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    Por favor, use este identificador para citar o enlazar este ítem:https://uvadoc.uva.es/handle/10324/55919

    Título
    Monitoring retreat of coastal sandy systems using geomatics techniques: Somo beach (Cantabrian coast, Spain, 1875–2017)
    Autor
    Sanjosé Blasco, José Juan de
    Gómez Lende, Manuel
    Sánchez Fernández, Manuel
    Serrano Cañadas, EnriqueAutoridad UVA Orcid
    Año del Documento
    2018
    Editorial
    MDPI
    Descripción
    Producción Científica
    Documento Fuente
    Remote Sensing, 2018, vol. 10, n. 9, p. 1500
    Resumen
    The dynamics and evolution of a coastal sandy system over the last 142 years (1875–2017) were analyzed using geomatics techniques (historical cartography, photogrammetry, topography, and terrestrial laser scanning (TLS)). The continuous beach–dune system is a very active confining sand barrier closing an estuarine system where damage is suffered by coastal infrastructures and houses. The techniques used and documentary sources involved historical cartography, digitalizing the 5-m-level curve on the maps of 1875, 1908, 1920, 1950, and 1985; photogrammetric flights of 1985, 1988, and 2001 without calibration certificates, digitalizing only the upper part of the sandy front; photogrammetric flights of 2005, 2007, 2010, and 2014, using photogrammetric restitution of the 5-m-level curve; topo-bathymetric profiles made monthly between 1988 and 1993 using a total station; a terrestrial laser scanner (TLS) since 2011 by means of two annual measurements; and the meteorological data for the period of 1985–2017. The retreat of the sandy complex was caused by winter storms with large waves and swells higher than 6 m, coinciding with periods demonstrating a high tidal range of over 100 and periods with a large number of strong storms. The retreat was 8 m between December 2013 and March 2014. The overall change of the coastline between 1875 and 2017 was approximately 415 m of retreat at Somo Beach. The erosive processes on the foredune involved the outcrop of the rock cliff in 1999 and 2014, which became a continuous rocky cliff without sands. To know the recent coastal evolution and its consequences on the human environment, the combined geomatic techniques and future TLS data series may lead to the improvement in the knowledge of shoreline changes in the context of sea level and global changes.
    Materias Unesco
    54 Geografía
    Palabras Clave
    Coastal geomorphology
    Monitoring
    Morphology
    Geomatic techniques
    Sandy systems
    ISSN
    2072-4292
    Revisión por pares
    SI
    DOI
    10.3390/rs10091500
    Patrocinador
    Junta de Extremadura y FEDER, (GR18053)
    Ministerio de Asuntos Económicos y Transformación Digital y FEDER ( the I+D+I project CGL2015-68144-R)
    Version del Editor
    https://www.mdpi.com/2072-4292/10/9/1500
    Propietario de los Derechos
    © 2018 The Authors
    Idioma
    eng
    URI
    https://uvadoc.uva.es/handle/10324/55919
    Tipo de versión
    info:eu-repo/semantics/publishedVersion
    Derechos
    openAccess
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    • DEP35 - Artículos de revista [155]
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    Universidad de Valladolid

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