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dc.contributor.advisorRestrepo López, Juan Camilo
dc.contributor.advisorEscobar Jaramillo, Jaime Humberto
dc.contributor.authorTorregroza Espinosa, Ana Carolina
dc.date.accessioned2020-08-06T16:43:50Z
dc.date.available2020-08-06T16:43:50Z
dc.date.issued2020
dc.identifier.urihttp://hdl.handle.net/10584/8954
dc.descriptionThe characteristics of estuaries depend mainly on the magnitude and variability of river discharge and tidal forcing (Kjerfve, 1994). Estuaries present strong temporal and spatial gradients with respect to their physical, chemical and biological properties, as a result of changes in fluvial contributions (Nogueira et al., 1997). Therefore, biogeochemical processes are extremely complex (Fourqurean et al., 1993; Fernández-Nóvoa et al., 2015). Temperature and salinity are the most relevant features of coastal marine ecosystem dynamics (Urquhart et al., 2013), as variations in these parameters can influence the movement of water masses, water column stratification caused by density differences, transport of sediments, and mixing conditions (Bianchi, 2007; Geyer, 2010; Obeso-Nieblas et al., 2012; Osadchiev et al., 2017). Also, temperature and salinity may play roles in nutrient distributions and concentrations (Windom et al., 2006), and biogeochemical processes and ecological productivity, through alterations in biochemical reactions that regulate the enzymatic processes of respiration and photosynthesis (Xia and Jiang, 2015; Quamrul et al., 2016). The physical dynamics of estuaries/deltas of the micro-tidal domain, which are highly stratified and turbid, have been little studied. Therefore, we lack detailed knowledge regarding relationships among spatio-temporal variations in salinity and temperature, the extent and structure of convergence fronts and the mixed layer, nutrient distribution and primary productivity in this type of estuary.es_ES
dc.formatapplication/pdfes_ES
dc.language.isoenges_ES
dc.publisherUniversidad del Nortees_ES
dc.subjectSalinidades_ES
dc.subjectSedimentos marinoses_ES
dc.titleSpatio-temporal distribution of temperature, salinity and suspended sediment on the deltaic front of the Magdalena River: Influence on nutrient concentration and primary productivityes_ES
dc.typedoctoralThesises_ES
dc.rights.accessRightsopenAccesses_ES
dc.type.hasVersionacceptedVersiones_ES
dc.publisher.programDoctorado en Ciencias del mares_ES
dc.publisher.departmentDepartamento de Física y Geocienciases_ES
dc.creator.degreeDoctor en Ciencias del mares_ES


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