Remote sensing monitoring of a coastal-valley earthflow in northwestern Galicia, Spain

dc.contributor.affiliationUniversidade de Santiago de Compostela. Departamento de Xeografíaes_ES
dc.contributor.authorGarcía, Horacio
dc.contributor.authorMuñoz-Narciso, Efrén
dc.contributor.authorTrenhaile, Alan
dc.contributor.authorPérez Alberti, Augusto
dc.date.accessioned2024-02-12T07:35:56Z
dc.date.available2024-02-12T07:35:56Z
dc.date.issued2019
dc.description.abstractHistorical air photographs, LiDAR, and an unmanned aerial vehicle (UAV) were used to record the movement, from 1956 to 2018, of a clay and clast earthflow in a coastal valley in northwestern Spain. Two procedures were employed. The first tracked changes, in a GIS environment, in the location of eight, easily identified objects on the surface of the deposit (large boulders, topographic lobes, and the foundations of an old hut). The second used DEMs of Difference (DoDs) based on Digital Elevation Models from a 2011 LiDAR flight and two UAV flights in 2016 and 2018 obtained by Structure from Motion-Photogrammetry techniques. While the first procedure provided estimates for earthflow movement over a 62-year period, the second produced more precise data for periods of up to 8-years. The first procedure indicated that the mean rate of movement was 0.48 m·yr−1, increasing from only 0.14 m·yr−1 from 1956 to 1983 to between 0.50 and 0.83 m·yr−1 from 1983 to 2018. Despite some temporal and spatial changes in direction, rates of surface movement were quite uniform on the deposit. The increase in earthflow movement after 1983 may be related to an increase in rainfall, although human activities associated with the removal of a wrecked ship from the nearshore may have been a contributing factor. The role of debuttressing due to the wave-induced removal of lateral support from the toe of the deposit is less clear. While there was no clear relationship between wave erosion and rates of movement, coastal retreat may have triggered changes in the direction and sediment flux in the toe of the deposit. This effect could have been tempered by negative feedback, however, whereby coastal erosion and increased flow activity were countered by the protection afforded by the accumulation of large, dislodged boulders on the beach. Because of this feedback, it is difficult to predict the impact of sea level rise and other elements of climate change along this coast.es_ES
dc.description.peerreviewedSIes_ES
dc.identifier.citationCATENA, Volume 178, 2019, Pages 276-287es_ES
dc.identifier.doi10.1016/j.catena.2019.03.028
dc.identifier.urihttp://hdl.handle.net/10347/32712
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.rightsCC BY-NC-NDes_ES
dc.rights.accessRightsopen accesses_ES
dc.subjectEarthflowes_ES
dc.subjectCoastal-valleyes_ES
dc.subjectUAVes_ES
dc.subjectLiDARes_ES
dc.subjectSfM-photogrammetryes_ES
dc.subjectGaliciaes_ES
dc.subject.classification250507 Geografía físicaes_ES
dc.titleRemote sensing monitoring of a coastal-valley earthflow in northwestern Galicia, Spaines_ES
dc.typejournal articlees_ES
dspace.entity.typePublication
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relation.isAuthorOfPublication.latestForDiscoveryf5e39bee-bc9f-4109-9db3-aedd3076e1fc

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