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dc.creatorCampo-Bescós, Migueles_ES
dc.creatorFlores Cervantes, J. H.es_ES
dc.creatorBras, R. L.es_ES
dc.creatorCasalí Sarasíbar, Javieres_ES
dc.creatorGiráldez Cervera, Juan Vicentees_ES
dc.date.accessioned2018-11-27T11:22:20Z
dc.date.available2018-11-27T11:22:20Z
dc.date.issued2013
dc.identifier.issn2169-9011
dc.identifier.urihttps://hdl.handle.net/2454/31500
dc.description.abstractA large fraction of soil erosion in temperate climate systems proceeds from gully headcut growth processes. Nevertheless, headcut retreat is not well understood. Few erosion models include gully headcut growth processes, and none of the existing headcut retreat models have been tested against long-term retreat rate estimates. In this work the headcut retreat resulting from plunge pool erosion in the Channel Hillslope Integrated Landscape Development (CHILD) model is calibrated and compared to long-term evolution measurements of six gullies at the Bardenas Reales, northeast Spain. The headcut retreat module of CHILD was calibrated by adjusting the shape factor parameter to fit the observed retreat and volumetric soil loss of one gully during a 36 year period, using reported and collected field data to parameterize the rest of the model. To test the calibrated model, estimates by CHILD were compared to observations of headcut retreat from five other neighboring gullies. The differences in volumetric soil loss rates between the simulations and observations were less than 0.05 m3 yr-1, on average, with standard deviations smaller than 0.35 m3 yr-1. These results are the first evaluation of the headcut retreat module implemented in CHILD with a field data set. These results also show the usefulness of the model as a tool for simulating long-term volumetric gully evolution due to plunge pool erosion.en
dc.description.sponsorshipThis work was made possible by financial support from the Spanish Ministry of Science and Technology, through the research project CGL2007-63453/HID, the Department of Education of the Government of Navarra, and the Public University of Navarra, with a fellowship awarded to the first author. CHILD development was supported by the U.S. Army Research Office (agreement DAAD 19-01-1-0513) and through the NSF grant (EAR 0642550).en
dc.format.extent15 p.
dc.format.mimetypeapplication/pdfen
dc.language.isoengen
dc.publisherAmerican Geophysical Unionen
dc.publisherWileyen
dc.relation.ispartofJournal of Geophysical Research: Earth Surface, vol. 118, 2159–2173en
dc.rights©2013. American Geophysical Union. All Rights Reserved.en
dc.subjectGully headcut retreaten
dc.subjectChannel Hillslope Integrated Landscape Development (CHILD) modelen
dc.titleEvaluation of a gully headcut retreat model using multitemporal aerial photographs and digital elevation modelsen
dc.typeinfo:eu-repo/semantics/articleen
dc.typeArtículo / Artikuluaes
dc.contributor.departmentProyectos e Ingeniería Rurales_ES
dc.contributor.departmentLanda Ingeniaritza eta Proiektuakeu
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen
dc.rights.accessRightsAcceso abierto / Sarbide irekiaes
dc.identifier.doi10.1002/jgrf.20147
dc.relation.publisherversionhttps://doi.org/10.1002/jgrf.20147
dc.type.versioninfo:eu-repo/semantics/publishedVersionen
dc.type.versionVersión publicada / Argitaratu den bertsioaes
dc.contributor.funderGobierno de Navarra / Nafarroako Gobernuaes
dc.contributor.funderUniversidad Pública de Navarra / Nafarroako Unibertsitate Publikoaes


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