Morphology and flow fields of three-dimensional dunes, Rio Paraná, Argentina: Results from simultaneous multibeam echo sounding and acoustic Doppler current profiling

Autores
Parsons, Daniel R.; Best, James L.; Orfeo, Oscar; Hardy, Richard J.; Kostaschuk, R.; Lane, Stuart N.
Año de publicación
2005
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
[1] Most past studies of river dune dynamics have concentrated on two-dimensional (2-D) bed forms, with constant heights and straight crest lines transverse to the flow, and their associated turbulent flow structure. This morphological simplification imposes inherent limitations on the interpretation and understanding of dune form and flow dynamics in natural channels, where dune form is predominantly three-dimensional. For example, studies over 2-D forms neglect the significant influence that lateral flows and secondary circulation may have on the flow structure and thus dune morphology. This paper details a field study of a swath of 3-D dunes in the Rio Paraná, Argentina. A large (0.35 km wide, 1.2 km long) area of dunes was surveyed using a multibeam echo sounder (MBES) that provided high-resolution 3-D detail of the river bed. Simultaneous with the MBES survey, 3-D flow information was obtained with an acoustic Doppler current profiler (ADCP), revealing a complicated pattern of dune morphology and associated flow structure within the swath. Dune three-dimensionality appears intimately connected to the morphology of the upstream dune, with changes in crest line curvature and crest line bifurcations/junctions significantly influencing the downstream dune form. Dunes with lobe or saddle-shaped crest lines were found to have larger, more structured regions of vertical velocity with smaller separation zones than more 2-D straight-crested dunes. These results represent the first integrated study of 3-D dune form and mean flow structure from the field and show several similarities to recent laboratory models of flow over 3-D dunes. Copyright 2005 by the American Geophysical Union.
Fil: Parsons, Daniel R.. University Of Leeds;
Fil: Best, James L.. University Of Leeds;
Fil: Orfeo, Oscar. Centro de Ecologica Applicada del Littoral; Argentina
Fil: Hardy, Richard J.. University Of Durham; Reino Unido
Fil: Kostaschuk, R.. University of Guelph; Canadá
Fil: Lane, Stuart N.. University Of Durham; Reino Unido
Materia
multibeam echo sounder (MBES)
acoustic Doppler current profiler (ADCP)
Rio Paraná
Argentina
river dune dynamics
dinámica de las dunas fluviales
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/56361

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network_name_str CONICET Digital (CONICET)
spelling Morphology and flow fields of three-dimensional dunes, Rio Paraná, Argentina: Results from simultaneous multibeam echo sounding and acoustic Doppler current profilingParsons, Daniel R.Best, James L.Orfeo, OscarHardy, Richard J.Kostaschuk, R.Lane, Stuart N.multibeam echo sounder (MBES)acoustic Doppler current profiler (ADCP)Rio ParanáArgentinariver dune dynamicsdinámica de las dunas fluvialeshttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1[1] Most past studies of river dune dynamics have concentrated on two-dimensional (2-D) bed forms, with constant heights and straight crest lines transverse to the flow, and their associated turbulent flow structure. This morphological simplification imposes inherent limitations on the interpretation and understanding of dune form and flow dynamics in natural channels, where dune form is predominantly three-dimensional. For example, studies over 2-D forms neglect the significant influence that lateral flows and secondary circulation may have on the flow structure and thus dune morphology. This paper details a field study of a swath of 3-D dunes in the Rio Paraná, Argentina. A large (0.35 km wide, 1.2 km long) area of dunes was surveyed using a multibeam echo sounder (MBES) that provided high-resolution 3-D detail of the river bed. Simultaneous with the MBES survey, 3-D flow information was obtained with an acoustic Doppler current profiler (ADCP), revealing a complicated pattern of dune morphology and associated flow structure within the swath. Dune three-dimensionality appears intimately connected to the morphology of the upstream dune, with changes in crest line curvature and crest line bifurcations/junctions significantly influencing the downstream dune form. Dunes with lobe or saddle-shaped crest lines were found to have larger, more structured regions of vertical velocity with smaller separation zones than more 2-D straight-crested dunes. These results represent the first integrated study of 3-D dune form and mean flow structure from the field and show several similarities to recent laboratory models of flow over 3-D dunes. Copyright 2005 by the American Geophysical Union.Fil: Parsons, Daniel R.. University Of Leeds;Fil: Best, James L.. University Of Leeds;Fil: Orfeo, Oscar. Centro de Ecologica Applicada del Littoral; ArgentinaFil: Hardy, Richard J.. University Of Durham; Reino UnidoFil: Kostaschuk, R.. University of Guelph; CanadáFil: Lane, Stuart N.. University Of Durham; Reino UnidoBlackwell Publishing Ltd2005-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/56361Parsons, Daniel R.; Best, James L.; Orfeo, Oscar; Hardy, Richard J.; Kostaschuk, R.; et al.; Morphology and flow fields of three-dimensional dunes, Rio Paraná, Argentina: Results from simultaneous multibeam echo sounding and acoustic Doppler current profiling; Blackwell Publishing Ltd; Journal of Geophysical Research: Earth Surface; 110; 4; 12-2005; 1-92169-9011CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1029/2004JF000231info:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2004JF000231info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-22T11:57:27Zoai:ri.conicet.gov.ar:11336/56361instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-10-22 11:57:27.241CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Morphology and flow fields of three-dimensional dunes, Rio Paraná, Argentina: Results from simultaneous multibeam echo sounding and acoustic Doppler current profiling
title Morphology and flow fields of three-dimensional dunes, Rio Paraná, Argentina: Results from simultaneous multibeam echo sounding and acoustic Doppler current profiling
spellingShingle Morphology and flow fields of three-dimensional dunes, Rio Paraná, Argentina: Results from simultaneous multibeam echo sounding and acoustic Doppler current profiling
Parsons, Daniel R.
multibeam echo sounder (MBES)
acoustic Doppler current profiler (ADCP)
Rio Paraná
Argentina
river dune dynamics
dinámica de las dunas fluviales
title_short Morphology and flow fields of three-dimensional dunes, Rio Paraná, Argentina: Results from simultaneous multibeam echo sounding and acoustic Doppler current profiling
title_full Morphology and flow fields of three-dimensional dunes, Rio Paraná, Argentina: Results from simultaneous multibeam echo sounding and acoustic Doppler current profiling
title_fullStr Morphology and flow fields of three-dimensional dunes, Rio Paraná, Argentina: Results from simultaneous multibeam echo sounding and acoustic Doppler current profiling
title_full_unstemmed Morphology and flow fields of three-dimensional dunes, Rio Paraná, Argentina: Results from simultaneous multibeam echo sounding and acoustic Doppler current profiling
title_sort Morphology and flow fields of three-dimensional dunes, Rio Paraná, Argentina: Results from simultaneous multibeam echo sounding and acoustic Doppler current profiling
dc.creator.none.fl_str_mv Parsons, Daniel R.
Best, James L.
Orfeo, Oscar
Hardy, Richard J.
Kostaschuk, R.
Lane, Stuart N.
author Parsons, Daniel R.
author_facet Parsons, Daniel R.
Best, James L.
Orfeo, Oscar
Hardy, Richard J.
Kostaschuk, R.
Lane, Stuart N.
author_role author
author2 Best, James L.
Orfeo, Oscar
Hardy, Richard J.
Kostaschuk, R.
Lane, Stuart N.
author2_role author
author
author
author
author
dc.subject.none.fl_str_mv multibeam echo sounder (MBES)
acoustic Doppler current profiler (ADCP)
Rio Paraná
Argentina
river dune dynamics
dinámica de las dunas fluviales
topic multibeam echo sounder (MBES)
acoustic Doppler current profiler (ADCP)
Rio Paraná
Argentina
river dune dynamics
dinámica de las dunas fluviales
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv [1] Most past studies of river dune dynamics have concentrated on two-dimensional (2-D) bed forms, with constant heights and straight crest lines transverse to the flow, and their associated turbulent flow structure. This morphological simplification imposes inherent limitations on the interpretation and understanding of dune form and flow dynamics in natural channels, where dune form is predominantly three-dimensional. For example, studies over 2-D forms neglect the significant influence that lateral flows and secondary circulation may have on the flow structure and thus dune morphology. This paper details a field study of a swath of 3-D dunes in the Rio Paraná, Argentina. A large (0.35 km wide, 1.2 km long) area of dunes was surveyed using a multibeam echo sounder (MBES) that provided high-resolution 3-D detail of the river bed. Simultaneous with the MBES survey, 3-D flow information was obtained with an acoustic Doppler current profiler (ADCP), revealing a complicated pattern of dune morphology and associated flow structure within the swath. Dune three-dimensionality appears intimately connected to the morphology of the upstream dune, with changes in crest line curvature and crest line bifurcations/junctions significantly influencing the downstream dune form. Dunes with lobe or saddle-shaped crest lines were found to have larger, more structured regions of vertical velocity with smaller separation zones than more 2-D straight-crested dunes. These results represent the first integrated study of 3-D dune form and mean flow structure from the field and show several similarities to recent laboratory models of flow over 3-D dunes. Copyright 2005 by the American Geophysical Union.
Fil: Parsons, Daniel R.. University Of Leeds;
Fil: Best, James L.. University Of Leeds;
Fil: Orfeo, Oscar. Centro de Ecologica Applicada del Littoral; Argentina
Fil: Hardy, Richard J.. University Of Durham; Reino Unido
Fil: Kostaschuk, R.. University of Guelph; Canadá
Fil: Lane, Stuart N.. University Of Durham; Reino Unido
description [1] Most past studies of river dune dynamics have concentrated on two-dimensional (2-D) bed forms, with constant heights and straight crest lines transverse to the flow, and their associated turbulent flow structure. This morphological simplification imposes inherent limitations on the interpretation and understanding of dune form and flow dynamics in natural channels, where dune form is predominantly three-dimensional. For example, studies over 2-D forms neglect the significant influence that lateral flows and secondary circulation may have on the flow structure and thus dune morphology. This paper details a field study of a swath of 3-D dunes in the Rio Paraná, Argentina. A large (0.35 km wide, 1.2 km long) area of dunes was surveyed using a multibeam echo sounder (MBES) that provided high-resolution 3-D detail of the river bed. Simultaneous with the MBES survey, 3-D flow information was obtained with an acoustic Doppler current profiler (ADCP), revealing a complicated pattern of dune morphology and associated flow structure within the swath. Dune three-dimensionality appears intimately connected to the morphology of the upstream dune, with changes in crest line curvature and crest line bifurcations/junctions significantly influencing the downstream dune form. Dunes with lobe or saddle-shaped crest lines were found to have larger, more structured regions of vertical velocity with smaller separation zones than more 2-D straight-crested dunes. These results represent the first integrated study of 3-D dune form and mean flow structure from the field and show several similarities to recent laboratory models of flow over 3-D dunes. Copyright 2005 by the American Geophysical Union.
publishDate 2005
dc.date.none.fl_str_mv 2005-12
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/56361
Parsons, Daniel R.; Best, James L.; Orfeo, Oscar; Hardy, Richard J.; Kostaschuk, R.; et al.; Morphology and flow fields of three-dimensional dunes, Rio Paraná, Argentina: Results from simultaneous multibeam echo sounding and acoustic Doppler current profiling; Blackwell Publishing Ltd; Journal of Geophysical Research: Earth Surface; 110; 4; 12-2005; 1-9
2169-9011
CONICET Digital
CONICET
url http://hdl.handle.net/11336/56361
identifier_str_mv Parsons, Daniel R.; Best, James L.; Orfeo, Oscar; Hardy, Richard J.; Kostaschuk, R.; et al.; Morphology and flow fields of three-dimensional dunes, Rio Paraná, Argentina: Results from simultaneous multibeam echo sounding and acoustic Doppler current profiling; Blackwell Publishing Ltd; Journal of Geophysical Research: Earth Surface; 110; 4; 12-2005; 1-9
2169-9011
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1029/2004JF000231
info:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2004JF000231
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Blackwell Publishing Ltd
publisher.none.fl_str_mv Blackwell Publishing Ltd
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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