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Discussion papers
https://doi.org/10.5194/os-2019-17
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-2019-17
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Submitted as: research article 27 Mar 2019

Submitted as: research article | 27 Mar 2019

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This discussion paper is a preprint. It has been under review for the journal Ocean Science (OS). The revised manuscript was not accepted.

Water masses and mixing processes in the Southern Caribbean upwelling system off Colombia

Marco Correa-Ramirez1, Ángel Rodriguez-Santana2, Constanza Ricaurte-Villota1, and Jorge Paramo3 Marco Correa-Ramirez et al.
  • 1Institute of Marine and Coastal Research (INVEMAR), Santa Marta, Colombia
  • 2Departamento F’isica, Universidad de las Palmas de Gran Canaria, España
  • 3Grupo de Investigación Ciencia y Tecnología Pesquera Tropical (CITEPT), Universidad del Magdalena, Santa Marta, Colombia

Abstract. The upwelling system off the southern Caribbean coast is probably the main nutrients source that support the biological productivity in this oligotrophic sea. The Subtropical Water Mass (SUW) that forms the subsurface salinity maximum in the Caribbean is the main source of upwelled waters in this system. Salinity and temperature vs. depth profiles from 4 oceanographic cruises in the western sector of the Caribbean upwelling system, showed that the salinity of upwelled SUW waters is ~ 0.2 g kg−1 lower than the SUW salinity in the central Caribbean and have a slight seasonal variation that agree with with the rainy/dry seasons in the region. Besides, the depth of these SUW waters in the continental slope (~ 100 m) is ~ 50 m shallower than the SUW depth in the rest of the Caribbean sea. The origin of these modified SUW waters was analyzed using the Mercator numerical model, which reproduces the main vertical characteristics of the subsurface salinity maximum. Modeled data showed that SUW waters upwelled off La Guajira peninsula come from the western Caribbean and arrive to the system transported by an intense Caribbean Coastal Undercurrent (CaCU, mean speed ~ 0.4 m s−1). The lower salinity observed in the upwelled SUW waters may be the result of intense vertical mixing processes with diluted surface waters in the Panama-Colombia gyro that could occur when the CaCU flows below this region before reaching the upwelling zones. The mixing processes in the SUW by double diffusion and mechanical turbulence driven by vertical shear of horizontal currents, were analyzed using the Turner angle and the Thorpe scale, respectively. Double diffusion by salt fingers was found between the SUW and the Central North Atlantic Waters (NACW) with diffusivity values ~ 10−5 m2 s−1. But the mechanical diffusivity was two orders of magnitude higher (10−3 m2 s−1.) than the double diffusivities in the entire water column, generating salt fluxes from the SUW towards surface and towards depth over 2 g kg−1 m d−1. Beyond modifying the salt content in coastal SUW waters, these mixing processes may also alter the nutrient content of upwelling waters, with effects still unknown to the upwelling ecosystem.

Marco Correa-Ramirez et al.
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Marco Correa-Ramirez et al.
Marco Correa-Ramirez et al.
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Short summary
Waters form the Subtropical Water mass (SUW) generated in the central Atlantic enter the Caribbean through Antilles and flow westward at the depth of the subsurface salinity maximum. Our evidence shows that part of these waters are returned to the east by a Coastal Undercurrent where their salt content is modified by intense processes of vertical mixing with diluted surface waters. Eventually these modified SUW waters reaches the surface in the coastal upwelling areas off Colombia and Venezuela.
Waters form the Subtropical Water mass (SUW) generated in the central Atlantic enter the...
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