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...
- 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 |
dc.type.redcol.spa.fl_str_mv |
http://purl.org/redcol/resource_type/ARTOTR |
dc.type.version.spa.fl_str_mv |
info:eu-repo/semantics/acceptedVersion |
format |
http://purl.org/coar/resource_type/c_816b |
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 |
dc.rights.uri.spa.fl_str_mv |
http://creativecommons.org/publicdomain/zero/1.0/ |
dc.rights.accessrights.spa.fl_str_mv |
info:eu-repo/semantics/openAccess |
dc.rights.coar.spa.fl_str_mv |
http://purl.org/coar/access_right/c_abf2 |
rights_invalid_str_mv |
CC0 1.0 Universal http://creativecommons.org/publicdomain/zero/1.0/ http://purl.org/coar/access_right/c_abf2 |
eu_rights_str_mv |
openAccess |
dc.publisher.spa.fl_str_mv |
Universidad de la Costa |
institution |
Corporación Universidad de la Costa |
bitstream.url.fl_str_mv |
https://repositorio.cuc.edu.co/bitstreams/b1a68d82-5f3c-4d73-8eef-2ca715be3ce4/download https://repositorio.cuc.edu.co/bitstreams/32039201-aca9-44ff-b6e1-2d121615f6f1/download https://repositorio.cuc.edu.co/bitstreams/2c8033c8-ae13-4d22-9cd9-b7fc4e518ecc/download https://repositorio.cuc.edu.co/bitstreams/4b6af5b9-5756-4af5-98ae-16a298337476/download https://repositorio.cuc.edu.co/bitstreams/789a5e23-cc8b-41cd-ad7d-07a92b5c1631/download |
bitstream.checksum.fl_str_mv |
d6dcc6a2fb3ade7a8c5520ab5a612eaf 42fd4ad1e89814f5e4a476b409eb708c 8a4605be74aa9ea9d79846c1fba20a33 dd504f02ae50baf180395ec217648aa5 86dd7f0138fe5b53763dcf830a1c5688 |
bitstream.checksumAlgorithm.fl_str_mv |
MD5 MD5 MD5 MD5 MD5 |
repository.name.fl_str_mv |
Repositorio de la Universidad de la Costa CUC |
repository.mail.fl_str_mv |
repdigital@cuc.edu.co |
_version_ |
1811760818719555584 |
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; charset=utf-8701https://repositorio.cuc.edu.co/bitstreams/32039201-aca9-44ff-b6e1-2d121615f6f1/download42fd4ad1e89814f5e4a476b409eb708cMD52LICENSElicense.txtlicense.txttext/plain; charset=utf-81748https://repositorio.cuc.edu.co/bitstreams/2c8033c8-ae13-4d22-9cd9-b7fc4e518ecc/download8a4605be74aa9ea9d79846c1fba20a33MD53THUMBNAILFluvial and oceanographic influences on suspended sediment dispersal in the Magdalena River Estuary.pdf.jpgFluvial and oceanographic influences on suspended sediment dispersal in the Magdalena River Estuary.pdf.jpgimage/jpeg70911https://repositorio.cuc.edu.co/bitstreams/4b6af5b9-5756-4af5-98ae-16a298337476/downloaddd504f02ae50baf180395ec217648aa5MD55TEXTFluvial and oceanographic influences on suspended sediment dispersal in the Magdalena River Estuary.pdf.txtFluvial and oceanographic influences on suspended sediment dispersal in the Magdalena River Estuary.pdf.txttext/plain2295https://repositorio.cuc.edu.co/bitstreams/789a5e23-cc8b-41cd-ad7d-07a92b5c1631/download86dd7f0138fe5b53763dcf830a1c5688MD5611323/5997oai:repositorio.cuc.edu.co:11323/59972024-09-17 12:50:03.739http://creativecommons.org/publicdomain/zero/1.0/CC0 1.0 Universalopen.accesshttps://repositorio.cuc.edu.coRepositorio de la Universidad de la Costa CUCrepdigital@cuc.edu.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 |