Tidal Forcings Promotes Loops in Coastal Channel Networks
- Supplementary Data for "Interplay of river and tidal forcings promotes loops in coastal channel networks"
- Supplementary Data for "Interplay of river and tidal forcings promotes loops in coastal channel networks"
- Interplay of River and Tidal Forcings Promotes Loops in Coastal Channel Networks
- Supplementary Data for "Interplay of river and tidal forcings promotes loops in coastal channel networks"
- Supplementary Data for "Interplay of river and tidal forcings promotes loops in coastal channel networks"
- Interplay of River and Tidal Forcings Promotes Loops in Coastal Channel Networks
- Supplementary Data for "Interplay of river and tidal forcings promotes loops in coastal channel networks"
- Supplementary Data for "Interplay of river and tidal forcings promotes loops in coastal channel networks"
- Ancient Channel-Mouth Bifurcation Angles on Earth and Mars
- Stratigraphic Evidence of Backwater Morphodynamics and Lowland River Deltas in the Northern Hemisphere of Mars
- River Delta Truck Channel Deposit Preserved in Inverted Relief, Weddington, Arkansas
- Significant Human Modification of the Lower Arkansas River Sediment Budget
- Significant Human Modification of the Lower Arkansas River Sediment Budget
- Significant Human Modification of the Lower Arkansas River Sediment Budget
- Morphodynamic Modeling of River-Dominated Deltas: A Review and Future Perspectives
- Morphodynamic Modeling of River-Dominated Deltas: A Review and Future Perspectives
- Morphodynamic Modeling of River-Dominated Deltas: A Review and Future Perspectives
- Morphodynamic Modeling of River-Dominated Deltas: A Review and Future Perspectives
- Morphodynamic Modeling of River-Dominated Deltas: A Review and Future Perspectives
- Morphodynamic Modeling of River-Dominated Deltas: A Review and Future Perspectives
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