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    The final countdown? Monitoring the rapid shrinkage of the Maladeta glacier (2010–2020), Southern Pyrenees

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    Identificadores
    URI: https://hdl.handle.net/10902/32275
    DOI: 10.1002/ldr.4886
    ISSN: 1099-145X
    ISSN: 1085-3278
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    Autoría
    Martínez-Fernández, A.; Serrano Cañadas, Enrique; Sanjosé Blasco, José Juan de; Gómez Lende, ManuelAutoridad Unican; Sánchez Fernández, M.; López Moreno, J. I.; Rico, I.; Pisabarro, A.
    Fecha
    2023-12
    Derechos
    © 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.
    Publicado en
    Land Degradation and Development, 2023, 34(18), 5905-5922
    Editorial
    John Wiley & Sons
    Palabras clave
    Glaciology
    Global Change
    Monitoring
    Geomatics
    Terrestrial Laser Scanning 39 (TLS)
    Photogrammetry
    Unmanned Aerial Vehicle (UAV)
    Pyrenees
    Resumen/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
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    UNIVERSIDAD DE CANTABRIA

    Repositorio realizado por la Biblioteca Universitaria utilizando DSpace software
    Contacto | Sugerencias
    Metadatos sujetos a:licencia de Creative Commons Reconocimiento 4.0 España