Identificador persistente para citar o vincular este elemento: http://hdl.handle.net/10553/77967
Campo DC Valoridioma
dc.contributor.authorHesp, Patrick A.en_US
dc.contributor.authorHernández Calvento, Luis Franciscoen_US
dc.contributor.authorHernández Cordero, Antonio Ignacioen_US
dc.contributor.authorGallego-Fernández, Juan B.en_US
dc.contributor.authorGarcía Romero, Leví Adayen_US
dc.contributor.authorMiot da Silva, Grazielaen_US
dc.contributor.authorRuz, Marie Heleneen_US
dc.date.accessioned2021-03-08T14:33:15Z-
dc.date.available2021-03-08T14:33:15Z-
dc.date.issued2021en_US
dc.identifier.issn0048-9697en_US
dc.identifier.otherScopus-
dc.identifier.otherWoS-
dc.identifier.urihttp://hdl.handle.net/10553/77967-
dc.description.abstractThis study examines the role of sediment supply in controlling the formation and the spatial patterns of nebkha, numbers and sizes, present in foredunes fronting coastal dunefields of the arid northwest African and the Canary Islands coasts. Sediment supply is estimated qualitatively and quantitatively by various measures, and the number and size of nebkhas are obtained on a range of beach-dune systems. In the case of the Canary Islands, LiDAR data and orthophotos with high spatial resolution (0.25 m) are used to measure sediment supply/activity, nebkha numbers and sizes, and vegetation variables, whereas data availability is less on the African coast. Results show that sediment supply exerts a major control on nebkha development such that as sediment supply increases, the number of coastal nebkha decreases, and the size of individual plants/nebkha increases. Once sediment supply is large, nebkha can only form on the immediate backshore if space is available, and a point is reached when the sediment supply is so large that nebkha do not, or cannot form. The data presented here provide two indicators which could be applicable to other dune systems. Firstly, by estimating the number of nebkha and the vegetation cover, the degree of aeolian sedimentary activity or sediment supply might be estimated. Secondly, the type of aeolian landform present provides a qualitative indication of sediment supply and aeolian activity.en_US
dc.languageengen_US
dc.relationAnálisis Del Impacto de Las Inundaciones en Áreas Turísticas Costeras: Canarias, Laboratorio Natural de Resilenciaen_US
dc.relation.ispartofScience of the Total Environmenten_US
dc.sourceScience of the Total Environment [ISSN 0048-9697], v. 773, (Junio 2021)en_US
dc.subject250618 Sedimentologíaen_US
dc.subject2506 Geologíaen_US
dc.subject.otherCanary Islandsen_US
dc.subject.otherCoastal Dunesen_US
dc.subject.otherForedunesen_US
dc.subject.otherNebkhaen_US
dc.subject.otherNw African Coasten_US
dc.subject.otherSediment Supplyen_US
dc.subject.otherMorphological-Characteristicsen_US
dc.subject.otherCoastal Nabkhasen_US
dc.titleNebkha development and sediment supplyen_US
dc.typeinfo:eu-repo/semantics/Articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.scitotenv.2020.144815en_US
dc.identifier.scopus85101049542-
dc.identifier.isi000635207100010-
dc.contributor.authorscopusid6701688719-
dc.contributor.authorscopusid51561623100-
dc.contributor.authorscopusid52863616700-
dc.contributor.authorscopusid7801475198-
dc.contributor.authorscopusid57221741115-
dc.contributor.authorscopusid8602511800-
dc.contributor.authorscopusid7003668859-
dc.identifier.eissn1879-1026-
dc.relation.volume773en_US
dc.investigacionArtes y Humanidadesen_US
dc.type2Artículoen_US
dc.contributor.daisngid30434929-
dc.contributor.daisngid2472102-
dc.contributor.daisngid42686799-
dc.contributor.daisngid43643725-
dc.contributor.daisngid44077750-
dc.contributor.daisngid40321592-
dc.contributor.daisngid1446719-
dc.description.numberofpages12en_US
dc.utils.revisionen_US
dc.contributor.wosstandardWOS:Hesp, PA-
dc.contributor.wosstandardWOS:Hernandez-Calvento, L-
dc.contributor.wosstandardWOS:Hernandez-Cordero, AI-
dc.contributor.wosstandardWOS:Gallego-Fernandez, JB-
dc.contributor.wosstandardWOS:Romero, LG-
dc.contributor.wosstandardWOS:da Silva, GM-
dc.contributor.wosstandardWOS:Ruz, MH-
dc.date.coverdateJunio 2021en_US
dc.identifier.ulpgcen_US
dc.contributor.buulpgcBU-HUMen_US
dc.description.sjr1,806
dc.description.jcr10,753
dc.description.sjrqQ1
dc.description.jcrqQ1
dc.description.scieSCIE
dc.description.miaricds11,0
item.grantfulltextnone-
item.fulltextSin texto completo-
crisitem.author.deptGIR IOCAG: Geografía, Medio Ambiente y Tecnologías de la Información Geográfica-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Geografía-
crisitem.author.deptGIR IOCAG: Geografía, Medio Ambiente y Tecnologías de la Información Geográfica-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Geografía-
crisitem.author.deptGIR IOCAG: Geografía, Medio Ambiente y Tecnologías de la Información Geográfica-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.orcid0000-0002-4948-7230-
crisitem.author.orcid0000-0002-8373-9235-
crisitem.author.orcid0000-0002-4985-9073-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.fullNameHernández Calvento, Luis Francisco-
crisitem.author.fullNameHernández Cordero, Antonio Ignacio-
crisitem.author.fullNameGarcía Romero, Leví Aday-
crisitem.project.principalinvestigatorMáyer Suárez, Pablo Lucas-
Colección:Artículos
Vista resumida

Citas SCOPUSTM   

16
actualizado el 24-nov-2024

Citas de WEB OF SCIENCETM
Citations

15
actualizado el 24-nov-2024

Visitas

122
actualizado el 11-may-2024

Google ScholarTM

Verifica

Altmetric


Comparte



Exporta metadatos



Los elementos en ULPGC accedaCRIS están protegidos por derechos de autor con todos los derechos reservados, a menos que se indique lo contrario.