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Shredding of environmental signals by sediment transport
by
Paola, Chris
, Jerolmack, Douglas J.
in
Avulsion
/ Bed load
/ Climate change
/ Computational fluid dynamics
/ Earth sciences
/ Earth, ocean, space
/ Exact sciences and technology
/ Fluid flow
/ fractal
/ Geomorphology
/ Geophysics
/ Hydrology
/ Landscapes
/ Mathematical models
/ Mathematics
/ Nonlinear systems
/ Paleoclimate
/ Sediment load
/ Sediment transport
/ self-organized criticality
/ sequence stratigraphy
/ stochastic
/ Stochastic models
/ Stratigraphy
/ Tectonics
/ Turbulence
/ Turbulent flow
2010
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Shredding of environmental signals by sediment transport
by
Paola, Chris
, Jerolmack, Douglas J.
in
Avulsion
/ Bed load
/ Climate change
/ Computational fluid dynamics
/ Earth sciences
/ Earth, ocean, space
/ Exact sciences and technology
/ Fluid flow
/ fractal
/ Geomorphology
/ Geophysics
/ Hydrology
/ Landscapes
/ Mathematical models
/ Mathematics
/ Nonlinear systems
/ Paleoclimate
/ Sediment load
/ Sediment transport
/ self-organized criticality
/ sequence stratigraphy
/ stochastic
/ Stochastic models
/ Stratigraphy
/ Tectonics
/ Turbulence
/ Turbulent flow
2010
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Shredding of environmental signals by sediment transport
by
Paola, Chris
, Jerolmack, Douglas J.
in
Avulsion
/ Bed load
/ Climate change
/ Computational fluid dynamics
/ Earth sciences
/ Earth, ocean, space
/ Exact sciences and technology
/ Fluid flow
/ fractal
/ Geomorphology
/ Geophysics
/ Hydrology
/ Landscapes
/ Mathematical models
/ Mathematics
/ Nonlinear systems
/ Paleoclimate
/ Sediment load
/ Sediment transport
/ self-organized criticality
/ sequence stratigraphy
/ stochastic
/ Stochastic models
/ Stratigraphy
/ Tectonics
/ Turbulence
/ Turbulent flow
2010
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Journal Article
Shredding of environmental signals by sediment transport
2010
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Overview
Landscapes respond to climate, tectonic motions and sea level, but this response is mediated by sediment transport. Understanding transmission of environmental signals is crucial for predicting landscape response to climate change, and interpreting paleo‐climate and tectonics from stratigraphy. Here we propose that sediment transport can act as a nonlinear filter that completely destroys (“shreds”) environmental signals. This results from ubiquitous thresholds in sediment transport systems; e.g., landsliding, bed load transport, and river avulsion. This “morphodynamic turbulence” is analogous to turbulence in fluid flows, where energy injected at one frequency is smeared across a range of scales. We show with a numerical model that external signals are shredded when their time and amplitude scales fall within the ranges of morphodynamic turbulence. As signal frequency increases, signal preservation becomes the exception rather than the rule, suggesting a critical re‐examination of purported sedimentary signals of external forcing.
Publisher
Blackwell Publishing Ltd,American Geophysical Union,John Wiley & Sons, Inc
Subject
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