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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorLUBAC, Bertrand
dc.date.accessioned2024-09-19T11:32:44Z
dc.date.available2024-09-19T11:32:44Z
dc.date.issued2018-02-16
dc.identifier.urioai:crossref.org:10.1002/9781119476726.ch1
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/201683
dc.description.abstractEnThis chapter presents a simple method which allows for the mapping of the bathymetry in the inlet of the Arcachon lagoon as well as the characterization of the temporal evolution of the sediment stock, using multispectral satellite images. It discusses the instantaneous water depth (H), which assumes a negative value, is defined as the vertical distance from the water surface to the bottom at a given time. In coastal shallow waters associated with tidal environments, the variations of H depend first on the phase of the tide. High spatial resolution satellite images (O ~10 m) associated with littoral aquatic systems generally have strong environmental noise, which has to be corrected before any analysis. One of the simplest methods used to characterize and quantify variations in submarine topography is based on the mapping of bathymetry for two distinct dates and then calculating their difference.
dc.language.isoENen_US
dc.publisherJohn Wiley & Sons, Inc.en_US
dc.sourcecrossref
dc.source.titleQGIS and Applications in Water and Risksen_US
dc.title.enMonitoring Coastal Bathymetry Using Multispectral Satellite Images at High Spatial Resolution
dc.typeChapitre d'ouvrageen_US
dc.identifier.doi10.1002/9781119476726.ch1en_US
bordeaux.page1-34en_US
bordeaux.volume4en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamMETHYSen_US
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hal.popularnonen_US
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