PROY P YECTTO B BASEE DE DATTOS BID – B – CM MAR Fund dació ón M Malp pelo y otros Ecosisstem mas M Marinoss Bibliograffía TEM MA: M MED DIO A AMB BIENTE Hidrodináámica // Deltaas CON NSULTOR: Ing. JHON FA ABIO BARREETO M. SUPERVISSOR: Dr. JULLIÁN BOTERO O Director Proyecto B BID –CMAR ASESOR R TÉCNICO CIIENTÍFICO: D Dr. VLADIMIIR PUENTES Faccilitador Colombia ASISTTENTE LOCALL: ASTRID M MONCALEAN NO RUBIO Apoyyo logístico CColombia BOGOTTÁ D.C. COLO OMBIA, OCTTUBRE DE 20011 1 Categoría principal Subcategorías País origen Autor(es) Personal(es) Entidad(es) relacionada(s) Título Año publicación Documento fuente Temas Ubicación física E-mail contacto Localización Web (URL) Resumen Categoría principal Subcategorías País origen Autor(es) Personal(es) Entidad(es) relacionada(s) Título Año publicación Documento fuente Temas Localización Web (URL) Resumen Medio Ambiente Hidrodinámica / Deltas / Ríos Colombia Restrepo, Juan D. / Kjerfve, Björn / Correa, Iván D. / González, Juan Universidad Nacional de Colombia, Sede Medellin Morphodynamics of a high discharge tropical delta, San Juan River, Pacific coast of Colombia 2002 Base de datos Science Direct Delta del rio San Juan Consulta gratis en la Hemeroteca Nacional [email protected] www.elsevier.com/locate/margeo The San Juan River has one of the most extensive and best developed deltas on the Pacific coast of South America, measuring 800 Km2. The river drainage basin measures 16465 Km2 and is located in one of the areas with the highest precipitation in the western hemisphere. The annual rainfall varies from 7000 to 11000 mm, and as a result the San juan River has the highest water discharge (2550 m3 s-1), sediment load (16x10 Medio Ambiente Hidrodinámica / Deltas / Ríos Colombia Restrepo, Juan D. / Kjerfve, Björn Department of Geological Sciences, Marine Science Program, University of South Carolina / Escuela de Ingenierías, Departamento de Geología, Area de Ciencias del Mar, Universidad EAFIT The San Juan Delta, Colombia: Tides, circulations, and salt dispersion 2002 Base de datos Science Direct Delta del Río San Juan http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6VBJ-44SK43N-1&_u ser=10&_coverDate=05%2F31%2F2002&_rdoc=1&_fmt=high&_orig=search&_sort=d &_docanchor=&view=c&_searchStrId=1438214766&_rerunOrigin=google&_acct=C00 0050221&_version=1&_urlVersion=0&_userid=10&md5=a4a1e8e57b4487f5241750c e8b128b37 The San Juan River delta (Colombia) with an area of 800 km2 is the largest delta environment on the Pacific coast of South America. It consists of active distributaries maintained by an average discharge of 2500 m3 s?1, is tide dominated, and has relatively narrow estuarine mixing zones <17 km wide and typically 7 km wide. Water level and current time series in two distributary mouths indicate that the tide is semidiurnal with a form number 0.1- 0.2 and a mean range of 3 m. Processes at tidal frequencies explain 75-95% of the water level variability with the remaining low-frequency variability attributed to meteorological forcing and river processes. The tidal phase for the main diurnal and semidiurnal constituents progress from north to south along the coast. Only the southernmost distributary experiences significant tidal asymmetry as a result of strong river discharge and shallow depths. In the northernmost distributary, shallow water constituents are insignificant. Tidal currents were more semidiurnal than the water level, with form number 0.09-0.13. Tidal ellipses indicated that currents were aligned with the channels and mean amplitudes <1 m s?1. In the delta distributaries, circulation modes varied from seaward flow at all depths during intermediate runoff conditions to gravitational circulation during rising and high discharge periods. In San Juan and Chavica distributaries, the currents were 2 ebb-directed, while in Charambirá they were flood-directed. The circulation appears to be controlled by the morphology of the distributaries, which were weakly stratified and only sometimes moderately stratified. The net salt transport was directed seaward in San Juan and Charambirá, and landward at Chavica, indicating an imbalance in the salt budget, and signifying non-steady state behavior. The net longitudinal salt flux in the San Juan delta is largely a balance between ebb-directed advective flux, and flood-directed tidal sloshing. Along the distributary channels, fringing vegetation is controlled by freshwater discharge, longitudinal distribution of salinity, and morphology. In the most active distributaries, Chavica and San Juan, the vegetation setting is strongly shaped by the short estuarine zone, and mangroves only occur 5 km upstream of any distributary mouth, whereas in the tide-dominated distributaries, Charambirá and Cacahual, dense mangroves intrude 14 and 17 km upstream, respectively. Also, salt dispersion, tidal intrusion, salinity distribution, and mangrove extent in the San Juan delta agree qualitatively with the productive coastal fishery at the tide-dominated distributaries. 3