Surface circulation patterns above the coastal shelf between El Uno bay and Las Vacas spit, Gulf of Urabá, Colombian Caribbean
DOI:
https://doi.org/10.25268/bimc.invemar.2021.50.2.993Keywords:
Circulación superficial, viento, marea, derivados, Corrientes costerasAbstract
Good knowledge of the coastal circulation patterns is essential for a proper management of the coastline, especially in areas with a high anthropic pressure. In order to determine the main characteristics of the coastal currents in the Gulf of Urabá, the seasonal
patterns of surface circulation were measured and analyzed during times of high and low rainfall along 6 km of coastline, between the Punta de Las Vacas and Punta Yarumal coastal spit systems, in the municipality of Turbo, Antioquia. These measurements were made with surface drifters, which were launched at different tide stages and tracked for time periods based on the semi-diurnal cycle. The in-situ measurements were analyzed alongside tide and wind data from a climatic station located near the gulf. The circulation patterns behaved differently depending on the season of the year. In the rainy season, with southerly winds, the drifters moved mainly towards the north while during the dry season, with northerly winds, all the drifters moved to the south. Although the circulation patterns showed a strong relationship with the tidal cycle and wind conditions, the Turbo and El Uno Bays modified some of the drifter’s paths.
References
Alcántara, J., A. Caicedo., J. Hernández., A. Jaramillo-Vélez and R. Manzolli. 2019. Sediment bypassing from the new human-induced lobe to the ancient lobe of the Turbo delta (Gulf of Urabá, Southern Caribbean Sea). J. Coast. Res., 35(1): 196-209.
Arroyo, L.M. 2019. Caracterización del ciclo de brisas diurnas en el Golfo de Urabá a partir de resultados del modelo atmosférico WRF. Universidad de Antioquia, Ingeniería Ambiental, Turbo, Colombia. 56 p.
Brakenridge, G. R. Kettner, A.J. Paris, S. Cohen, S. and S. Nghiem. 2021. River and reservoir watch Version 4.0. DFO Flood Observatory, University of Colorado, USA. http://floodobservatory.colorado.edu/SiteDisplays/40.htm. Fecha de consulta: 03/02/2021.
CIOH. 2017. Pronóstico del nivel del mar para el golfo de Urabá. Cartagena, Colombia. https://www.cioh.org.co/meteorologia/mareas.php. Fecha de consulta: 10/10/2017.
Correa, I. D. y G. Vernette. 2004. Introducción al problema de la erosión litoral en Urabá (sector Arboletes-Turbo) Costa Caribe Colombiana. Bol. Invest. Mar. Cost., 33: 7-28.
Correa-Ramírez, M., A. Rodríguez-Santana., C. Ricaurte-Villota and J. Páramo. 2020. The Southern Caribbean upwelling system off Colombia: Water masses and mixing processes. Deep Sea Res. Part I: Oceanogr. Res. Pap., 155: 103145.
Escobar, A. 2011. Relevancia de procesos costeros en la hidrodinámica del golfo de Urabá (Caribe colombiano). Bol. Invest. Mar. Cost., 40(2): 327-346.
Escobar, C., L. Velásquez and Posada, F. 2015. Marine Currents in the Gulf of Urabá, Colombian Caribbean Sea. J. of Coast. Res. 31(6), 1363–1374.
Grifoll, M., A. Aretxabaleta, J. Pelegri and M. Espino. 2016. Temporal evolution of the momentum balance terms and frictional adjustment observed over the inner shelf during a storm. Oc. Sci., 137-151.
Godin, G. 1993. On tidal resonance. Cont. Shelf Res., 13: 89-107.
Higuita. M. y R. Quintana. 2020. Modulación de las corrientes oceánicas en el golfo de Urabá a partir de la onda de marea. Tesis de grado, Oceanografía e Ingeniería Oceanográfica. Universidad de Antioquia. Turbo. 55 p.
IDEAM. 2019. Pronóstico de pleamares y bajamares en la costa Caribe colombiana 2020. 171 p.
Invemar. 2003. Diagnóstico, zonificación y definición de la estructura administrativa y manejo de la unidad costera del Darién, Caribe colombiano. Fase I. Caracterización y diagnóstico. Informe técnico. 698 p.
Kjerfve, B. 1981. Tides of the Caribbean Sea. J. Geophys. Res., 96, 4243-4247.
Lonin, S. y J.G. Vásquez. 2005. Hidrodinámica y distribución de coliformes en el Golfo de Urabá. Bol. Cient. CIOH, 23: 76-89.
Lozano-Duque, Y., J. Medellín-Mora y G.R. Navas. 2010. Contexto climatológico y oceanográfico del mar Caribe colombiano: 54-84. En Biodiversidad del margen continental del Caribe colombiano, Invemar Serie Publ. Espec., 20.
Lucero, M. y M. Mindiola. 2007. Distribución de las corrientes superficiales y subsuperficiales en la Caleta Aeolian-isla Baltra, Ecuador. Acta Oceanogr. Pac., 14: 14-19.
MacMahan, J., J. Brown and E. Thornton.2009. Low-cost handheld Global Positioning System for measuring surf-zone currents. J. Coast. Res., 25(3): 744-754.
Montoya, L. y M. Toro. 2006. Calibración de un modelo hidrodinámico, para el estudio de los patrones de circulación del golfo de Urabá, Colombia. Av. Rec. Hidr., 13: 37-54.
Nienhuis, J. 2019. Local wave and tide data. Earth Engine App. https://jhnienhuis.users.earthengine.app/view/changing-shores. Fecha de consulta: 19/11/2019.
Proudman, J. 1953. Dynamical oceanography. Methuen, London, 409 p.
Prüssmann-Uribe, J. e I.D. Correa-Arango. 2012. Base de datos espacial geomorfológica de la franja litoral de los departamentos de Antioquia y Chocó. Geol. Col., 37(1): 47-48.
Ricaurte-Villota, C. y M.L. Bastidas Salamanca. 2017. Regionalización oceanográfica: una visión dinámica del Caribe.Ser. Publ. Espec., Invemar 14, 180 p.
Shafiei, B. and G. Abbas. 2011. Design of small GPS drifters for current measurements in the coastal zone. Oc. Coast. Manag., 54(2): 158-163.
Toro, V., W. Mosquera, N. Barrientos e Y. Bedoya. 2019. Circulación oceánica del golfo de Urabá usando campos de vientos de alta resolución temporal. Bol. Cient. CIOH. 38 (2): 26-35.
Wu, J. 1983. Sea-surface drift currents induced by winds and waves. J.Phys. Oceanogr., 13: 1441-1451.
Downloads
Published
How to Cite
Issue
Section
License
Copyright (c) 2021 Bulletin of Marine and Coastal Research
This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License.