Numerical model of the circulation induced by the wind at Bahia de Los Angeles, B.C., Mexico

Numerical model of the circulation induced by the wind at Bahia de Los Angeles, B.C., Mexico

The circulation induced by the M2 component of the tide and wind at Bahía de los Angeles was predicted. The tide amplitude and the phase are practically the same at the bay, the tide currents values are 3 cm/s and the tide residuals 0.5 cm/s. Otherwise, the induced currents by the wind reach until 2...

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Autores principales: Amador-Buenrostro, A, Serrano-Guzmán, SJ, Argote-Espinoza, MA
Formato: Online
Lenguaje:eng
Publicado: Iniversidad Autónoma de Baja California 2021
Acceso en línea:https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/822
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spelling oai:cienciasmarinas.com.mx:article-8222013-08-19T03:29:29Z Numerical model of the circulation induced by the wind at Bahia de Los Angeles, B.C., Mexico Modelado numérico de la circulación inducida por el viento en Bahía de Los Ángeles, B.C., México Amador-Buenrostro, A Serrano-Guzmán, SJ Argote-Espinoza, MA The circulation induced by the M2 component of the tide and wind at Bahía de los Angeles was predicted. The tide amplitude and the phase are practically the same at the bay, the tide currents values are 3 cm/s and the tide residuals 0.5 cm/s. Otherwise, the induced currents by the wind reach until 25 cm/s at the intensification areas. The coast configuration and the bathymetry dominate the main characteristics of the circulation. There is a strong interchange with the exterior to any dominant direction of the wind, and a persistent gyre at the inlet of La Gringa and at the middle of the bay. The most intenses flux zones are the southern channel and the coastal zone to the South of La Gringa inlet. Se predice numéricamente la circulación inducida por la componente M2 de la marea y el viento en Bahía de los Ángeles. La amplitud y la fase de la marea son prácticamente iguales en toda la bahía, las corrientes de marea son del orden de 3 cm/s y las residuales de la marea de 0.5 cm/s. En cambio las corrientes inducidas por el viento alcanzan hasta 25 cm/s en las áreas de intensificación. La configuración de la costa y la batimetría dominan las principales características de la circulación. Para cualquier dirección del viento dominante, se presenta un fuerte intercambio con el exterior, y un giro persistente en la ensenada La Gringa y con la parte central de la bahía. Las zonas de flujo más intenso son el canal sur y la zona costera al sur de la ensenada La Gringa. Iniversidad Autónoma de Baja California 2021-02-16 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed Article Artículo Arbitrado application/pdf https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/822 10.7773/cm.v17i3.822 Ciencias Marinas; Vol. 17 No. 3 (1991); 39-57 Ciencias Marinas; Vol. 17 Núm. 3 (1991); 39-57 2395-9053 0185-3880 eng https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/822/420420526 Copyright (c) 2021 Ciencias Marinas
institution Ciencias Marinas
collection OJS
language eng
format Online
author Amador-Buenrostro, A
Serrano-Guzmán, SJ
Argote-Espinoza, MA
spellingShingle Amador-Buenrostro, A
Serrano-Guzmán, SJ
Argote-Espinoza, MA
Numerical model of the circulation induced by the wind at Bahia de Los Angeles, B.C., Mexico
author_facet Amador-Buenrostro, A
Serrano-Guzmán, SJ
Argote-Espinoza, MA
author_sort Amador-Buenrostro, A
title Numerical model of the circulation induced by the wind at Bahia de Los Angeles, B.C., Mexico
title_short Numerical model of the circulation induced by the wind at Bahia de Los Angeles, B.C., Mexico
title_full Numerical model of the circulation induced by the wind at Bahia de Los Angeles, B.C., Mexico
title_fullStr Numerical model of the circulation induced by the wind at Bahia de Los Angeles, B.C., Mexico
title_full_unstemmed Numerical model of the circulation induced by the wind at Bahia de Los Angeles, B.C., Mexico
title_sort numerical model of the circulation induced by the wind at bahia de los angeles, b.c., mexico
description The circulation induced by the M2 component of the tide and wind at Bahía de los Angeles was predicted. The tide amplitude and the phase are practically the same at the bay, the tide currents values are 3 cm/s and the tide residuals 0.5 cm/s. Otherwise, the induced currents by the wind reach until 25 cm/s at the intensification areas. The coast configuration and the bathymetry dominate the main characteristics of the circulation. There is a strong interchange with the exterior to any dominant direction of the wind, and a persistent gyre at the inlet of La Gringa and at the middle of the bay. The most intenses flux zones are the southern channel and the coastal zone to the South of La Gringa inlet.
publisher Iniversidad Autónoma de Baja California
publishDate 2021
url https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/822
_version_ 1715724015820079104

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