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
dor_id: 4132167
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336.#.#.b: article
336.#.#.3: Artículo de Investigación
336.#.#.a: Artículo
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351.#.#.b: Geofísica Internacional
351.#.#.a: Artículos
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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
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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
file_modification_date: 2022-07-06 15:34:25.0
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
last_modified: 2023-06-20 16:00:00
license_url: https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es
license_type: by-nc-sa
Gómez-valdés, José; J. Vázquez, Heriberto
Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM
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