Characterization of Multi-Decadal Beach Changes in Cartagena Bay (Valparaíso, Chile) from Satellite Imagery

dc.article.number2360
dc.catalogadordfo
dc.contributor.authorBriceno de Urbaneja I.C.
dc.contributor.authorPardo-Pascual J.E.
dc.contributor.authorCabezas-Rabadan C.
dc.contributor.authorAguirre C.
dc.contributor.authorMártinez Reyes, Carolina Del Pilar
dc.contributor.authorPerez-Martinez W.
dc.contributor.authorPalomar-Vazquez J.
dc.date.accessioned2025-01-08T14:05:56Z
dc.date.available2025-01-08T14:05:56Z
dc.date.issued2024
dc.description.abstractSandy coastlines are very dynamic spaces affected by a variety of natural and human factors. In Central Chile, changes in oceanographic and wave conditions, modes of inter-annual climate variability such as El Niño Southern Oscillation (ENSO), and extreme events such as earthquakes and tsunamis condition the beach morphology. At the same time, direct human actions alter the arrival of sediments to the coast and their alongshore distribution. Despite the relevance of the beaches for this coastal region and the interesting relationship their morphology has with the aforementioned factors, there is a lack of robust morphological datasets to provide a deep characterization and understanding of the dynamism of the Chilean coast. Based on the information provided by satellite-derived shorelines (SDSs) defined by using the SHOREX algorithm, this paper characterizes the morphological changes of Playa Grande in Cartagena Bay (Central Chile) during the period 1985–2019. The shoreline position data are analyzed in the context of changing beach transforming elements, allowing for a better understanding of the changes according to multiple drivers. While some of these factors, such as earthquakes or coastal storms, have a punctual character, changes in wave patterns vary at different time scales, from seasonal to multi-annual, linked to climate phases such as ENSO. Its effects are translated into shoreline erosion and accretion conditioned by the morphology and orientation of the coast while influenced by the availability of sediment in the coastal system. According to that, a conceptual model of the dynamism and redistribution of sediment in the Bay of Cartagena is proposed. The work proves the high utility that the systematic analysis of multi-decadal SDS datasets obtained from the images acquired in the optical by the Landsat and Sentinel-2 offer for beach monitoring and understanding the coastal dynamism.
dc.fechaingreso.objetodigital2025-01-08
dc.fuente.origenSCOPUS
dc.identifier.doi10.3390/rs16132360
dc.identifier.issn2072-4292
dc.identifier.scopusidSCOPUS_ID:85198331241
dc.identifier.urihttps://doi.org/10.3390/ rs16132360
dc.identifier.urihttps://repositorio.uc.cl/handle/11534/89560
dc.information.autorucInstituto de Geografía; Martinez Reyes Carolina Del Pilar; 0000-0002-7631-5311; 249883
dc.language.isoen
dc.nota.accesoContenido completo
dc.revistaRemote Sensing
dc.rightsacceso abierto
dc.rights.licenseAttribution 4.0 International (CC BY 4.0)
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/deed.es
dc.subjectBeach monitoring
dc.subjectCentral Chile
dc.subjectCoastal erosion
dc.subjectENSO phenomenon
dc.subjectLandsat
dc.subjectCatellite-derived shorelines
dc.subjectSentinel-2
dc.subjectSHOREX
dc.subjectsubpixel waterline definition
dc.subject.ddc550
dc.subject.deweyCiencias de la tierraes_ES
dc.subject.ods15 Life on land
dc.subject.odspa15 Vida de ecosistemas terrestres
dc.titleCharacterization of Multi-Decadal Beach Changes in Cartagena Bay (Valparaíso, Chile) from Satellite Imagery
dc.typeartículo
dc.volumen16
sipa.codpersvinculados249883
sipa.trazabilidadSCOPUS;2024-07-21
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