Morphology of the Kosi megafan channels

We report on a new set of measurements on the morphology of braided and meandering threads of the Kosi megafan, North Bihar, India. All threads develop on a uniform sandy sediment and under a similar climate. The data set is composed of the width, depth, water discharge and grain size of 51 threads....

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Main Authors: K. Gaurav, F. Métivier, O. Devauchelle, R. Sinha, H. Chauvet, M. Houssais, H. Bouquerel
Format: Article
Language:English
Published: Copernicus Publications 2015-07-01
Series:Earth Surface Dynamics
Online Access:http://www.earth-surf-dynam.net/3/321/2015/esurf-3-321-2015.pdf
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spelling doaj-223b9a67eeac4019a6b6ec7822e0516f2020-11-25T00:15:11ZengCopernicus PublicationsEarth Surface Dynamics2196-63112196-632X2015-07-013332133110.5194/esurf-3-321-2015Morphology of the Kosi megafan channelsK. Gaurav0F. Métivier1O. Devauchelle2R. Sinha3H. Chauvet4M. Houssais5H. Bouquerel6Institute de Physique du Globe de Paris, 1 Rue Jussieu, 75005 Paris CEDEX 05, FranceInstitute de Physique du Globe de Paris, 1 Rue Jussieu, 75005 Paris CEDEX 05, FranceInstitute de Physique du Globe de Paris, 1 Rue Jussieu, 75005 Paris CEDEX 05, FranceDepartment of Earth Sciences, Indian Institute of Technology, Kanpur, 208016 UP, IndiaInstitute de Physique du Globe de Paris, 1 Rue Jussieu, 75005 Paris CEDEX 05, FranceDepartment of Earth and Environmental Science, University of Pennsylvania, Philadelphia, PA 19104, USAInstitute de Physique du Globe de Paris, 1 Rue Jussieu, 75005 Paris CEDEX 05, FranceWe report on a new set of measurements on the morphology of braided and meandering threads of the Kosi megafan, North Bihar, India. All threads develop on a uniform sandy sediment and under a similar climate. The data set is composed of the width, depth, water discharge and grain size of 51 threads. Downstream slopes and sinuosity are also available. Using this data set, we show that braided and meandering threads share common hydraulic geometries. We then use the threshold theory to explain why the aspect ratio of threads is almost naturally detrended, and rescale the data according to this theory. As expected, the rescaled dimensions of braided and meandering threads are weakly correlated to water discharge. We propose that the large dispersion observed, which is common to meandering and braided threads, is the signature of sediment transport, vegetation or cohesion effects.http://www.earth-surf-dynam.net/3/321/2015/esurf-3-321-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author K. Gaurav
F. Métivier
O. Devauchelle
R. Sinha
H. Chauvet
M. Houssais
H. Bouquerel
spellingShingle K. Gaurav
F. Métivier
O. Devauchelle
R. Sinha
H. Chauvet
M. Houssais
H. Bouquerel
Morphology of the Kosi megafan channels
Earth Surface Dynamics
author_facet K. Gaurav
F. Métivier
O. Devauchelle
R. Sinha
H. Chauvet
M. Houssais
H. Bouquerel
author_sort K. Gaurav
title Morphology of the Kosi megafan channels
title_short Morphology of the Kosi megafan channels
title_full Morphology of the Kosi megafan channels
title_fullStr Morphology of the Kosi megafan channels
title_full_unstemmed Morphology of the Kosi megafan channels
title_sort morphology of the kosi megafan channels
publisher Copernicus Publications
series Earth Surface Dynamics
issn 2196-6311
2196-632X
publishDate 2015-07-01
description We report on a new set of measurements on the morphology of braided and meandering threads of the Kosi megafan, North Bihar, India. All threads develop on a uniform sandy sediment and under a similar climate. The data set is composed of the width, depth, water discharge and grain size of 51 threads. Downstream slopes and sinuosity are also available. Using this data set, we show that braided and meandering threads share common hydraulic geometries. We then use the threshold theory to explain why the aspect ratio of threads is almost naturally detrended, and rescale the data according to this theory. As expected, the rescaled dimensions of braided and meandering threads are weakly correlated to water discharge. We propose that the large dispersion observed, which is common to meandering and braided threads, is the signature of sediment transport, vegetation or cohesion effects.
url http://www.earth-surf-dynam.net/3/321/2015/esurf-3-321-2015.pdf
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AT hchauvet morphologyofthekosimegafanchannels
AT mhoussais morphologyofthekosimegafanchannels
AT hbouquerel morphologyofthekosimegafanchannels
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