Patrones de circulación de corrientes en una zona insular del Caribe y su influencia en la descarga de efluentes. Caso de estudio San Andrés, Colombia
ilustraciones, diagramas, mapas
- Autores:
-
Espinosa Ordoñez, Paula Andrea
- Tipo de recurso:
- Fecha de publicación:
- 2023
- Institución:
- Universidad Nacional de Colombia
- Repositorio:
- Universidad Nacional de Colombia
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.unal.edu.co:unal/85049
- Palabra clave:
- 550 - Ciencias de la tierra
620 - Ingeniería y operaciones afines::627 - Ingeniería hidráulica
Contaminantes del agua
Circulación atmosférica
Efluentes
Atmospheric circulation
Water pollutants
Effluent
Circulación
Corrientes
Olas
Marea
Viento
Trazadores pasivos
Current circulation
Wave-driven
Tide-driven
Wind-driven
Discharge
- Rights
- openAccess
- License
- Atribución-NoComercial-SinDerivadas 4.0 Internacional
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Universidad Nacional de Colombia |
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| dc.title.spa.fl_str_mv |
Patrones de circulación de corrientes en una zona insular del Caribe y su influencia en la descarga de efluentes. Caso de estudio San Andrés, Colombia |
| dc.title.translated.eng.fl_str_mv |
Currents and circulation patterns in a Caribbean Island and their influence on effluent discharge. Case study: San Andrés, Colombia |
| title |
Patrones de circulación de corrientes en una zona insular del Caribe y su influencia en la descarga de efluentes. Caso de estudio San Andrés, Colombia |
| spellingShingle |
Patrones de circulación de corrientes en una zona insular del Caribe y su influencia en la descarga de efluentes. Caso de estudio San Andrés, Colombia 550 - Ciencias de la tierra 620 - Ingeniería y operaciones afines::627 - Ingeniería hidráulica Contaminantes del agua Circulación atmosférica Efluentes Atmospheric circulation Water pollutants Effluent Circulación Corrientes Olas Marea Viento Trazadores pasivos Current circulation Wave-driven Tide-driven Wind-driven Discharge |
| title_short |
Patrones de circulación de corrientes en una zona insular del Caribe y su influencia en la descarga de efluentes. Caso de estudio San Andrés, Colombia |
| title_full |
Patrones de circulación de corrientes en una zona insular del Caribe y su influencia en la descarga de efluentes. Caso de estudio San Andrés, Colombia |
| title_fullStr |
Patrones de circulación de corrientes en una zona insular del Caribe y su influencia en la descarga de efluentes. Caso de estudio San Andrés, Colombia |
| title_full_unstemmed |
Patrones de circulación de corrientes en una zona insular del Caribe y su influencia en la descarga de efluentes. Caso de estudio San Andrés, Colombia |
| title_sort |
Patrones de circulación de corrientes en una zona insular del Caribe y su influencia en la descarga de efluentes. Caso de estudio San Andrés, Colombia |
| dc.creator.fl_str_mv |
Espinosa Ordoñez, Paula Andrea |
| dc.contributor.advisor.none.fl_str_mv |
Osorio Arias, Andres Fernando Osorio Cano, Juan David |
| dc.contributor.author.none.fl_str_mv |
Espinosa Ordoñez, Paula Andrea |
| dc.contributor.researchgroup.spa.fl_str_mv |
Oceanicos Grupo de Oceanografía E Ingeniería Costera de la Universidad Nacional |
| dc.contributor.orcid.spa.fl_str_mv |
Osorio Cano, Juan David [0000-0002-5324-7790] |
| dc.subject.ddc.spa.fl_str_mv |
550 - Ciencias de la tierra 620 - Ingeniería y operaciones afines::627 - Ingeniería hidráulica |
| topic |
550 - Ciencias de la tierra 620 - Ingeniería y operaciones afines::627 - Ingeniería hidráulica Contaminantes del agua Circulación atmosférica Efluentes Atmospheric circulation Water pollutants Effluent Circulación Corrientes Olas Marea Viento Trazadores pasivos Current circulation Wave-driven Tide-driven Wind-driven Discharge |
| dc.subject.armarc.spa.fl_str_mv |
Contaminantes del agua |
| dc.subject.lemb.spa.fl_str_mv |
Circulación atmosférica Efluentes |
| dc.subject.lemb.eng.fl_str_mv |
Atmospheric circulation Water pollutants Effluent |
| dc.subject.proposal.spa.fl_str_mv |
Circulación Corrientes Olas Marea Viento Trazadores pasivos |
| dc.subject.proposal.eng.fl_str_mv |
Current circulation Wave-driven Tide-driven Wind-driven Discharge |
| description |
ilustraciones, diagramas, mapas |
| publishDate |
2023 |
| dc.date.accessioned.none.fl_str_mv |
2023-12-06T20:53:28Z |
| dc.date.available.none.fl_str_mv |
2023-12-06T20:53:28Z |
| dc.date.issued.none.fl_str_mv |
2023-08-01 |
| dc.type.spa.fl_str_mv |
Trabajo de grado - Maestría |
| dc.type.driver.spa.fl_str_mv |
info:eu-repo/semantics/masterThesis |
| dc.type.version.spa.fl_str_mv |
info:eu-repo/semantics/acceptedVersion |
| dc.type.content.spa.fl_str_mv |
Text |
| dc.type.redcol.spa.fl_str_mv |
http://purl.org/redcol/resource_type/TM |
| status_str |
acceptedVersion |
| dc.identifier.uri.none.fl_str_mv |
https://repositorio.unal.edu.co/handle/unal/85049 |
| dc.identifier.instname.spa.fl_str_mv |
Universidad Nacional de Colombia |
| dc.identifier.reponame.spa.fl_str_mv |
Repositorio Institucional Universidad Nacional de Colombia |
| dc.identifier.repourl.spa.fl_str_mv |
https://repositorio.unal.edu.co/ |
| url |
https://repositorio.unal.edu.co/handle/unal/85049 https://repositorio.unal.edu.co/ |
| identifier_str_mv |
Universidad Nacional de Colombia Repositorio Institucional Universidad Nacional de Colombia |
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spa |
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spa |
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RedCol LaReferencia |
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Delft3D-FLOW User Manual Hydro-Morphodynamics. 710. Deltares, D. (2019). Conceptual Description - Wave current interaction. En Delft3D-Flow User Manual (p. 230). Diaz, J. M., Barrios, L. M., Cendales, M. H., Garzón, J., Geister, J., López, M., Ospina, G. H., Parra, F., Pinzón, J., Vargas, B., Zapata, F., & Zea, S. (2000). Áreas Coralinas de Colombia. En J. M. Diaz (Ed.), Invemar: Vol. Sereie de (Número November). Egon, A. (2009). Hydrodynamics of Lagoon Fringed by a Coral Reef. Escobar, C. A., Velásquez, L., & Posada, F. (2015). Marine Currents in the Gulf of Urabá, Colombian Caribbean Sea. Journal of Coastal Research, 31(6), 1363-1374. https://doi.org/10.2112/JCOASTRES-D-14-00186.1 Espinosa-Ordoñez, P. A. (2020). Estudio de la disipación del oleaje en un arrecife de coral: Caso de estudio Isla de San Andrés, Colombia [Tesis de pregrado]. Universidad Nacional de Colombia. Ezer, T., Heyman, W. D., Houser, C., & Kjerfve, B. (2012). 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(2007b). Reef Environments and Geology of an Oceanic Archipelago: San Andrés, Old Providence and Sta. Catalina (Caribbean Sea, Colombia). 104. Gómez Giraldo, A., Osorio, A., Toro, F., Osorio, J., Álvarez, O., & Arrieta, A. (2009). Patrón de circulación en Bahía Barbacoas y su influencia sobre el transporte de sedimentos hacia las islas del Rosario. Avances en Recursos Hidráulicos, 20, 21-39. Gonzáles, O. C., & Hurtado, G. (2012). Caracterización climática del archipiélago de San Andrés y Providencia. pp (48-52) en CORALINA-INVEMAR, 2012. Gómez-López, D. I., C. Segura-Quintero, P. C. Sierra-Correa y J. Garay-Tinoco (Eds). Atlas de la Reserva de Biósfera Seaflower. Archipiélago de. En Serie de publicaciones especiales, Invema, No. 28, p. 180 (28.a ed., Vol. 28). Serie de Publicaciones Especiales INVEMAR. http://www.invemar.org.co/redcostera1/invemar/docs/10447AtlasSAISeaflower.pdf Grimaldi, C. M., Lowe, R. J., Benthuysen, J. A., Green, R. H., Reyns, J., Kernkamp, H., & Gilmour, J. 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Application of an unstructured 3D finite volume numerical model to flows and salinity dynamics in the San Francisco Bay-Delta. Estuarine, Coastal and Shelf Science, 192, 86-107. https://doi.org/10.1016/j.ecss.2017.04.024 Massel, S. R. (1989). Currents in coastal zone. En Elsevier Oceanography Series (Ed.), Hydrodynamics Of Coastal Zones (Vol. 48, pp. 253-275). Monismith, S. G., Herdman, L. M. M., Ahmerkamp, S., & Hench, J. L. (2013). Wave Transformation and Wave-Driven Flow across a Steep Coral Reef. Journal of Physical Oceanography, 43(7), 1356-1379. https://doi.org/10.1175/JPO-D-12-0164.1 Monismith, S. G., Rogers, J. S., Koweek, D., & Dunbar, R. B. (2015). Frictional wave dissipation on a remarkably rough reef. Geophysical Research Letters, 42(10), 4063-4071. https://doi.org/10.1002/2015GL063804 Montoya, R. D., Menendez, M., & Osorio, A. F. (2018). Exploring changes in Caribbean hurricane-induced wave heights. 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Universidad Nacional de Colombia. Ortiz, J. C., Plazas, J. M., & Lizano, O. (2015). Evaluation of Extreme Waves Associated with Cyclonic Activity on San Andrés Island in the Caribbean Sea since 1900. Journal of Coastal Research, 313(Figure 2), 557-568. https://doi.org/10.2112/jcoastres-d-14-00072.1 Ortiz Royero, J. C., Plazas, J. M., & Lizano, O. (2015). Evaluation of Extreme Waves Associated with Cyclonic Activity on San Andrés Island in the Caribbean Sea since 1900. Journal of Coastal Research, 31(3), 557-568. https://doi.org/10.2112/JCOASTRES-D-14-00072.1 Osorio, A. F., Montoya, R. D., Ortiz, J. C., & Peláez, D. (2016). Construction of synthetic ocean wave series along the Colombian Caribbean Coast: A wave climate analysis. Applied Ocean Research, 56, 119-131. https://doi.org/10.1016/j.apor.2016.01.004 Osorio, A. F., Santiago Peláez-Zapata, D., Guerrero-Gallego, J., Álvarez-Silva, O., David Osorio-Cano, J., Toro, F. M., & Giraldo, A. (2014). Hidrodinámica aplicada a la gestión y la conservación de ecosistemas marinos y costeros: Isla Gorgona, Océano Pacífico Colombiano. En Rev. Biol. Trop. (Int. J. Trop. Biol. ISSN (Vol. 62). Osorio-Cano, J. D., Alcérreca-Huerta, J. C., Osorio, A. F., & Oumeraci, H. (2018). CFD modelling of wave damping over a fringing reef in the Colombian Caribbean. Coral Reefs, 37(4), 1093-1108. https://doi.org/10.1007/s00338-018-1736-4 Pérez-Santos, I., Garcés-Vargas, J., Schneider, W., Ross, L., Parra, S., & Valle-Levinson, A. (2014). Double-diffusive layering and mixing in Patagonian fjords. https://doi.org/10.1016/j.pocean.2014.03.012 Piccolo, M. C. (2021). Chapter 12 - Effects of rainfall extreme events on coastal marine ecosystems. En J. Rodrigo-Comino (Ed.), Precipitation (pp. 261-285). Elsevier. https://doi.org/https://doi.org/10.1016/B978-0-12-822699-5.00024-0 Piecuch, C. G., & Ponte, R. M. (2012). Buoyancy-driven interannual sea level changes in the southeast tropical Pacific. Geophysical Research Letters, 39(5). https://doi.org/10.1029/2012GL051130 Rey, W., Ruiz-Salcines, P., Salles, P., Urbano-Latorre, C. P., Escobar-Olaya, G., Osorio, A. F., Ramírez, J. P., Cabarcas-Mier, A., Jigena-Antelo, B., & Appendini, C. M. (2021). Hurricane Flood Hazard Assessment for the Archipelago of San Andres, Providencia and Santa Catalina, Colombia. Frontiers in Marine Science, 8. https://doi.org/10.3389/fmars.2021.766258 Ricaurte, C., Morales, D. F., Coca, O., Bastidad, M. L., & Romero, D. A. (2015). Erosión costera en la isla de san andrés informe técnico final. Invemar, 72. Rogers, J. S., Monismith, S. G., Koweek, D. A., & Dunbar, R. B. (2016). Wave dynamics of a Pacific Atoll with high frictional effects. Journal of Geophysical Research: Oceans, 121, 350-367. https://doi.org/10.1002/jgrc.20224 Soliman, M. N., Guen, F. Z., Ahmed, S. A., Saleem, H., Khalil, M. J., & Zaidi, S. J. (2021). Energy consumption and environmental impact assessment of desalination plants and brine disposal strategies. Process Safety and Environmental Protection, 147, 589-608. https://doi.org/10.1016/j.psep.2020.12.038 Spall, M. A. (2002). Wind- and buoyancy-forced upper ocean circulation in two-strait marginal seas with application to the Japan/East Sea. Journal of Geophysical Research: Oceans, 107(C1), 6-1. https://doi.org/10.1029/2001JC000966 Stevens, C., Ward, B., Law, C., & Walkington, M. (2010). Surface layer mixing during the SAGE ocean fertilization experiment. https://doi.org/10.1016/j.dsr2.2010.10.017 Sun, Z., Xu, D., Liu, X., Zhang, H., & Cai, Z. (2021). Observation and simulation of wind waves near a typical reef lagoon in South China Sea. Journal of Hydrodynamics, 33(1), 24-32. https://doi.org/10.1007/s42241-021-0010-3 Taebi, S., Lowe, R. J., Pattiaratchi, C. B., Ivey, G. N., & Symonds, G. (2012). A numerical study of the dynamics of the wave-driven circulation within a fringing reef system. Ocean Dynamics, 62(4), 585-602. https://doi.org/10.1007/s10236-011-0514-4 Telesford, J. N. (2021). Critiquing «islandness» as immunity to COVID-19: A case exploration of the Grenada, Carriacou and Petite Martinique archipelago in the Caribbean region. Island Studies Journal, 16(1), 308-324. https://doi.org/10.24043/isj.155 Thomas, Y. F., Nicolae-Lerma, A., & Posada, B. (2012). Atlas climatológico del Mar Caribe Colombiano. En Serie de Publicaciones especiales (Número 25). Tippins, D., & Tomczak, M. (2003). Meridional Turner angles and density compensation in the upper ocean. Ocean Dynamics, 53(4), 332-342. https://doi.org/10.1007/s10236-003-0056-5 Troost, T. A., de Kluijver, A., & Los, F. J. (2014). Evaluation of eutrophication variables and thresholds in the Dutch North Sea in a historical context — A model analysis. 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Communications Earth & Environment, 2(1), 46. https://doi.org/10.1038/s43247-021-00113-x Velásquez, C. (2020). The 2016 Water Crisis in San Andres Island: An Opportunity for Change? Ciencia Política, 15(29), 73-109. https://doi.org/10.15446/cp.v15n29.86373 Walstra, D. J. R., Roelvink, J. A., & Groeneweg, J. (2000). Calculation of Wave-Driven Currents in a 3D Mean Flow Model. Coastal Engineering, 1050-1063. https://doi.org/10.1061/40549(276)81 Winter, G., Van Dongeren, A., De Schipper, M., & Van Thiel De Vries, J. (2012). A FIELD AND NUMERICAL STUDY INTO RIP CURRENTS IN WIND-SEA DOMINATED ENVIRONMENTS. Coastal Engineering Proceedings, 1(33), currents.36. https://doi.org/10.9753/icce.v33.currents.36 Yamano, H., Kayanne, H., Yonekura, N., Nakamura, H., & Kudo, K. (1998). Water circulation in a fringing reef located in a monsoon area: Kabira Reef, Ishigaki Island, Southwest Japan. Coral Reefs, 17(1), 89-99. https://doi.org/10.1007/s003380050101 Yao, Y., Huang, Z., He, W., & Monismith, S. G. (2018). Wave-induced setup and wave-driven current over Quasi-2DH reef-lagoon-channel systems. Coastal Engineering, 138, 113-125. https://doi.org/https://doi.org/10.1016/j.coastaleng.2018.04.009 Yao, Y., Liu, Y., Chen, L., Deng, Z., & Jiang, C. (2020). Study on the wave-driven current around the surf zone over fringing reefs. https://doi.org/10.1016/j.oceaneng.2020.106968 You, Y. (2002). A global ocean climatological atlas of the Turner angle: implications for double-diffusion and water-mass structure. En Deep-Sea Research I (Vol. 49). Zea, S., Geister, J., Garzon-Ferreira, J., & Diaz, J. M. (1998). Biotic changes in the reef complex of San Andres Island (Southeastern Caribbean Sea, Columbia) occuring over three decades. Atoll Research Bulletin, 456(456), 1-30. https://doi.org/10.5479/si.00775630.456.1 Zheng, J., Yao, Y., Chen, S., Chen, S., & Zhang, Q. (2020). Laboratory study on wave-induced setup and wave-driven current in a 2DH reef-lagoon-channel system. https://doi.org/10.1016/j.coastaleng.2020.103772 |
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Atribución-NoComercial-SinDerivadas 4.0 Internacionalhttp://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Osorio Arias, Andres Fernando81cc941243fa5b804b2287c6f5d32cf2Osorio Cano, Juan David5b24aa226d5883f38fcbd2fc56739f96Espinosa Ordoñez, Paula Andrea4873121d277721e945d68e128901fa9dOceanicos Grupo de Oceanografía E Ingeniería Costera de la Universidad NacionalOsorio Cano, Juan David [0000-0002-5324-7790]2023-12-06T20:53:28Z2023-12-06T20:53:28Z2023-08-01https://repositorio.unal.edu.co/handle/unal/85049Universidad Nacional de ColombiaRepositorio Institucional Universidad Nacional de Colombiahttps://repositorio.unal.edu.co/ilustraciones, diagramas, mapasLos patrones de circulación de corrientes en aguas poco profundas pueden controlar procesos claves como el transporte y difusión de efluentes. En este estudio, se investigaron los patrones de circulación de corrientes y la influencia sobre las descargas de efluentes en la isla de San Andrés ubicada al noroeste del mar Caribe. Para caracterizar estos patrones se empleó el modelo numérico acoplado de olas y corrientes Delft Wave-Flow, calibrado y validado con datos de campo de corrientes, olas y marea. Los resultados revelaron que la marea ejerce una mayor influencia en la laguna arrecifal con velocidades entre 0.01 ms-1 y 0.04 ms-1. Las corrientes influenciadas por las olas alcanzaron velocidades entre 0.3 ms-1 - 0.75 ms-1 sobre la cresta de la barrera arrecifal. El viento ejerce influencia sobre las corrientes generando magnitudes de velocidad que oscilan entre 0.2 ms-1 y 0.8 ms-1 en la cresta de los arrecifes y en aguas poco profundas del oeste de la isla. En el análisis de estacionalidad de las corrientes, se encontró que durante el trimestre de diciembre, enero y febrero las magnitudes de las corrientes son máximas y pueden variar entre 0.6 ms-1 a 0.8 ms-1, mientras que para el trimestre de septiembre, octubre y noviembre las corrientes son mínimas con valores entre 0.15 ms-1 a 0.35 ms-1. Los escenarios de eventos sintéticos extremos muestran que las corrientes pueden alcanzar velocidades entre 0.75 ms-1 y 1.2 ms-1 cuando se propagan olas desde el norte con una altura de ola significante de 3.5 m. Finalmente se evaluó el transporte de las descargas de efluentes en el costado oeste y al norte de la isla, bajo condiciones estacionales y extremas. En condiciones extremas se encontró que el 10% de la concentración de la descarga en el norte cubre áreas de la isla con presencia de ecosistemas marinos sensibles tales como, corales, pastos y manglares. El presente estudio permitiría contribuir a la formulación de lineamientos técnicos y toma de decisiones informadas en relación con la protección y conservación de los ecosistemas costeros, así como la gestión sostenible de los recursos marinos. (Texto tomado de la fuente)Current circulation patterns in shallow waters can control key processes such as effluent transport and diffusion. This study investigated current circulation patterns and their influence on effluent discharge on San Andres Island in the northwestern Caribbean Sea. The Delft Wave-Flow coupled numerical wave-current model, calibrated, and validated with current, wave, and tidal field data, was used to characterize these patterns. The results revealed that the tide exerts an influence on the reef lagoon with velocities between 0.01 ms-1 and 0.04 ms-1. Wave-influenced currents reached velocities between 0.3 ms-1to 0.75 ms-1at the coral reef crest. Wind influences the currents, generating velocity magnitudes ranging from 0.2 ms-1 to 0.8 ms-1. In the analysis of the seasonality of currents, we found that during the December, January, and February quarters, the magnitudes of currents are maximum and can vary between 0.6 ms-1to 0.8 ms-1, while for the September, October, and November quarters, the currents are minimal, with values between 0.15 ms-1 to 0.35 ms-1. The extreme synthetic event scenarios show that currents can reach velocities of 0.75 ms-1 and 1.2 ms-1 whit waves from the north with a significant wave height of 3.5 m. Finally, we evaluated the transport of effluent discharges on the west and north sides of the island under seasonal and extreme conditions. Under extreme conditions, 10% of the discharge concentration in the north covers areas of the island with marine ecosystems such as corals, grasses, and mangroves. This study contributes to the formulation of technical guidelines and informed decision-making concerning the protection and conservation of coastal ecosystems and the sustainable management of marine resources.Universidad Nacional de ColombiaFundación Universidad del Norte de BarranquillaMaestríaMagíster en Ingeniería - Recursos Hidráulicos- Mediciones de campo - Análsis de datos de campo - Implementación de modelos hidrodinámicosIngeniería de puertos y costasÁrea Curricular de Medio Ambiente105 páginasapplication/pdfspaUniversidad Nacional de ColombiaMedellín - Minas - Maestría en Ingeniería - Recursos HidráulicosFacultad de MinasMedellín, ColombiaUniversidad Nacional de Colombia - Sede Medellín550 - Ciencias de la tierra620 - Ingeniería y operaciones afines::627 - Ingeniería hidráulicaContaminantes del aguaCirculación atmosféricaEfluentesAtmospheric circulationWater pollutantsEffluentCirculaciónCorrientesOlasMareaVientoTrazadores pasivosCurrent circulationWave-drivenTide-drivenWind-drivenDischargePatrones de circulación de corrientes en una zona insular del Caribe y su influencia en la descarga de efluentes. Caso de estudio San Andrés, ColombiaCurrents and circulation patterns in a Caribbean Island and their influence on effluent discharge. Case study: San Andrés, ColombiaTrabajo de grado - Maestríainfo:eu-repo/semantics/masterThesisinfo:eu-repo/semantics/acceptedVersionTexthttp://purl.org/redcol/resource_type/TMSan Andres (Isla), ColombiaRedColLaReferenciaAdcroft, A., Hallberg, R., Dunne, J. P., Samuels, B. L., Galt, J. A., Barker, C. H., & Payton, D. (2010). Simulations of underwater plumes of dissolved oil in the Gulf of Mexico. Geophysical Research Letters, 37(18). https://doi.org/10.1029/2010GL044689Akter, A., & Tanim, A. H. (2021). Salinity Distribution in River Network of a Partially Mixed Estuary. Journal of Waterway, Port, Coastal, and Ocean Engineering, 147(2), 04020055. https://doi.org/10.1061/(asce)ww.1943-5460.0000621Albarakati, A. M. A., Ahmad, F., Albarakati, A. M. A., & Ahmad, F. (2012). 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(2019). Encuesta de hábitat y usos socioeconómicos, 2019 archipiélago de San Andrés, Providencia y Santa Catalina.DANE. (2020). Boletín Técnico Encuesta de Hábitat y Usos Socioeconómicos 2019.Deltares. (2014). Delft3D-FLOW User Manual Hydro-Morphodynamics. 710.Deltares, D. (2019). Conceptual Description - Wave current interaction. En Delft3D-Flow User Manual (p. 230).Diaz, J. M., Barrios, L. M., Cendales, M. H., Garzón, J., Geister, J., López, M., Ospina, G. H., Parra, F., Pinzón, J., Vargas, B., Zapata, F., & Zea, S. (2000). Áreas Coralinas de Colombia. En J. M. Diaz (Ed.), Invemar: Vol. Sereie de (Número November).Egon, A. (2009). Hydrodynamics of Lagoon Fringed by a Coral Reef.Escobar, C. A., Velásquez, L., & Posada, F. (2015). Marine Currents in the Gulf of Urabá, Colombian Caribbean Sea. Journal of Coastal Research, 31(6), 1363-1374. https://doi.org/10.2112/JCOASTRES-D-14-00186.1Espinosa-Ordoñez, P. A. (2020). 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Laboratory study on wave-induced setup and wave-driven current in a 2DH reef-lagoon-channel system. https://doi.org/10.1016/j.coastaleng.2020.103772Análisis de impactos ambientales en sistemas acoplados de desalinización de agua de mar (DAM) - generación de energía de gradiente salino (EGS) y planteamiento de medidas preventivasMinisterio de Ciencia Tecnología e InnovaciónAdministradoresConsejerosEstudiantesGrupos comunitariosInvestigadoresMaestrosMedios de comunicaciónPúblico generalResponsables políticosLICENSElicense.txtlicense.txttext/plain; charset=utf-85879https://repositorio.unal.edu.co/bitstream/unal/85049/1/license.txteb34b1cf90b7e1103fc9dfd26be24b4aMD51ORIGINAL1017233648.2023.pdf1017233648.2023.pdfTesis de Maestría en Ingeniería - Recursos Hidráulicosapplication/pdf33391024https://repositorio.unal.edu.co/bitstream/unal/85049/2/1017233648.2023.pdfa60d1938cea4f5d6e71dd576384f0002MD52THUMBNAIL1017233648.2023.pdf.jpg1017233648.2023.pdf.jpgGenerated 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