Transport-limited fluvial erosion – simple formulation and efficient numerical treatment

<p>Most of the recent studies modeling fluvial erosion in the context of tectonic geomorphology focus on the detachment-limited regime. One reason for this simplification is the simple relationship of the constitutive law used here – often called stream-power law – to empirical results on long...

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Main Author: S. Hergarten
Format: Article
Language:English
Published: Copernicus Publications 2020-10-01
Series:Earth Surface Dynamics
Online Access:https://esurf.copernicus.org/articles/8/841/2020/esurf-8-841-2020.pdf
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spelling doaj-6390177223324247bce6085f6d6c4ccc2020-11-25T03:59:35ZengCopernicus PublicationsEarth Surface Dynamics2196-63112196-632X2020-10-01884185410.5194/esurf-8-841-2020Transport-limited fluvial erosion – simple formulation and efficient numerical treatmentS. Hergarten<p>Most of the recent studies modeling fluvial erosion in the context of tectonic geomorphology focus on the detachment-limited regime. One reason for this simplification is the simple relationship of the constitutive law used here – often called stream-power law – to empirical results on longitudinal river profiles. Another no less important reason lies in the numerical effort that is much higher for transport-limited models than for detachment-limited models. This study proposes a formulation of transport-limited erosion where the relationship to empirical results on river profiles is almost as simple as it is for the stream-power law. As a central point, a direct solver for the fully implicit scheme is presented. This solver requires no iteration for the linear version of the model, allows for arbitrarily large time increments, and is almost as efficient as the established implicit solver for detachment-limited erosion. The numerical scheme can also be applied to linear hybrid models that cover the range between the two end-members of detachment-limited and transport-limited erosion.</p>https://esurf.copernicus.org/articles/8/841/2020/esurf-8-841-2020.pdf
collection DOAJ
language English
format Article
sources DOAJ
author S. Hergarten
spellingShingle S. Hergarten
Transport-limited fluvial erosion – simple formulation and efficient numerical treatment
Earth Surface Dynamics
author_facet S. Hergarten
author_sort S. Hergarten
title Transport-limited fluvial erosion – simple formulation and efficient numerical treatment
title_short Transport-limited fluvial erosion – simple formulation and efficient numerical treatment
title_full Transport-limited fluvial erosion – simple formulation and efficient numerical treatment
title_fullStr Transport-limited fluvial erosion – simple formulation and efficient numerical treatment
title_full_unstemmed Transport-limited fluvial erosion – simple formulation and efficient numerical treatment
title_sort transport-limited fluvial erosion – simple formulation and efficient numerical treatment
publisher Copernicus Publications
series Earth Surface Dynamics
issn 2196-6311
2196-632X
publishDate 2020-10-01
description <p>Most of the recent studies modeling fluvial erosion in the context of tectonic geomorphology focus on the detachment-limited regime. One reason for this simplification is the simple relationship of the constitutive law used here – often called stream-power law – to empirical results on longitudinal river profiles. Another no less important reason lies in the numerical effort that is much higher for transport-limited models than for detachment-limited models. This study proposes a formulation of transport-limited erosion where the relationship to empirical results on river profiles is almost as simple as it is for the stream-power law. As a central point, a direct solver for the fully implicit scheme is presented. This solver requires no iteration for the linear version of the model, allows for arbitrarily large time increments, and is almost as efficient as the established implicit solver for detachment-limited erosion. The numerical scheme can also be applied to linear hybrid models that cover the range between the two end-members of detachment-limited and transport-limited erosion.</p>
url https://esurf.copernicus.org/articles/8/841/2020/esurf-8-841-2020.pdf
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