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

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336.#.#.a: Artículo

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

856.4.0.u: https://www.revistascca.unam.mx/atm/index.php/atm/article/view/8560/8030

100.1.#.a: Castro, R.; Mascarenhas, A.; Martínez Díaz De León, A.; Durazo, R.; Gil Silva, E.

524.#.#.a: Castro, R., et al. (2006). Spatial influence and oceanic thermal response to Santa Ana events along the Baja California Peninsula. Atmósfera; Vol. 19 No. 3, 2006. Recuperado de https://repositorio.unam.mx/contenidos/11127

245.1.0.a: Spatial influence and oceanic thermal response to Santa Ana events along the Baja California Peninsula

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

561.1.#.a: Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM

264.#.0.c: 2006

264.#.1.c: 2009-10-05

653.#.#.a: SANTA ANA CONDITION; METEOROLOGICAL STATIONS; PACIFIC AND GULF OF CALIFORNIA; HEAT FLUXES; Santa Ana condition; meteorological stations; Pacific and Gulf of California; heat fluxes

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 4.0 Internacional, https://creativecommons.org/licenses/by-nc/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico editora@atmosfera.unam.mx

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041.#.7.h: eng

520.3.#.a: Meteorological data were recorded at eight stations located along the coast of the Pacific Ocean and three along the coast of the Gulf of California, aimed to assess the spatial influence of Santa Ana weather conditions in the Baja California Peninsula. February 2002 featured two Santa Ana events: one from the 9 to the 12 and another from the 21 to the 22. The first Santa Ana event had the strongest winds, however relative humidity and temperature behaved similarly on both events at some stations. Data from the Pacific Ocean showed typical Santa Ana condition patterns: wind speed and temperature increase opposed to decreased relative humidity values. Data from the Gulf of California did not show the typical temperature rise of a Santa Ana condition, but there was a decrease on the amplitude of the diurnal variability of air temperature and relative humidity as well as a marked increase on wind strength. Wind direction during the Santa Ana events on the Pacific side was NE and NW on the Gulf of California. NE winds are associated to the shift on the position of the North Pacific High Pressure Center, which moves towards the continent. Data suggest that relative humidity may be the best parameter to monitor both occurrence and length of Santa Ana conditions on the Pacific side. Normal weather conditions show a negative air-sea temperature difference, but during both Santa Ana events this difference was positive and higher than 10 ºC. Latent and sensible heat fluxes drastically increased during both events, reaching values more than three times higher than those for normal conditions, which is due to the presence of strong winds combined with a drier and hotter air mass over the ocean.

773.1.#.t: Atmósfera; Vol. 19 No. 3 (2006)

773.1.#.o: https://www.revistascca.unam.mx/atm/index.php/atm/index

046.#.#.j: 2021-10-20 00:00:00.000000

022.#.#.a: ISSN electrónico: 2395-8812; ISSN impreso: 0187-6236

310.#.#.a: Trimestral

264.#.1.b: Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM

handle: 009c4c7c165c9ca0

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

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245.1.0.b: Spatial influence and oceanic thermal response to Santa Ana events along the Baja California peninsula

last_modified: 2023-06-20 16:00:00

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Artículo

Spatial influence and oceanic thermal response to Santa Ana events along the Baja California Peninsula

Castro, R.; Mascarenhas, A.; Martínez Díaz De León, A.; Durazo, R.; Gil Silva, E.

Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM, publicado en Atmósfera, y cosechado de Revistas UNAM

Licencia de uso

Procedencia del contenido

Entidad o dependencia
Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM
Revista
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Castro, R., et al. (2006). Spatial influence and oceanic thermal response to Santa Ana events along the Baja California Peninsula. Atmósfera; Vol. 19 No. 3, 2006. Recuperado de https://repositorio.unam.mx/contenidos/11127

Descripción del recurso

Autor(es)
Castro, R.; Mascarenhas, A.; Martínez Díaz De León, A.; Durazo, R.; Gil Silva, E.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Spatial influence and oceanic thermal response to Santa Ana events along the Baja California Peninsula
Fecha
2009-10-05
Resumen
Meteorological data were recorded at eight stations located along the coast of the Pacific Ocean and three along the coast of the Gulf of California, aimed to assess the spatial influence of Santa Ana weather conditions in the Baja California Peninsula. February 2002 featured two Santa Ana events: one from the 9 to the 12 and another from the 21 to the 22. The first Santa Ana event had the strongest winds, however relative humidity and temperature behaved similarly on both events at some stations. Data from the Pacific Ocean showed typical Santa Ana condition patterns: wind speed and temperature increase opposed to decreased relative humidity values. Data from the Gulf of California did not show the typical temperature rise of a Santa Ana condition, but there was a decrease on the amplitude of the diurnal variability of air temperature and relative humidity as well as a marked increase on wind strength. Wind direction during the Santa Ana events on the Pacific side was NE and NW on the Gulf of California. NE winds are associated to the shift on the position of the North Pacific High Pressure Center, which moves towards the continent. Data suggest that relative humidity may be the best parameter to monitor both occurrence and length of Santa Ana conditions on the Pacific side. Normal weather conditions show a negative air-sea temperature difference, but during both Santa Ana events this difference was positive and higher than 10 ºC. Latent and sensible heat fluxes drastically increased during both events, reaching values more than three times higher than those for normal conditions, which is due to the presence of strong winds combined with a drier and hotter air mass over the ocean.
Tema
SANTA ANA CONDITION; METEOROLOGICAL STATIONS; PACIFIC AND GULF OF CALIFORNIA; HEAT FLUXES; Santa Ana condition; meteorological stations; Pacific and Gulf of California; heat fluxes
Idioma
eng
ISSN
ISSN electrónico: 2395-8812; ISSN impreso: 0187-6236

Enlaces