Rainfall and water yield in Macizo del Caroig, Eastern Iberian Peninsulaevent runoff at plot scale during a rare flash flood at the Barranco de Benacancil

  1. Artemi Cerdà 3
  2. Agata Novara 4
  3. Pavel Dlapa 12
  4. Manuel López Vicente 13
  5. Xavier Úbeda 14
  6. Zorica Popovic 10
  7. Mulatie Mekonnen 9
  8. Enric Terol 11
  9. Saeid Janizadeh 1
  10. Sonia Mbarki 2
  11. Eduardo Saldanha Vogelmann 5
  12. Sajjad Hazrati 6
  13. Srikanta Sannigrahi 7
  14. Misagh Parhizkar 8
  15. Antonio Giménez Morera 11
  1. 1 Tarbiat Modares University
    info

    Tarbiat Modares University

    Teherán, Irán

    ROR https://ror.org/03mwgfy56

  2. 2 National Research Institute of Rural Engineering, Water and Forests
    info

    National Research Institute of Rural Engineering, Water and Forests

    Ariana, Túnez

    ROR https://ror.org/02zcy8d62

  3. 3 Universitat de València
    info

    Universitat de València

    Valencia, España

    ROR https://ror.org/043nxc105

  4. 4 University of Palermo
    info

    University of Palermo

    Palermo, Italia

    ROR https://ror.org/044k9ta02

  5. 5 Fundação Universidade Federal do Rio Grande
    info

    Fundação Universidade Federal do Rio Grande

    Rio Grande, Brasil

    ROR https://ror.org/05hpfkn88

  6. 6 University of Tehran
    info

    University of Tehran

    Teherán, Irán

    ROR https://ror.org/05vf56z40

  7. 7 University College Dublin
    info

    University College Dublin

    Dublín, Irlanda

    ROR https://ror.org/05m7pjf47

  8. 8 University of Guilan
    info

    University of Guilan

    Rasht, Irán

    ROR https://ror.org/01bdr6121

  9. 9 Bahir Dar University
    info

    Bahir Dar University

    Bahir Dar, Etiopía

    ROR https://ror.org/01670bg46

  10. 10 University of Belgrade
    info

    University of Belgrade

    Belgrado, Serbia

    ROR https://ror.org/02qsmb048

  11. 11 Universidad Politécnica de Valencia
    info

    Universidad Politécnica de Valencia

    Valencia, España

    ROR https://ror.org/01460j859

  12. 12 Comenius University
    info

    Comenius University

    Bratislava, Eslovaquia

    ROR https://ror.org/0587ef340

  13. 13 Wageningen Environmental Research
  14. 14 Universitat de Barcelona
    info

    Universitat de Barcelona

    Barcelona, España

    ROR https://ror.org/021018s57

Mostrar afiliaciones +
Revista:
Cuadernos de investigación geográfica: Geographical Research Letters
  1. Romero Díaz, María Asunción (ed. lit.)

ISSN: 0211-6820,  1697-9540

Año de publicación: 2021

Volumen: 47

Número: 1

Páginas: 95-119

Tipo: Artículo

DOI: 10.18172/CIG.4833 DIALNET GOOGLE SCHOLAR lock_openAcceso abierto editor

Otras publicaciones en: Cuadernos de investigación geográfica: Geographical Research Letters

Resumen

Las inundaciones son consecuencia de lluvias extremas. Aunque la generación de escorrentía superficial es el origen de la descarga, la investigación de inundaciones generalmente se enfoca en las tierras bajas donde el impacto es mayor. La escorrentía y la distribución de sedimentos a escala de pendiente y pedón reciben mucha menos atención en la comprensión del comportamiento de las inundaciones en el tiempo y el espacio. Esto es especialmente relevante en zonas donde, debido a las condiciones climáticas e hidrogeológicas, los cauces son efímeros. Son los llamados ríos secos (“wadis”, “ramblas” o “barrancos”) muy extendidos por todo el Mediterráneo. Este artículo investiga la relación entre el suministro de agua a escala de pedón y ladera con las crecidas de ríos secos en Macizo del Caroig, este de la Península Ibérica. Las parcelas de 1x1, 1x2, 1x4 y 2x8 m localizadas en la Estación de Investigación de Erosión y Degradación de Suelos “El Teularet” fueron monitoreadas de 2004 a 2014 para medir la producción de suelo y agua. También se monitorearon las precipitaciones y el caudal en el río seco Barranco de Benacancil. Los resultados muestran que la escorrentía y la descarga de sedimentos se concentraron en pocos eventos durante los 11 años de investigación. Se registró un solo evento de inundación en el canal el 28 de septiembre de 2009, sin embargo, la escorrentía se registró 160 veces en las parcelas. La descarga de escorrentía dependió del tamaño de las parcelas. Las parcelas más grandes produjeron una menor descarga de escorrentía por unidad de área, lo que sugiere una corta distancia y duración del recorrido de escorrentía. Tres eventos de lluvia contribuyeron con el 26% de la descarga total de la escorrentía y cinco lograron el 56% de la escorrentía. Se concluye que la escorrentía generada a escala de la parcela está desconectada del canal principal. Desde un punto de vista espacial, hay una disminución en el coeficiente de escorrentía a lo largo de la pendiente. Desde un punto de vista temporal, la escorrentía se concentra en unos pocos eventos de lluvia. Estos resultados muestran que la escorrentía generada a escala de parcela y pendiente no contribuyen a las inundaciones excepto para eventos de lluvia con más de 100 mm día-1. La desconexión de la escorrentía y la entrega de sedimentos se confirma por la reducción de la escorrentía a escala de parcela debido al control de la longitud (pendiente) sobre la escorrentía y la entrega de sedimentos.

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Información de financiación

Artemi Cerdà thanks the Co-operative Research program from the OECD (Biological Resource Management for Sustainable Agricultural Systems) for its support with the 2016 CRP fellowship (OCDE TAD/CRP JA00088807), POSTFIRE Project (CGL2013-47862-C2-1 and 2-R), and POSTFIRE_CARE Project (CGL2016-75178-C2-2-R) sponsored by the Spanish Ministry of Economy and Competitiveness and AEI/FEDER, UE. This paper was written as a result of the collaboration that was initiated due to the COST ActionES1306: Connecting European Connectivity research and COST CA18135 FIRElinks: Fire in the Earth System. Science and Society. We wish to thank the Department of Geography secretariat team (Nieves Gómez, Nieves Dominguez, and Susana Tomás) for their support for three decades to our research at the Soil Erosion and Degradation Research team (SEDER), with special thanks to the scientific researchers that as visitors from other research teams contributed to the

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Fuente de los datos: Dialnet