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Modelación de la estructura Dinámica de las aguas de la Cuenca del Pacífico Colombiano

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Modelación de la estructura ...
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Author
Villegas Bolaños, Nancy Liliana
Málikov, Igor
Corporate Author
Dirección General Marítima
Date
2006

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Abstract
La circulación de las aguas de la cuenca del Pacífico colombiano y los componentes de velocidad U y V de las corrientes son resultados obtenidos de la modelación de la evolución de características termohalinas y dinámicas de la región. En el presente estudio se observó que la circulación de las capas superficiales se encuentra bajo la influencia de la migración de la Zona de Convergencia Intertropical. La circulación depende también de corrientes superficiales y subsuperficiales (corriente del Perú, contracorriente Ecuatorial del Norte, corriente de Colombia y corriente de Panamá), las cuales cambian su intensidad durante el año por influencia de los vientos alisios. Bajo estas capas, la distribución vertical de las características dinámicas prácticamente es constante. Las cordilleras submarinas dificultan el intercambio de las aguas con otras regiones, formando una circulación de carácter local en las capas profundas. En el sistema de circulación se observa una estructura vertical de tres capas: de 0 a 80m, de 80 a 200m y de 200m hasta el fondo.
Water circulation and U - V sea velocity components of Colombian Pacific Ocean (CPO) are the results obtained from evolution modeling of thermohaline and dynamic characteristics of CPO. It was observed that superficial layer circulation is under the influence of Inter - Tropical Convergence Zone (ITCZ) migration. This circulation also depends on the influence of superficial and sub-superficial currents (Peru Current, North Equatorial Countercurrent, Colombian Current, and Panama Current), which change their intensity during the year depending on trade winds influence. Vertical distribution of dynamic characteristics under these layers is practically constant. Submarine mountain ranges make it difficult to interchange waters of CPO with those of other regions, forming a local circulation in deep layers. In circulation system, a three layer vertical structure is observed: 0 - 80m, 80 - 200m and 200m - bottom.
Journal
Boletín Científico CCCP
Issue/Article Nr
13
Page Range
Pp.97-114
DOI
https://doi.org/10.26640/01213423.13.97_114
Resource/Dataset Location
http://cecoldodigital.dimar.mil.co/421/
URI
http://hdl.handle.net/1834/17321
ae974a485f413a2113503eed53cd6c53
https://doi.org/10.26640/01213423.13.97_114
Scopus Count
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DIMAR Publications

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