Mostrar el registro sencillo

dc.contributor.authorMartínez-Fernández, A.
dc.contributor.authorSerrano Cañadas, Enrique
dc.contributor.authorSanjosé Blasco, José Juan de
dc.contributor.authorGómez Lende, Manuel 
dc.contributor.authorSánchez Fernández, M.
dc.contributor.authorLópez Moreno, J. I.
dc.contributor.authorRico, I.
dc.contributor.authorPisabarro, A.
dc.contributor.otherUniversidad de Cantabriaes_ES
dc.date.accessioned2024-03-15T15:28:19Z
dc.date.available2025-01-01T00:27:55Z
dc.date.issued2023-12
dc.identifier.issn1099-145X
dc.identifier.issn1085-3278
dc.identifier.otherCGL2015-68144-Res_ES
dc.identifier.otherPID2020-113247RB-C21es_ES
dc.identifier.urihttps://hdl.handle.net/10902/32275
dc.description.abstractSmall glaciers are one of the best indicators of climatic variations and their short-term effects. Located in the Spanish Pyrenees, the Maladeta is one of these glaciers. Its systematic observation began in the 1980s, being one of the few Pyrenean glaciers with a tongue-shaped front. This study presents the evolution of the Maladeta glacial tongue over a decade (2010?2020) through multiple geomatic techniques. Surveys have ranged from Total Stations and Global Navigation Satellite System devices to massive data capture techniques such as Terrestrial Laser Scanners or Unmanned Aerial Vehicles photogrammetry. The aim is to analyze in detail the loss of surface area and thickness of the glacier and its transition from being a glacier with a tongue partially determined by climate to a topoclimatically determined cirque glacier. The results reveal a tongue retreat of over 5 m/yr and area losses of over 0.2 ha/yr, along with ice thickness and volume losses of 1.7 m/yr and over 21 103 m3/yr, respectively. If this trend continues, the tongue, and possibly the Maladeta glacier, could disappear by the end of the 2030ses_ES
dc.format.extent18 p.es_ES
dc.language.isoenges_ES
dc.publisherJohn Wiley & Sonses_ES
dc.rights© John Wiley & Sons. This is the peer reviewed version of the following article: Martínez-Fernández, A., Serrano, E., de Sanjosé, J. J., Gómez-Lende, M., Sánchez-Fernández, M., López-Moreno, J. I., Rico, I., & Pisabarro, A. (2023). The final countdown? Monitoring the rapid shrinkage of the Maladeta glacier (2010–2020), Southern Pyrenees. Land Degradation & Development, 34(18), 5905–5922, which has been published in final form at https://doi.org/10.1002/ldr.4886. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Self-Archiving.es_ES
dc.sourceLand Degradation and Development, 2023, 34(18), 5905-5922es_ES
dc.subject.otherGlaciologyes_ES
dc.subject.otherGlobal Changees_ES
dc.subject.otherMonitoringes_ES
dc.subject.otherGeomaticses_ES
dc.subject.otherTerrestrial Laser Scanning 39 (TLS)es_ES
dc.subject.otherPhotogrammetryes_ES
dc.subject.otherUnmanned Aerial Vehicle (UAV)es_ES
dc.subject.otherPyreneeses_ES
dc.titleThe final countdown? Monitoring the rapid shrinkage of the Maladeta glacier (2010–2020), Southern Pyreneeses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsopenAccesses_ES
dc.relation.projectIDinfo:eu-repo/grantAgreement/MINECO//CGL2015-68144-R/ES/INTERACCIONES Y DINAMICA DE LA CRIOSFERA EN LA MONTAÑA CANTABRICA Y PIRINEOS: PERMAFROST, GLACIARES, CUEVAS HELADAS Y CAMBIO GLOBAL/
dc.relation.projectIDinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/PID2020-113247RB-C21/ES/DINAMICA, EVOLUCION RECIENTE Y MODELIZACION DE LA CRIOSFERA EN AMBIENTES TEMPLADOS Y TROPICALES. GLACIARES, GLACIARES ROCOSOS, PERMAFROST Y CUEVAS HELADAS EN EL NORTE DE ESPAÑ/
dc.identifier.DOI10.1002/ldr.4886
dc.type.versionacceptedVersiones_ES


Ficheros en el ítem

Thumbnail

Este ítem aparece en la(s) siguiente(s) colección(ones)

Mostrar el registro sencillo