Climatología del transporte potencial de sedimentos costeros inducido por oleaje en la Isla San Andrés
ilustraciones, gráficas, tablas
- Autores:
-
Olarte Cáceres, Paloma Marina
- Tipo de recurso:
- Fecha de publicación:
- 2019
- Institución:
- Universidad Nacional de Colombia
- Repositorio:
- Universidad Nacional de Colombia
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.unal.edu.co:unal/77571
- Palabra clave:
- 620 - Ingeniería y operaciones afines::627 - Ingeniería hidráulica
Oleaje
Transporte potencial longitudinal de sedimentos
San Andres Isla
Eventos extremos
Erosion costera
Waves
Potential longshore sediment transport
San Andres Island
Extreme events
Costal erosion
- Rights
- openAccess
- License
- Atribución-NoComercial-SinDerivadas 4.0 Internacional
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| dc.title.spa.fl_str_mv |
Climatología del transporte potencial de sedimentos costeros inducido por oleaje en la Isla San Andrés |
| dc.title.translated.eng.fl_str_mv |
Climatology of the potential coastal sediment transport induced by waves in San Andres island |
| title |
Climatología del transporte potencial de sedimentos costeros inducido por oleaje en la Isla San Andrés |
| spellingShingle |
Climatología del transporte potencial de sedimentos costeros inducido por oleaje en la Isla San Andrés 620 - Ingeniería y operaciones afines::627 - Ingeniería hidráulica Oleaje Transporte potencial longitudinal de sedimentos San Andres Isla Eventos extremos Erosion costera Waves Potential longshore sediment transport San Andres Island Extreme events Costal erosion |
| title_short |
Climatología del transporte potencial de sedimentos costeros inducido por oleaje en la Isla San Andrés |
| title_full |
Climatología del transporte potencial de sedimentos costeros inducido por oleaje en la Isla San Andrés |
| title_fullStr |
Climatología del transporte potencial de sedimentos costeros inducido por oleaje en la Isla San Andrés |
| title_full_unstemmed |
Climatología del transporte potencial de sedimentos costeros inducido por oleaje en la Isla San Andrés |
| title_sort |
Climatología del transporte potencial de sedimentos costeros inducido por oleaje en la Isla San Andrés |
| dc.creator.fl_str_mv |
Olarte Cáceres, Paloma Marina |
| dc.contributor.advisor.spa.fl_str_mv |
Bernal Franco, Gladys Rocio Osorio Arias, Andrés Fernando |
| dc.contributor.author.spa.fl_str_mv |
Olarte Cáceres, Paloma Marina |
| dc.contributor.researchgroup.spa.fl_str_mv |
OCEANICOS - Grupo de Oceanografía e Ingeniería Costera de la Universidad Nacional |
| dc.subject.ddc.spa.fl_str_mv |
620 - Ingeniería y operaciones afines::627 - Ingeniería hidráulica |
| topic |
620 - Ingeniería y operaciones afines::627 - Ingeniería hidráulica Oleaje Transporte potencial longitudinal de sedimentos San Andres Isla Eventos extremos Erosion costera Waves Potential longshore sediment transport San Andres Island Extreme events Costal erosion |
| dc.subject.proposal.spa.fl_str_mv |
Oleaje Transporte potencial longitudinal de sedimentos San Andres Isla Eventos extremos Erosion costera |
| dc.subject.proposal.eng.fl_str_mv |
Waves Potential longshore sediment transport San Andres Island Extreme events Costal erosion |
| description |
ilustraciones, gráficas, tablas |
| publishDate |
2019 |
| dc.date.issued.spa.fl_str_mv |
2019-07-02 |
| dc.date.accessioned.spa.fl_str_mv |
2020-05-29T17:06:35Z |
| dc.date.available.spa.fl_str_mv |
2020-05-29T17:06:35Z |
| dc.type.spa.fl_str_mv |
Trabajo de grado - Maestría |
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info:eu-repo/semantics/masterThesis |
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info:eu-repo/semantics/acceptedVersion |
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Text |
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http://purl.org/redcol/resource_type/TM |
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https://repositorio.unal.edu.co/handle/unal/77571 |
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Universidad Nacional de Colombia |
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Repositorio Institucional Universidad Nacional de Colombia |
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https://repositorio.unal.edu.co/ |
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https://repositorio.unal.edu.co/handle/unal/77571 https://repositorio.unal.edu.co/ |
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Universidad Nacional de Colombia Repositorio Institucional Universidad Nacional de Colombia |
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spa |
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spa |
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En The proceedings of the coastal sediments 2015. World Scienti c. Bayram, A., Larson, M., y Hanson, H. (2007). A new formula for the total longshore sediment transport rate. Coastal Engineering, 54 (9), 700{710. Bijker, E. W. (1967). Some considerations about scales for coastal models with movable bed. Bijker, E. W. (1971). Longshore transport computations. Journal of the Waterways, Harbors and Coastal Engineering Division, 97 (4), 687{701. Booij, N., Ris, R. C., y Holthuijsen, L. H. (1999). A third-generation wave model for coastal regions: 1. model description and validation. Journal of geophysical research: Oceans, 104 (C4), 7649{7666. Bowen, A. J. (1969). The generation of longshore currents on a plane beach. J. Mar. Res., 27 (2), 206{215. Buckley, M., Lowe, R., y Hansen, J. (2014). Evaluation of nearshore wave models in steep reef environments. Ocean Dynamics, 64 (6), 47{862. Cartier, A., Larroud e, P., y H equette, A. (2013). Longshore sediment transport measurements on sandy macrotidal beaches compared with sediment transport formulae. En Sediment transport processes and their modelling applications. IntechOpen. Castaño-Isaza, J., Newball, R., Roach, B., y Lau, W. W. (2014). Valuing beaches to develop payment for ecosystem services schemes in Colombia's Sea Flower marine protected area. Ecosystem services, 11 , 22{31. CERC. (1984). Shore protection manual, vols. i and ii. Coastal Engineering Research Center, USACE. Christensen, E. D., Walstra, D.-J., y Emerat, N. (2002). Vertical variation of the flow across the surf zone. Coastal Engineering, 45 (3-4), 169{198. Dally, W. R. (2005). Surf zone processes. Encyclopedia of coastal science, 929{935. Davidson-Arnott, R. (2010). Introduction to coastal processes and geomorphology. Cambridge University Press. Davis, R. A., y FitzGerald, D. M. (2009). Beaches and coasts. John Wiley & Sons. del Valle, R., Medina, R., y Losada, M. A. (1993). Dependence of coeficient k on grain size. Journal of waterway, port, coastal, and ocean engineering, 119 (5), 568{574. Devis-Morales, A., Montoya-Sánchez, R., Bernal, G., y Osorio, A. (2017). Assessment of extreme wind and waves in the Colombian Caribbean Sea for offshore applications. Applied Ocean Research, 69 , 10{26. Díaz, J., Barrios, L., Cendales, M., Garzón-Ferreira, J., Geister, J., López-Victoria, M., . . .others (2000). Areas Coralinas de Colombia [Coral areas in Colombia]. Santa Marta, Colombia: Instituto de Investigaciones Marinas y Costeras \José Benito Vives de Andreis"(Invemar), 17{167. Díaz, M., Manuel, J., Díaz-Pulido, G., Garzón-Ferreira, J., Geister, J., Sánchez, J. A., y Zea, S. (1996). Atlas de los arrecifes coralinos del Caribe colombiano: I. complejos arrecifales oceánicos. Esteves, L. S., Williams, J. J., y Lisniowski, M. A. (2009). Measuring and modelling longshore sediment transport. Estuarine, Coastal and Shelf Science, 83 (1), 47{59 Fern andez-Fern andez, S., Baptista, P., Martins, V. A., Silva, P. A., Abreu, T., Pais-Barbosa, J., . . . others (2015). Longshore transport estimation on O r Beach in Northwest Portugal: Sand-tracer experiment. Journal of Waterway, Port, Coastal, and Ocean Engineering, 142 (2), 04015017. Filipot, J.-F., y Cheung, K. F. (2012). Spectral wave modeling in fringing reef environments. Coastal Engineering, 67 , 67{79. Gamboa, L., y Posada, B. O. (2012). Geolog a del archipi elago de San Andr es, Providencia y Santa Catalina. Atlas de la Reserva de Bi osfera Sea Flower: archipi elago de San Andr es, Providencia y Santa Catalina, 36{46. Geister, G., J. Gorin. (2007). Evolution d un archipel oc eanique des Cara bes (San Andr es et Providencia, Colombie). 3 eme Cycle Romand en Sciences de la Terre, Cours de terrain du 14 au 29 septembre 2007 . Geister, J. (1992). Modern reef development and Cenozoic evolution of an oceanic island/reef complex: Isla de Providencia (Western Caribbean Sea, Colombia). Facies, 27 (1), 1. Gonz alez, y Hurtado, G. (2012). Caracterizaci on clim atica del archipi elago de San Andr es y Providencia. pp (48- 52) en CORALINA- INVEMAR, 2012. G omez{L opez, D.I., C. Segura Quintero, P. C. Sierra- Correa y J. Garay- Tinoco (Eds). Atlas de la Reserva de Biosfera Sea Flower. Archipi elago de San Andr es Providencia y Santa Catalina. Instituto de Investigaciones Marinas y Costeras \Jos e Benito Vives D Andr eis"{INVEMAR y Corporaci on para el desarrollo Sostenible del Archipi elago de San Andr es, Providencia y Santa Catalina { CORALINA. Serie de Publicaciones Especiales de INVEMAR 28. Santa Marta-Colombia, 28 , 180 p. Gowthaman, R., Kumar, V. S., Dwarakish, G. S., Shanas, P., Jena, B. K., y Singh, J. (2015). Nearshore waves and longshore sediment transport along Rameshwaram Island o the east coast of India. International Journal of Naval Architecture and Ocean Engineering, 7 (6), 939{950. Grant, U. (1948). Influence of the water table on beach aggradation and degradation. publisher not identi fied. Hearn, C. J. (2008). The dynamics of coastal models. Cambridge University Press. Hoeke, R., Storlazzi, C., y Ridd, P. (2011). Hydrodynamics of a bathymetrically complex fringing coral reef embayment: Wave climate, in situ observations, and wave prediction. Journal of Geophysical Research: Oceans, 116 (C4). Hoeke, R. K., Storlazzi, C. D., y Ridd, P. V. (2013). Drivers of circulation in a fringing coral reef embayment: A wave- flow coupled numerical modeling study of Hanalei Bay, Hawaii. Continental Shelf Research, 58 , 79{95. Holland, G. J. (1980). An analytic model of the wind and pressure pro les in hurricanes. Monthly weather review, 108 (8), 1212{1218. Inch, K. (2014). Surf zone hydrodynamics: Measuring waves and currents. Geomorphological Techniques, 3 , 1{13. Inman, D., y Bagnold, R. (1963). Littoral processes. The Sea: Ideas and Observations, vol. 3 , 529{533. INVEMAR-GEO. (2015). Erosi on costera en la isla de San Andr es. informe t ecnico nal. Actividad GEO - BPIN INVEMAR. Santa Marta, 71 p. Kamphuis, J., y Readshaw, J. (1978). A model study of alongshore sediment transport rat. Coastal Engineering Proceedings, 1 (16). Kamphuis, J. W. (1991). Alongshore sediment transport rate. Journal of Waterway, Port, Coastal, and Ocean Engineering, 117 (6), 624{640. Komar, P. D. (1979). Beach-slope dependence of longshore currents. Journal of the Water- way, Port, Coastal and Ocean Division, 105 (4), 460{464. Komar, P. D., y Inman, D. L. (1970). Longshore sand transport on beaches. Journal of geophysical research, 75 (30), 5914{5927. Kumar, V. S., Shanas, P., Dora, G. U., Glejin, J., y Philip, S. (2014). Longshore sediment transport in the surf zone based on di erent formulae: a case study along the central west coast of India. Journal of coastal conservation, 21 (1), 1{13. Larson, M., Hanson, H., y Kraus, N. C. (1987). Analytical solutions of the one-line model of shoreline change. (Inf. T ec.). COASTAL ENGINEERING RESEARCH CENTER VICKSBURG MS. Lee, J., Liu, J., y Teng, M. (2006). A numerical study on nearshore sediment transport around Oahu Island in Hawaii. Journal of Coastal research, 1700{1705. List, J. (2005). Surf zone processes. Encyclopedia of coastal science, 846{850. Longuet-Higgins, M. S. (1970a). Longshore currents generated by obliquely incident sea waves: 1. Journal of geophysical research, 75 (33), 6778{6789. Longuet-Higgins, M. S. (1970b). Longshore currents generated by obliquely incident sea waves: 2. Journal of geophysical research, 75 (33), 6778{6789. Longuet-Higgins, M. S., y Stewart, R. (1964). Radiation stresses in water waves; a physical discussion, with applications. En Deep sea research and oceanographic abstracts (Vol. 11, pp. 529{562). Lowe, R. J., Falter, J. L., Monismith, S. G., y Atkinson, M. J. (2009). 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C., y Pel aez, D. (2016). Construction of synthetic ocean wave series along the Colombian Caribbean Coast: A wave climate analysis. Applied Ocean Research, 56 , 119{131. Othman, N., Wahab, A. K. A., y Jamal, M. H. (2014). E ects of seasonal variations on sandy beach groundwater table and swash zone sediment transport. Coastal Engineering Proceedings, 1 (34), 59. Otvos, E. G. (1999). Rain-induced beach processes; landforms of ground water sapping and surface runo . Journal of Coastal Research, 1040{1054. Perry, C. T., Kench, P. S., Smithers, S. G., Riegl, B., Yamano, H., y O'leary, M. J. (2011). Implications of reef ecosystem change for the stability and maintenance of coral reef islands. Global Change Biology, 17 (12), 3679{3696. Posada, B., y Guzman, W. (2007). Diagnostico de la erosi on costera en las islas de San Andr es, Providencia y Santa Catalina. Recomendaciones generales para el manejo y control de la erosi on. 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INVEMAR-Instituto de Investigaciones Marinas y Costeras. USACE. (1984). Coastal engineering manual. Printing O ce, Washington, DC, USA, vols. USACE. (2002). Coastal engineering manual. Engineer manual 1110{2-1100 . Van Rijn, L. C. (2014). A simple general expression for longshore transport of sand, gravel and shingle. Coastal Engineering, 90 , 23{39. Van Rijn, L. C., y cols. (1993). Principles of sediment transport in rivers, estuaries and coastal seas (Vol. 1006). Aqua publications Amsterdam. Vargas, G. (2004). Geolog a y aspectos geogr a cos de la Isla de San Andr es. Geolog a Colombiana, 29 , 73{89. Wang, P., Ebersole, B. A., y Smith, E. R. (2002). Longshore sand transport-initial results from large-scale sediment transport facility (Inf. T ec.). Engineer Research And Development Center Vicksburg Ms Coastal And Hydraulics Lab. Watts, G. M. (1953). A study of sand movement at South Lake Worth Inlet Florida (Inf. T ec.). Coastal Engineering Research Center Vicksburg MS. Williams, J. J., y Esteves, L. S. (2005). Predicting shoreline changes: A case study in Rio Grande do Sul, Brazil. Geophysical Research Letters, 32 (11). Zijlema, M., Stelling, G., y Smit, P. (2011). Swash: An operational public domain code for simulating wave elds and rapidly varied ows in coastal waters. Coastal Engineering, 58 (10), 992{1012. |
| dc.rights.spa.fl_str_mv |
Derechos reservados - Universidad Nacional de Colombia |
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http://purl.org/coar/access_right/c_abf2 |
| dc.rights.license.spa.fl_str_mv |
Atribución-NoComercial-SinDerivadas 4.0 Internacional |
| dc.rights.spa.spa.fl_str_mv |
Acceso abierto |
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http://creativecommons.org/licenses/by-nc-nd/4.0/ |
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info:eu-repo/semantics/openAccess |
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Atribución-NoComercial-SinDerivadas 4.0 Internacional Derechos reservados - Universidad Nacional de Colombia Acceso abierto http://creativecommons.org/licenses/by-nc-nd/4.0/ http://purl.org/coar/access_right/c_abf2 |
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openAccess |
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113 páginas |
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application/pdf |
| dc.coverage.region.spa.fl_str_mv |
San Andrés Isla, Colombia |
| dc.publisher.spa.fl_str_mv |
Universidad Nacional de Colombia |
| dc.publisher.program.spa.fl_str_mv |
Medellín - Minas - Maestría en Ingeniería - Recursos Hidráulicos |
| dc.publisher.department.spa.fl_str_mv |
Departamento de Geociencias y Medo Ambiente |
| dc.publisher.faculty.spa.fl_str_mv |
Facultad de Minas |
| dc.publisher.place.spa.fl_str_mv |
Medellín, Colombia |
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Universidad Nacional de Colombia - Sede Medellín |
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Universidad Nacional de Colombia |
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Atribución-NoComercial-SinDerivadas 4.0 InternacionalDerechos reservados - Universidad Nacional de ColombiaAcceso abiertohttp://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Bernal Franco, Gladys Rocio3bd413ee-42b1-4391-9908-ad25bbeef6d4Osorio Arias, Andrés Fernando51c751e0-bf37-4a8f-b27f-f4ba5804adc6Olarte Cáceres, Paloma Marinaa310a354-f828-4bb9-9925-e506b3d91b09OCEANICOS - Grupo de Oceanografía e Ingeniería Costera de la Universidad Nacional2020-05-29T17:06:35Z2020-05-29T17:06:35Z2019-07-02https://repositorio.unal.edu.co/handle/unal/77571Universidad Nacional de ColombiaRepositorio Institucional Universidad Nacional de Colombiahttps://repositorio.unal.edu.co/ilustraciones, gráficas, tablasLas islas oceánicas arrecifales son ambientes marinos considerados altamente vulnerables a las amenazas del cambio climático, en especial la erosión costera. Para entender esta problemática es preciso considerar que la erosión costera es un proceso dinámico que opera en diferentes escalas temporales. En consecuencia, las aproximaciones deben ser múltiples, especialmente en ambientes arrecifales, donde la compleja interacción entre geomorfología, disponibilidad de sedimentos y clima marítimo determinan las variaciones morfológicas de la zona costera. Uno de los factores determinantes de la erosión costera son los gradientes espaciales en la tasa de transporte longitudinal de sedimentos. Por lo tanto, en esta investigación se propone una metodología integrada para estimar la tasa de transporte potencial longitudinal de sedimentos (TPLS) alrededor de una isla oceánica arrecifal, considerando procesos a nivel estacional, interanual y eventos extremos. La metodología fue implementada en la isla de San Andrés, en el Caribe colombiano. A partir de información de oleaje del reanálisis ERA-Interim, el modelo numérico SWAN fue empleado para simular la propagación del oleaje desde aguas abiertas hasta la zona litoral. Los resultados del modelo fueron validados con mediciones de campo. La tasa de TPLS fue estimada haciendo uso de formulaciones empíricas, y posteriormente empleada para inferir condiciones de erosión y depositación que fueron corroboradas con imágenes satelitales. Los resultados sugieren que en la isla se presentan diferencias estacionales en los patrones de TPLS y ratifican la importancia de la barrera arrecifal para la disipación de energía del oleaje. La tasa de TPLS se incrementa durante eventos extremos. La metodología propuesta puede ser aplicable en otras islas arrecifales y provee información relevante para el manejo de la erosión costera en estos ambientes. (Texto tomado de la fuente)Ocean reef islands are marine environments considered highly vulnerable to threats of climate change, especially coastal erosion. To understand this problem, it is necessary to consider that coastal erosion is a dynamic process that operates at di_erent time scales. Consequently, the approaching must be multiple, especially in reef environments, where the complex interaction between geomorphology, sediment availability and maritime climate determines the morphological variations of the coastal zone. One of the determining factors of coastal erosion is the spatial gradients in the sediment longshore transport rate. Therefore, this research proposes an integrated methodology to estimate the potential longshore sediment transport (PLST) around an oceanic reef island, considering seasonal, interannual and extreme events processes. The methodology was implemented on San Andr_es Island, in the Colombian Caribbean. Using wave data from the ERA-Interim reanalysis, the SWAN numerical model was used to simulate the propagation of waves from open waters to the coastal zone. The results of the model were validated with _eld measurements. The PLST rate was estimated using empirical formulations and used to infer erosion and deposition conditions that were corroborated with satellite images. The results suggest that seasonal di_erences in PLST patterns occur on the island and con_rm the importance of the reef barrier for wave energy dissipation. The PLST rate increases during extreme events. The proposed methodology may be applicable in other reef islands and provides relevant information for the management of coastal erosion in these environmentsMaestríaMagíster en Ingeniería - Recursos HidráulicosÁrea Curricular de Medio Ambiente113 páginasapplication/pdfspaUniversidad Nacional de ColombiaMedellín - Minas - Maestría en Ingeniería - Recursos HidráulicosDepartamento de Geociencias y Medo AmbienteFacultad de MinasMedellín, ColombiaUniversidad Nacional de Colombia - Sede Medellín620 - Ingeniería y operaciones afines::627 - Ingeniería hidráulicaOleajeTransporte potencial longitudinal de sedimentosSan Andres IslaEventos extremosErosion costeraWavesPotential longshore sediment transportSan Andres IslandExtreme eventsCostal erosionClimatología del transporte potencial de sedimentos costeros inducido por oleaje en la Isla San AndrésClimatology of the potential coastal sediment transport induced by waves in San Andres islandTrabajo de grado - Maestríainfo:eu-repo/semantics/masterThesisinfo:eu-repo/semantics/acceptedVersionTexthttp://purl.org/redcol/resource_type/TMSan Andrés Isla, ColombiaAagaard, T., y Kroon, A. 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