dor_id: 4132167

506.#.#.a: Público

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510.0.#.a: Consejo Nacional de Ciencia y Tecnología (CONACyT); Scientific Electronic Library Online (SciELO); SCOPUS, Dialnet, Directory of Open Access Journals (DOAJ); Geobase

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650.#.4.x: Físico Matemáticas y Ciencias de la Tierra

336.#.#.b: article

336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

351.#.#.6: http://revistagi.geofisica.unam.mx/index.php/RGI

351.#.#.b: Geofísica Internacional

351.#.#.a: Artículos

harvesting_group: RevistasUNAM

270.1.#.p: Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

590.#.#.c: Open Journal Systems (OJS)

270.#.#.d: MX

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883.#.#.u: https://revistas.unam.mx/catalogo/

883.#.#.a: Revistas UNAM

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883.#.#.q: Dirección General de Publicaciones y Fomento Editorial

850.#.#.a: Universidad Nacional Autónoma de México

856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/439/453

100.1.#.a: Gómez-valdés, José; J. Vázquez, Heriberto

524.#.#.a: Gómez-valdés, José, et al. (2012). Vertical structure of tidal flows at the entrance to Guaymas Bay, Mexico. Geofísica Internacional; Vol. 51 Núm. 3: Julio 1, 2012; 271-279. Recuperado de https://repositorio.unam.mx/contenidos/4132167

245.1.0.a: Vertical structure of tidal flows at the entrance to Guaymas Bay, Mexico

502.#.#.c: Universidad Nacional Autónoma de México

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2012

264.#.1.c: 2012-07-01

653.#.#.a: mareas; corrientes; laguna semiárida; Golfo de California; Bahía de Guaymas; tides; tidal current; semiarid lagoon; Gulf of California; Guaymas Bay

506.1.#.a: La titularidad de los derechos patrimoniales de esta obra pertenece a las instituciones editoras. Su uso se rige por una licencia Creative Commons BY-NC-SA 4.0 Internacional, https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico revistagi@igeofisica.unam.mx

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/439

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/439

041.#.7.h: spa

520.3.#.a: A 144-day bottom-mounted ADP experiment at the entrance to Guaymas Bay was used to examine the vertical structure of the tidal flows of a small basin (33.6 km2) located in a semiarid region. Harmonic analysis techniques were used to extract the tidal ellipse parameters of the time series of ADP and to determine amplitude and phase of the tidal components of additional time series of tide height from two sites on the inner side of the bay taken before the experiment. The K1-current and the M2-current were the tidal currents of foremost importance; they were aligned with topography and showed amplitudes of 7.8 ± 0.2 cm s-1 and 7.4 ± 0.3 cm s-1, respectively. The M4-current was the principal shallow water tidal current with amplitude of 1.0 ± 0.2 cm s-1. Because of the small embayment condition, the main tidal motions showed characteristics of a standing wave. The vertical structure of the tidal currents was parabolic, which suggests that the barotropic tidal currents were affected by boundary layer process, furthermore, the mean current profile confirmed previous indication of an inverse estuarine circulation. The diurnal currents rotated anticlockwise in the upper layer and clockwise in the lower layer, which suggests that they were modulated by stratiflcation.doi: https://doi.org/10.22201/igeof.00167169p.2012.51.3.1196

773.1.#.t: Geofísica Internacional; Vol. 51 Núm. 3: Julio 1, 2012; 271-279

773.1.#.o: http://revistagi.geofisica.unam.mx/index.php/RGI

022.#.#.a: ISSN-L: 2954-436X; ISSN impreso: 0016-7169

310.#.#.a: Trimestral

300.#.#.a: Páginas: 271-279

264.#.1.b: Instituto de Geofísica, UNAM

doi: https://doi.org/10.22201/igeof.00167169p.2012.51.3.1196

handle: 00f9e8602f6bd08f

harvesting_date: 2023-06-20 16:00:00.0

856.#.0.q: application/pdf

file_creation_date: 2022-07-06 15:34:25.0

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file_creator: José Gómez-Valdés

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245.1.0.b: Vertical structure of tidal flows at the entrance to Guaymas Bay, Mexico

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Artículo

Vertical structure of tidal flows at the entrance to Guaymas Bay, Mexico

Gómez-valdés, José; J. Vázquez, Heriberto

Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM

Licencia de uso

Procedencia del contenido

Entidad o dependencia
Instituto de Geofísica, UNAM
Revista
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Gómez-valdés, José, et al. (2012). Vertical structure of tidal flows at the entrance to Guaymas Bay, Mexico. Geofísica Internacional; Vol. 51 Núm. 3: Julio 1, 2012; 271-279. Recuperado de https://repositorio.unam.mx/contenidos/4132167

Descripción del recurso

Autor(es)
Gómez-valdés, José; J. Vázquez, Heriberto
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Vertical structure of tidal flows at the entrance to Guaymas Bay, Mexico
Fecha
2012-07-01
Resumen
A 144-day bottom-mounted ADP experiment at the entrance to Guaymas Bay was used to examine the vertical structure of the tidal flows of a small basin (33.6 km2) located in a semiarid region. Harmonic analysis techniques were used to extract the tidal ellipse parameters of the time series of ADP and to determine amplitude and phase of the tidal components of additional time series of tide height from two sites on the inner side of the bay taken before the experiment. The K1-current and the M2-current were the tidal currents of foremost importance; they were aligned with topography and showed amplitudes of 7.8 ± 0.2 cm s-1 and 7.4 ± 0.3 cm s-1, respectively. The M4-current was the principal shallow water tidal current with amplitude of 1.0 ± 0.2 cm s-1. Because of the small embayment condition, the main tidal motions showed characteristics of a standing wave. The vertical structure of the tidal currents was parabolic, which suggests that the barotropic tidal currents were affected by boundary layer process, furthermore, the mean current profile confirmed previous indication of an inverse estuarine circulation. The diurnal currents rotated anticlockwise in the upper layer and clockwise in the lower layer, which suggests that they were modulated by stratiflcation.doi: https://doi.org/10.22201/igeof.00167169p.2012.51.3.1196
Tema
mareas; corrientes; laguna semiárida; Golfo de California; Bahía de Guaymas; tides; tidal current; semiarid lagoon; Gulf of California; Guaymas Bay
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces