Fluvial and oceanographic influences on suspended sediment dispersal in the Magdalena River Estuary

The Magdalena River is the main contributor of fresh water and sediment to the Caribbean Sea. Hydrological inputs from the Magdalena River are 10,287 and 4068 m3 s−1 at high and low flows, respectively. Sediment delivery from the Magdalena River is among the largest in the world, with 142 × 106 t yr...

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Autores:
Torregroza Espinosa, Ana Carolina
Restrepo, Juan Camilo
Correa-Metrio, Alexander
Hoyos, Natalia
Escobar, Jaime
Pierini, Jorge
Martinez, Jean-Michel
Tipo de recurso:
http://purl.org/coar/resource_type/c_816b
Fecha de publicación:
2019
Institución:
Corporación Universidad de la Costa
Repositorio:
REDICUC - Repositorio CUC
Idioma:
OAI Identifier:
oai:repositorio.cuc.edu.co:11323/5997
Acceso en línea:
https://hdl.handle.net/11323/5997
https://repositorio.cuc.edu.co/
Palabra clave:
Remote sensing
Sediment transport
Turbid plume
MODIS
Magdalena River
Rights
openAccess
License
CC0 1.0 Universal
id RCUC2_6fc6a2e48023d86194b39c82d004e6f1
oai_identifier_str oai:repositorio.cuc.edu.co:11323/5997
network_acronym_str RCUC2
network_name_str REDICUC - Repositorio CUC
repository_id_str
dc.title.spa.fl_str_mv Fluvial and oceanographic influences on suspended sediment dispersal in the Magdalena River Estuary
title Fluvial and oceanographic influences on suspended sediment dispersal in the Magdalena River Estuary
spellingShingle Fluvial and oceanographic influences on suspended sediment dispersal in the Magdalena River Estuary
Remote sensing
Sediment transport
Turbid plume
MODIS
Magdalena River
title_short Fluvial and oceanographic influences on suspended sediment dispersal in the Magdalena River Estuary
title_full Fluvial and oceanographic influences on suspended sediment dispersal in the Magdalena River Estuary
title_fullStr Fluvial and oceanographic influences on suspended sediment dispersal in the Magdalena River Estuary
title_full_unstemmed Fluvial and oceanographic influences on suspended sediment dispersal in the Magdalena River Estuary
title_sort Fluvial and oceanographic influences on suspended sediment dispersal in the Magdalena River Estuary
dc.creator.fl_str_mv Torregroza Espinosa, Ana Carolina
Restrepo, Juan Camilo
Correa-Metrio, Alexander
Hoyos, Natalia
Escobar, Jaime
Pierini, Jorge
Martinez, Jean-Michel
dc.contributor.author.spa.fl_str_mv Torregroza Espinosa, Ana Carolina
Restrepo, Juan Camilo
Correa-Metrio, Alexander
Hoyos, Natalia
Escobar, Jaime
Pierini, Jorge
Martinez, Jean-Michel
dc.subject.spa.fl_str_mv Remote sensing
Sediment transport
Turbid plume
MODIS
Magdalena River
topic Remote sensing
Sediment transport
Turbid plume
MODIS
Magdalena River
description The Magdalena River is the main contributor of fresh water and sediment to the Caribbean Sea. Hydrological inputs from the Magdalena River are 10,287 and 4068 m3 s−1 at high and low flows, respectively. Sediment delivery from the Magdalena River is among the largest in the world, with 142 × 106 t yr−1 of transported suspended matter. We used MODIS images to develop a regional model and assess the spatial and temporal variability of suspended sediment concentration at the mouth of the Magdalena River, map the extent of the turbidity plume using its morphometric properties, and identify the main fluvial and oceanographic factors associated with plume variability. We analyzed monthly average suspended sediment concentration data for the period 2003–2017. MODIS images were calibrated with in situ measurements of suspended sediment concentrations in surface waters of the study area. A finite mixing model was used to identify turbidity thresholds and define areas within the plume. Calculated suspended sediment concentrations indicate high turbidity in the Magdalena River mouth (178.6 } 78.7 mg L−1), values that are of the same order of magnitude as those measured in the Yangtze, Huang He and Amazon River mouths. Calculated plume areas (diffuse, solid and mixing) and their shapes suggest that the Magdalena River plume has a limited area, related to conditions such as wind speed and direction, streamflow, and sediment transport. Calculated areas and shapes demonstrate the ability to generate a near-field area, which indicates the presence of a clear convergence front. The data also emphasize the importance of sediment transport from the Magdalena River to the Caribbean Sea. Such fluvial transport is important in the biogeochemistry of estuarine systems, especially in turbid estuaries, where there is marked variability in the distribution of sediment in surface waters.
publishDate 2019
dc.date.issued.none.fl_str_mv 2019-12-16
dc.date.accessioned.none.fl_str_mv 2020-02-05T16:46:00Z
dc.date.available.none.fl_str_mv 2020-02-05T16:46:00Z
dc.type.spa.fl_str_mv Pre-Publicación
dc.type.coar.spa.fl_str_mv http://purl.org/coar/resource_type/c_816b
dc.type.content.spa.fl_str_mv Text
dc.type.driver.spa.fl_str_mv info:eu-repo/semantics/preprint
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dc.type.version.spa.fl_str_mv info:eu-repo/semantics/acceptedVersion
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status_str acceptedVersion
dc.identifier.uri.spa.fl_str_mv https://hdl.handle.net/11323/5997
dc.identifier.instname.spa.fl_str_mv Corporación Universidad de la Costa
dc.identifier.reponame.spa.fl_str_mv REDICUC - Repositorio CUC
dc.identifier.repourl.spa.fl_str_mv https://repositorio.cuc.edu.co/
url https://hdl.handle.net/11323/5997
https://repositorio.cuc.edu.co/
identifier_str_mv Corporación Universidad de la Costa
REDICUC - Repositorio CUC
dc.rights.spa.fl_str_mv CC0 1.0 Universal
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dc.publisher.spa.fl_str_mv Universidad de la Costa
institution Corporación Universidad de la Costa
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spelling Torregroza Espinosa, Ana CarolinaRestrepo, Juan CamiloCorrea-Metrio, AlexanderHoyos, NataliaEscobar, JaimePierini, JorgeMartinez, Jean-Michel2020-02-05T16:46:00Z2020-02-05T16:46:00Z2019-12-16https://hdl.handle.net/11323/5997Corporación Universidad de la CostaREDICUC - Repositorio CUChttps://repositorio.cuc.edu.co/The Magdalena River is the main contributor of fresh water and sediment to the Caribbean Sea. Hydrological inputs from the Magdalena River are 10,287 and 4068 m3 s−1 at high and low flows, respectively. Sediment delivery from the Magdalena River is among the largest in the world, with 142 × 106 t yr−1 of transported suspended matter. We used MODIS images to develop a regional model and assess the spatial and temporal variability of suspended sediment concentration at the mouth of the Magdalena River, map the extent of the turbidity plume using its morphometric properties, and identify the main fluvial and oceanographic factors associated with plume variability. We analyzed monthly average suspended sediment concentration data for the period 2003–2017. MODIS images were calibrated with in situ measurements of suspended sediment concentrations in surface waters of the study area. A finite mixing model was used to identify turbidity thresholds and define areas within the plume. Calculated suspended sediment concentrations indicate high turbidity in the Magdalena River mouth (178.6 } 78.7 mg L−1), values that are of the same order of magnitude as those measured in the Yangtze, Huang He and Amazon River mouths. Calculated plume areas (diffuse, solid and mixing) and their shapes suggest that the Magdalena River plume has a limited area, related to conditions such as wind speed and direction, streamflow, and sediment transport. Calculated areas and shapes demonstrate the ability to generate a near-field area, which indicates the presence of a clear convergence front. The data also emphasize the importance of sediment transport from the Magdalena River to the Caribbean Sea. Such fluvial transport is important in the biogeochemistry of estuarine systems, especially in turbid estuaries, where there is marked variability in the distribution of sediment in surface waters.Torregroza Espinosa, Ana Carolina-will be generated-orcid-0000-0001-8077-8880-600Restrepo, Juan CamiloCorrea-Metrio, Alexander-will be generated-orcid-0000-0002-1278-2746-600Hoyos, NataliaEscobar, JaimePierini, Jorge-will be generated-orcid-0000-0002-3004-8334-600Martinez, Jean-Michel-will be generated-orcid-0000-0003-3281-8512-600Universidad de la CostaCC0 1.0 Universalhttp://creativecommons.org/publicdomain/zero/1.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Remote sensingSediment transportTurbid plumeMODISMagdalena RiverFluvial and oceanographic influences on suspended sediment dispersal in the Magdalena River EstuaryPre-Publicaciónhttp://purl.org/coar/resource_type/c_816bTextinfo:eu-repo/semantics/preprinthttp://purl.org/redcol/resource_type/ARTOTRinfo:eu-repo/semantics/acceptedVersionPublicationORIGINALFluvial and oceanographic influences on suspended sediment dispersal in the Magdalena River Estuary.pdfFluvial and oceanographic influences on suspended sediment dispersal in the Magdalena River Estuary.pdfapplication/pdf64867https://repositorio.cuc.edu.co/bitstreams/b1a68d82-5f3c-4d73-8eef-2ca715be3ce4/downloadd6dcc6a2fb3ade7a8c5520ab5a612eafMD51CC-LICENSElicense_rdflicense_rdfapplication/rdf+xml; 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