dc.contributor.author | Martínez-Fernández, A. | |
dc.contributor.author | Serrano Cañadas, Enrique | |
dc.contributor.author | Sanjosé Blasco, José Juan de | |
dc.contributor.author | Gómez Lende, Manuel | |
dc.contributor.author | Sánchez Fernández, M. | |
dc.contributor.author | López Moreno, J. I. | |
dc.contributor.author | Rico, I. | |
dc.contributor.author | Pisabarro, A. | |
dc.contributor.other | Universidad de Cantabria | es_ES |
dc.date.accessioned | 2024-03-15T15:28:19Z | |
dc.date.available | 2025-01-01T00:27:55Z | |
dc.date.issued | 2023-12 | |
dc.identifier.issn | 1099-145X | |
dc.identifier.issn | 1085-3278 | |
dc.identifier.other | CGL2015-68144-R | es_ES |
dc.identifier.other | PID2020-113247RB-C21 | es_ES |
dc.identifier.uri | https://hdl.handle.net/10902/32275 | |
dc.description.abstract | Small 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 2030s | es_ES |
dc.format.extent | 18 p. | es_ES |
dc.language.iso | eng | es_ES |
dc.publisher | John Wiley & Sons | es_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.source | Land Degradation and Development, 2023, 34(18), 5905-5922 | es_ES |
dc.subject.other | Glaciology | es_ES |
dc.subject.other | Global Change | es_ES |
dc.subject.other | Monitoring | es_ES |
dc.subject.other | Geomatics | es_ES |
dc.subject.other | Terrestrial Laser Scanning 39 (TLS) | es_ES |
dc.subject.other | Photogrammetry | es_ES |
dc.subject.other | Unmanned Aerial Vehicle (UAV) | es_ES |
dc.subject.other | Pyrenees | es_ES |
dc.title | The final countdown? Monitoring the rapid shrinkage of the Maladeta glacier (2010–2020), Southern Pyrenees | es_ES |
dc.type | info:eu-repo/semantics/article | es_ES |
dc.rights.accessRights | openAccess | es_ES |
dc.relation.projectID | info: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.projectID | info: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.DOI | 10.1002/ldr.4886 | |
dc.type.version | acceptedVersion | es_ES |