Variación anual del contenido de calor de la capa activa del Pacífico colombiano.
The present work made for the first time with data of sea temperature specifically of the Colombian Pacific Ocean, presents the space and temporary distribution of the heat content of the active layer in this region. The used methodology was the analysis of the annual behavior of the temperatura in representative stations of the investigation area. It was obtained that the annual oscillations of temperature in the study area show two maximums and two minimums: december and june of heating, and march and september of cooling which shows the influence of the displacement of the Intertropical convergence zona, ITCZ. As far as the thickness of the active layer in the Colombian Pacific was that this one varies between the 150 -200 meters in the zonas near the coast and between 200 -300 meters in oceanic zones. Fluctuation depends on the displacement of the atmospheric processes in each observad zona
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Format: | Journal Contribution biblioteca |
Language: | Spanish / Castilian |
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2003
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Subjects: | Capa Activa, Calor, Convergencia, Oscilación, Temperatura, ZCIT, ASFA_2015::P::Physical oceanography, |
Online Access: | http://hdl.handle.net/1834/17401 |
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dig-aquadocs-1834-174012021-05-19T06:32:04Z Variación anual del contenido de calor de la capa activa del Pacífico colombiano. Villegas Bolaños, Nancy Liliana Dirección General Marítima Capa Activa Calor Convergencia Oscilación Temperatura ZCIT ASFA_2015::P::Physical oceanography The present work made for the first time with data of sea temperature specifically of the Colombian Pacific Ocean, presents the space and temporary distribution of the heat content of the active layer in this region. The used methodology was the analysis of the annual behavior of the temperatura in representative stations of the investigation area. It was obtained that the annual oscillations of temperature in the study area show two maximums and two minimums: december and june of heating, and march and september of cooling which shows the influence of the displacement of the Intertropical convergence zona, ITCZ. As far as the thickness of the active layer in the Colombian Pacific was that this one varies between the 150 -200 meters in the zonas near the coast and between 200 -300 meters in oceanic zones. Fluctuation depends on the displacement of the atmospheric processes in each observad zona El presente trabajo se realizó utilizando por primera vez datos de temperatura del mar específicamente de la Cuenca del Pacifico Colombiano, CPC, dando a conocer la distribución espacial y temporal del contenido de metodología utilizada fue el análisis del comportamiento anual de temperatura en estaciones representativas del área de investigación. Se obtuvo que las oscilaciones anuales de temperatura en el área de estudio presentan dos máximos y dos mínimos: diciembre y junio de calentamiento y marzo y septiembre de enfriamiento, lo cual muestra la influencia del desplazamiento de la Zona de Convergencia intertropical, ZCIT. En cuanto al grosor de la capa activa en el Pacífico Colombiano se encontró que varía entre los 150 y 200 m, en las zonas cercanas a la costa, y entre 200 y 300 m en la zonas más oceánicas, Su fluctuación depende del desplazamiento de los procesos atmosféricos en cada zona observada. Published 2020-08-10T20:57:12Z 2020-08-10T20:57:12Z 2003 Journal Contribution Not Known 0121-3423 ttps://doi.org/10.26640/01213423.10.31_42 http://hdl.handle.net/1834/17401 es http://cecoldodigital.dimar.mil.co/395/ pp.31-42 Pacífico Colombiano |
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Capa Activa Calor Convergencia Oscilación Temperatura ZCIT ASFA_2015::P::Physical oceanography Capa Activa Calor Convergencia Oscilación Temperatura ZCIT ASFA_2015::P::Physical oceanography |
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Capa Activa Calor Convergencia Oscilación Temperatura ZCIT ASFA_2015::P::Physical oceanography Capa Activa Calor Convergencia Oscilación Temperatura ZCIT ASFA_2015::P::Physical oceanography Villegas Bolaños, Nancy Liliana Variación anual del contenido de calor de la capa activa del Pacífico colombiano. |
description |
The present work made for the first time with data of sea temperature specifically of the Colombian Pacific Ocean, presents the space and temporary distribution of the heat content of the active layer in this region. The used methodology was the analysis of the annual behavior of the temperatura in representative stations of the investigation area. It was obtained that the annual oscillations of temperature in the study area show two maximums and two minimums: december and june of heating, and march and september of cooling which shows the influence of the displacement of the Intertropical convergence zona, ITCZ. As far as the thickness of the active layer in the Colombian Pacific was that this one varies between the 150 -200 meters in the zonas near the coast and between 200 -300 meters in oceanic zones. Fluctuation depends on the displacement of the atmospheric processes in each observad zona |
author2 |
Dirección General Marítima |
author_facet |
Dirección General Marítima Villegas Bolaños, Nancy Liliana |
format |
Journal Contribution |
topic_facet |
Capa Activa Calor Convergencia Oscilación Temperatura ZCIT ASFA_2015::P::Physical oceanography |
author |
Villegas Bolaños, Nancy Liliana |
author_sort |
Villegas Bolaños, Nancy Liliana |
title |
Variación anual del contenido de calor de la capa activa del Pacífico colombiano. |
title_short |
Variación anual del contenido de calor de la capa activa del Pacífico colombiano. |
title_full |
Variación anual del contenido de calor de la capa activa del Pacífico colombiano. |
title_fullStr |
Variación anual del contenido de calor de la capa activa del Pacífico colombiano. |
title_full_unstemmed |
Variación anual del contenido de calor de la capa activa del Pacífico colombiano. |
title_sort |
variación anual del contenido de calor de la capa activa del pacífico colombiano. |
publishDate |
2003 |
url |
http://hdl.handle.net/1834/17401 |
work_keys_str_mv |
AT villegasbolanosnancyliliana variacionanualdelcontenidodecalordelacapaactivadelpacificocolombiano |
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1756075677416685568 |