Temporal variability in the relationships between precipitation, discharge and suspended sediment concentration in a small Mediterranean mountain catchment
Relationships between discharge and suspended sediment are very complex in most Mediterranean catchments. In the case of the Arnás catchment (Central Spanish Pyrenees), with a long history of human activity, the main factors that explain the variability of suspended sediment concentration (SCC) duri...
| Autores: | , , , , , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2007 |
| País: | España |
| Institución: | Universidad de La Rioja (UR) |
| Repositorio: | RIUR. Repositorio Institucional de la Universidad de La Rioja |
| OAI Identifier: | oai:portal.dialnet.es:doc/5e81db8c29995270f8358e92 |
| Acceso en línea: | https://investigacion.unirioja.es/documentos/5e81db8c29995270f8358e92 |
| Access Level: | acceso abierto |
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Temporal variability in the relationships between precipitation, discharge and suspended sediment concentration in a small Mediterranean mountain catchmentLana-Renault, Noemi [0000-0002-0272-2504]Regüés, null [0000-0003-3232-0300]Martí-Bono, nullBeguería, null [0000-0002-3974-2947]Latron, null [0000-0003-3253-6734]Nadal, null [0000-0002-4651-7828]Serrano, nullGarcía-Ruiz, null [0000-0002-8535-817X]Relationships between discharge and suspended sediment are very complex in most Mediterranean catchments. In the case of the Arnás catchment (Central Spanish Pyrenees), with a long history of human activity, the main factors that explain the variability of suspended sediment concentration (SCC) during floods are the peak flow and the intensity of precipitation. A cluster analysis distinguishes four types of floods according to different characteristics of precipitation, discharge, suspended sediment transport and antecedent moisture conditions. G1 and G2 floods occur under dry conditions (which prevail most of the year), with moderate rainfall and low precipitation intensity; the discharge and suspended sediment response are very fast but limited in intensity. This suggests that the origin of water and sediment is restricted to areas located very close to the channel. G3 floods also occur under dry conditions, although during intense rainfall events; then the response in both discharge and suspended sediment is very high, showing an enlargement of the contributing areas. Under very wet conditions (G4 floods) relatively moderate precipitation produces a very high response in discharge, but suspended sediment concentration records moderate values due to the effect of dilution when the entire catchment is contributing. © IWA Publishing 2007.2007info:eu-repo/semantics/articleSubtype: Articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://investigacion.unirioja.es/documentos/5e81db8c29995270f8358e92reponame:RIUR. Repositorio Institucional de la Universidad de La Riojainstname:Universidad de La Rioja (UR)Inglésinfo:eu-repo/semantics/altIdentifier/doi/10.2166/NH.2007.003info:eu-repo/semantics/altIdentifier/pissn/0029-1277Temporal variability in the relationships between precipitation, discharge and suspended sediment concentration in a small Mediterranean mountain catchment, 2007, vol. 38, núm. 2, pág. 139-150info:eu-repo/semantics/openAccessoai:portal.dialnet.es:doc/5e81db8c29995270f8358e922026-06-14T12:47:17Z |
| dc.title.none.fl_str_mv |
Temporal variability in the relationships between precipitation, discharge and suspended sediment concentration in a small Mediterranean mountain catchment |
| title |
Temporal variability in the relationships between precipitation, discharge and suspended sediment concentration in a small Mediterranean mountain catchment |
| spellingShingle |
Temporal variability in the relationships between precipitation, discharge and suspended sediment concentration in a small Mediterranean mountain catchment Lana-Renault, Noemi [0000-0002-0272-2504] |
| title_short |
Temporal variability in the relationships between precipitation, discharge and suspended sediment concentration in a small Mediterranean mountain catchment |
| title_full |
Temporal variability in the relationships between precipitation, discharge and suspended sediment concentration in a small Mediterranean mountain catchment |
| title_fullStr |
Temporal variability in the relationships between precipitation, discharge and suspended sediment concentration in a small Mediterranean mountain catchment |
| title_full_unstemmed |
Temporal variability in the relationships between precipitation, discharge and suspended sediment concentration in a small Mediterranean mountain catchment |
| title_sort |
Temporal variability in the relationships between precipitation, discharge and suspended sediment concentration in a small Mediterranean mountain catchment |
| dc.creator.none.fl_str_mv |
Lana-Renault, Noemi [0000-0002-0272-2504] Regüés, null [0000-0003-3232-0300] Martí-Bono, null Beguería, null [0000-0002-3974-2947] Latron, null [0000-0003-3253-6734] Nadal, null [0000-0002-4651-7828] Serrano, null García-Ruiz, null [0000-0002-8535-817X] |
| author |
Lana-Renault, Noemi [0000-0002-0272-2504] |
| author_facet |
Lana-Renault, Noemi [0000-0002-0272-2504] Regüés, null [0000-0003-3232-0300] Martí-Bono, null Beguería, null [0000-0002-3974-2947] Latron, null [0000-0003-3253-6734] Nadal, null [0000-0002-4651-7828] Serrano, null García-Ruiz, null [0000-0002-8535-817X] |
| author_role |
author |
| author2 |
Regüés, null [0000-0003-3232-0300] Martí-Bono, null Beguería, null [0000-0002-3974-2947] Latron, null [0000-0003-3253-6734] Nadal, null [0000-0002-4651-7828] Serrano, null García-Ruiz, null [0000-0002-8535-817X] |
| author2_role |
author author author author author author author |
| description |
Relationships between discharge and suspended sediment are very complex in most Mediterranean catchments. In the case of the Arnás catchment (Central Spanish Pyrenees), with a long history of human activity, the main factors that explain the variability of suspended sediment concentration (SCC) during floods are the peak flow and the intensity of precipitation. A cluster analysis distinguishes four types of floods according to different characteristics of precipitation, discharge, suspended sediment transport and antecedent moisture conditions. G1 and G2 floods occur under dry conditions (which prevail most of the year), with moderate rainfall and low precipitation intensity; the discharge and suspended sediment response are very fast but limited in intensity. This suggests that the origin of water and sediment is restricted to areas located very close to the channel. G3 floods also occur under dry conditions, although during intense rainfall events; then the response in both discharge and suspended sediment is very high, showing an enlargement of the contributing areas. Under very wet conditions (G4 floods) relatively moderate precipitation produces a very high response in discharge, but suspended sediment concentration records moderate values due to the effect of dilution when the entire catchment is contributing. © IWA Publishing 2007. |
| publishDate |
2007 |
| dc.date.none.fl_str_mv |
2007 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article Subtype: Article info:eu-repo/semantics/publishedVersion |
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article |
| status_str |
publishedVersion |
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https://investigacion.unirioja.es/documentos/5e81db8c29995270f8358e92 |
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https://investigacion.unirioja.es/documentos/5e81db8c29995270f8358e92 |
| dc.language.none.fl_str_mv |
Inglés |
| language_invalid_str_mv |
Inglés |
| dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.2166/NH.2007.003 info:eu-repo/semantics/altIdentifier/pissn/0029-1277 Temporal variability in the relationships between precipitation, discharge and suspended sediment concentration in a small Mediterranean mountain catchment, 2007, vol. 38, núm. 2, pág. 139-150 |
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info:eu-repo/semantics/openAccess |
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openAccess |
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application/pdf |
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Universidad de La Rioja (UR) |
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RIUR. Repositorio Institucional de la Universidad de La Rioja |
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