Study of the dynamic behaviour of the Sancti Petri Channel, southwest coast of Spain
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Redalyc · Ciencias Marinas
The dynamic behaviour of the Sancti Petri tidal channel (southwest coast of Spain), which is open at both ends and connected to water bodies with different dynamic characteristics (Atlantic Ocean and Cádiz Bay), is studied herein. This singular estuary is characterized by double inflow-outflow extre...
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| Publicado en: | Ciencias Marinas |
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| Formato: | Artículo científico |
| Lenguaje: | en |
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Universidad Autónoma de Baja California
2005
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| _version_ | 1878325297939480576 |
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| author | J. Vidal |
| author_facet | J. Vidal |
| collection | Ciencias Marinas |
| container_title | Ciencias Marinas |
| contents | Study of the dynamic behaviour of the Sancti Petri Channel, southwest coast of Spain J. Vidal B. Tejedor Ciencias de la Tierra Sancti Petri tidal channel double inflow numerical model outflow extremes The dynamic behaviour of the Sancti Petri tidal channel (southwest coast of Spain), which is open at both ends and connectedto water bodies with different dynamic characteristics (Atlantic Ocean and Cádiz Bay), is studied herein. This singular estuary ischaracterized by double inflow-outflow extremes, the tide penetrating almost simultaneously through both ends with a smalldifference of amplitude. For this study, sea level recordings were obtained from different points throughout the channel and thecorresponding harmonic constituents were determined. The results show that the phases of the semidiurnal tides increase from themouths to a zone located in the vicinity of the channels halfway point, while their amplitudes increase from the Atlantic Ocean toCádiz Bay along the channel. A one-dimensional numerical model with geometry that is representative of the channel was used toreproduce the features observed for the semidiurnal and diurnal tidal constituents. The data supplied by the model were verifiedwith values obtained at strategically chosen sites of the inner domain. The model developed may be used for operationalpredictions of tides in the study area, especially for the ports of Gallineras and Sancti Petri. 2005 artículo científico 0185-3880 https://www.redalyc.org/articulo.oa?id=48031402 en http://www.redalyc.org/revista.oa?id=480 Ciencias Marinas application/pdf Universidad Autónoma de Baja California Ciencias Marinas (México) Num.4 Vol.31 |
| ctrlnum | oai:cienciasmarinas.com.mx:article/25 10.7773/cm.v31i4.25 |
| description | The dynamic behaviour of the Sancti Petri tidal channel (southwest coast of Spain), which is open at both ends and connected to water bodies with different dynamic characteristics (Atlantic Ocean and Cádiz Bay), is studied herein. This singular estuary is characterized by double inflow-outflow extremes, the tide penetrating almost simultaneously through both ends with a small difference of amplitude. For this study, sea level recordings were obtained from different points throughout the channel and the corresponding harmonic constituents were determined. The results show that the phases of the semidiurnal tides increase from the mouths to a zone located in the vicinity of the channel´ s halfway point, while their amplitudes increase from the Atlantic Ocean to Cádiz Bay along the channel. A one-dimensional numerical model with geometry that is representative of the channel was used to reproduce the features observed for the semidiurnal and diurnal tidal constituents. The data supplied by the model were verified with values obtained at strategically chosen sites of the inner domain. The model developed may be used for operational predictions of tides in the study area, especially for the ports of Gallineras and Sancti Petri.
El canal de marea de Sancti Petri se sitúa en el suroeste de las costas españolas y se encuentra conectado a dos cuerpos de agua con características dinámicas propias (Océano Atlántico y Bahía de Cádiz) a través de sus dos extremos. Es éste un singular estuario, por cuanto la propagación de la marea se produce, casi simultáneamente, desde sus dos desembocaduras, con una pequeña diferencia de amplitud. A partir de los datos experimentales se observa que las amplitudes de las constituyentes semidiurnas aumentan a lo largo del canal desde el extremo más al sur (Océano Atlántico) hasta el extremo que conecta con la Bahía de Cádiz, mientras que las fases de estas constituyentes presentan un máximo en una zona próxima al punto intermedio del canal. A partir de un modelo numérico unidimensional, se estudió la propagación de las principales constituyentes semidiurnas y diurnas de la marea. Los resultados obtenidos mediante los modelos han sido validados con datos experimentales tomados en puntos estratégicos dentro del canal. El modelo desarrollado puede ser utilizado para obtener predicciones de mareas en la zona de estudio, especialmente en los puertos de Gallineras y Sancti Petri. |
| format | Artículo científico |
| id | redalyc_48031402 |
| institution | Redalyc Ciencias Marinas |
| language | en |
| publishDate | 2005 |
| publisher | Universidad Autónoma de Baja California |
| spelling | Study of the dynamic behaviour of the Sancti Petri Channel, southwest coast of Spain Estudio del comportamiento dinámico del Caño de Sancti Petri Vidal, J Tejedor, B tidal channel numerical model double inflow-outflow extremes Sancti Petri canal de mareas modelo numérico doble entrada de flujo y reflujo Sancti Petri The dynamic behaviour of the Sancti Petri tidal channel (southwest coast of Spain), which is open at both ends and connected to water bodies with different dynamic characteristics (Atlantic Ocean and Cádiz Bay), is studied herein. This singular estuary is characterized by double inflow-outflow extremes, the tide penetrating almost simultaneously through both ends with a small difference of amplitude. For this study, sea level recordings were obtained from different points throughout the channel and the corresponding harmonic constituents were determined. The results show that the phases of the semidiurnal tides increase from the mouths to a zone located in the vicinity of the channel´ s halfway point, while their amplitudes increase from the Atlantic Ocean to Cádiz Bay along the channel. A one-dimensional numerical model with geometry that is representative of the channel was used to reproduce the features observed for the semidiurnal and diurnal tidal constituents. The data supplied by the model were verified with values obtained at strategically chosen sites of the inner domain. The model developed may be used for operational predictions of tides in the study area, especially for the ports of Gallineras and Sancti Petri. El canal de marea de Sancti Petri se sitúa en el suroeste de las costas españolas y se encuentra conectado a dos cuerpos de agua con características dinámicas propias (Océano Atlántico y Bahía de Cádiz) a través de sus dos extremos. Es éste un singular estuario, por cuanto la propagación de la marea se produce, casi simultáneamente, desde sus dos desembocaduras, con una pequeña diferencia de amplitud. A partir de los datos experimentales se observa que las amplitudes de las constituyentes semidiurnas aumentan a lo largo del canal desde el extremo más al sur (Océano Atlántico) hasta el extremo que conecta con la Bahía de Cádiz, mientras que las fases de estas constituyentes presentan un máximo en una zona próxima al punto intermedio del canal. A partir de un modelo numérico unidimensional, se estudió la propagación de las principales constituyentes semidiurnas y diurnas de la marea. Los resultados obtenidos mediante los modelos han sido validados con datos experimentales tomados en puntos estratégicos dentro del canal. El modelo desarrollado puede ser utilizado para obtener predicciones de mareas en la zona de estudio, especialmente en los puertos de Gallineras y Sancti Petri. Universidad Autónoma de Baja California, Instituto de Investigaciones Oceanológicas 2005-03-06 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed Article Artículo Arbitrado application/pdf https://cienciasmarinas.com.mx/index.php/cmarinas/article/view/25 10.7773/cm.v31i4.25 Ciencias Marinas; Vol. 31 No. 4 (2005); 617-626 Ciencias Marinas; Vol. 31 Núm. 4 (2005); 617-626 2395-9053 0185-3880 eng https://cienciasmarinas.com.mx/index.php/cmarinas/article/view/25/10 ['Redalyc'] redalyc_48031402 Study of the dynamic behaviour of the Sancti Petri Channel, southwest coast of Spain ['Study of the dynamic behaviour of the Sancti Petri Channel, southwest coast of Spain', 'J. Vidal', 'Ciencias de la Tierra', 'Sancti Petri', 'tidal channel', 'double inflow', 'numerical model', 'outflow extremes', 'Study of the dynamic behaviour of the Sancti Petri Channel, southwest coast of Spain J. Vidal B. Tejedor Ciencias de la Tierra Sancti Petri tidal channel double inflow numerical model outflow extremes The dynamic behaviour of the Sancti Petri tidal channel (southwest coast of Spain), which is open at both ends and connectedto water bodies with different dynamic characteristics (Atlantic Ocean and Cádiz Bay), is studied herein. This singular estuary ischaracterized by double inflow-outflow extremes, the tide penetrating almost simultaneously through both ends with a smalldifference of amplitude. For this study, sea level recordings were obtained from different points throughout the channel and thecorresponding harmonic constituents were determined. The results show that the phases of the semidiurnal tides increase from themouths to a zone located in the vicinity of the channel\x92s halfway point, while their amplitudes increase from the Atlantic Ocean toCádiz Bay along the channel. A one-dimensional numerical model with geometry that is representative of the channel was used toreproduce the features observed for the semidiurnal and diurnal tidal constituents. The data supplied by the model were verifiedwith values obtained at strategically chosen sites of the inner domain. The model developed may be used for operationalpredictions of tides in the study area, especially for the ports of Gallineras and Sancti Petri. 2005 artículo científico 0185-3880 https://www.redalyc.org/articulo.oa?id=48031402 en http://www.redalyc.org/revista.oa?id=480 Ciencias Marinas application/pdf Universidad Autónoma de Baja California Ciencias Marinas (México) Num.4 Vol.31'] ['J. Vidal'] ['J. Vidal'] ['Artículo científico'] ['2005'] ['Universidad Autónoma de Baja California'] ['en'] ['Ciencias de la Tierra', 'Sancti Petri', 'tidal channel', 'double inflow', 'numerical model', 'outflow extremes'] ['https://www.redalyc.org/articulo.oa?id=48031402'] ['Study of the dynamic behaviour of the Sancti Petri Channel, southwest coast of Spain J. Vidal B. Tejedor Ciencias de la Tierra Sancti Petri tidal channel double inflow numerical model outflow extremes The dynamic behaviour of the Sancti Petri tidal channel (southwest coast of Spain), which is open at both ends and connectedto water bodies with different dynamic characteristics (Atlantic Ocean and Cádiz Bay), is studied herein. This singular estuary ischaracterized by double inflow-outflow extremes, the tide penetrating almost simultaneously through both ends with a smalldifference of amplitude. For this study, sea level recordings were obtained from different points throughout the channel and thecorresponding harmonic constituents were determined. The results show that the phases of the semidiurnal tides increase from themouths to a zone located in the vicinity of the channel\x92s halfway point, while their amplitudes increase from the Atlantic Ocean toCádiz Bay along the channel. A one-dimensional numerical model with geometry that is representative of the channel was used toreproduce the features observed for the semidiurnal and diurnal tidal constituents. The data supplied by the model were verifiedwith values obtained at strategically chosen sites of the inner domain. The model developed may be used for operationalpredictions of tides in the study area, especially for the ports of Gallineras and Sancti Petri. 2005 artículo científico 0185-3880 https://www.redalyc.org/articulo.oa?id=48031402 en http://www.redalyc.org/revista.oa?id=480 Ciencias Marinas application/pdf Universidad Autónoma de Baja California Ciencias Marinas (México) Num.4 Vol.31'] |
| spellingShingle | Study of the dynamic behaviour of the Sancti Petri Channel, southwest coast of Spain J. Vidal Ciencias de la Tierra Sancti Petri tidal channel double inflow numerical model outflow extremes Study of the dynamic behaviour of the Sancti Petri Channel, southwest coast of Spain J. Vidal B. Tejedor Ciencias de la Tierra Sancti Petri tidal channel double inflow numerical model outflow extremes The dynamic behaviour of the Sancti Petri tidal channel (southwest coast of Spain), which is open at both ends and connectedto water bodies with different dynamic characteristics (Atlantic Ocean and Cádiz Bay), is studied herein. This singular estuary ischaracterized by double inflow-outflow extremes, the tide penetrating almost simultaneously through both ends with a smalldifference of amplitude. For this study, sea level recordings were obtained from different points throughout the channel and thecorresponding harmonic constituents were determined. The results show that the phases of the semidiurnal tides increase from themouths to a zone located in the vicinity of the channels halfway point, while their amplitudes increase from the Atlantic Ocean toCádiz Bay along the channel. A one-dimensional numerical model with geometry that is representative of the channel was used toreproduce the features observed for the semidiurnal and diurnal tidal constituents. The data supplied by the model were verifiedwith values obtained at strategically chosen sites of the inner domain. The model developed may be used for operationalpredictions of tides in the study area, especially for the ports of Gallineras and Sancti Petri. 2005 artículo científico 0185-3880 https://www.redalyc.org/articulo.oa?id=48031402 en http://www.redalyc.org/revista.oa?id=480 Ciencias Marinas application/pdf Universidad Autónoma de Baja California Ciencias Marinas (México) Num.4 Vol.31 |
| title | Study of the dynamic behaviour of the Sancti Petri Channel, southwest coast of Spain |
| title_alt | Estudio del comportamiento dinámico del Caño de Sancti Petri |
| topic | Ciencias de la Tierra Sancti Petri tidal channel double inflow numerical model outflow extremes |
| topic_facet | tidal channel numerical model double inflow-outflow extremes Sancti Petri canal de mareas modelo numérico doble entrada de flujo y reflujo |
| url | https://www.redalyc.org/articulo.oa?id=48031402 https://cienciasmarinas.com.mx/index.php/cmarinas/article/view/25 |