dor_id: 4122618

506.#.#.a: Público

590.#.#.d: Los artículos enviados a la revista "Atmósfera", se juzgan por medio de un proceso de revisión por pares

510.0.#.a: Consejo Nacional de Ciencia y Tecnología (CONACyT); Sistema Regional de Información en Línea para Revistas Científicas de América Latina, el Caribe, España y Portugal (Latindex); Scientific Electronic Library Online (SciELO); SCOPUS, Web Of Science (WoS); SCImago Journal Rank (SJR)

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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: https://www.revistascca.unam.mx/atm/index.php/atm/index

351.#.#.b: Atmósfera

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

270.1.#.d: México

590.#.#.b: Concentrador

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

883.#.#.a: Revistas UNAM

590.#.#.a: Coordinación de Difusión Cultural

883.#.#.1: https://www.publicaciones.unam.mx/

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

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

856.4.0.u: https://www.revistascca.unam.mx/atm/index.php/atm/article/view/8494/7964

100.1.#.a: Zavala Hidalgo, J.; Pares Sierra, Alejandro; Ochoa, J.

524.#.#.a: Zavala Hidalgo, J., et al. (2002). Seasonal variability of the temperature and heat fluxes in the Gulf of Mexico. Atmósfera; Vol. 15 No. 2, 2002. Recuperado de https://repositorio.unam.mx/contenidos/4122618

245.1.0.a: Seasonal variability of the temperature and heat fluxes in the Gulf of Mexico

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

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

264.#.0.c: 2002

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

653.#.#.a: Gulf of México; heat fluxes; numerical model; sea surface temperature; seasonal variability; GOLFO DE MÉXICO; FLUJOS DE CALOR; MODELACION NUMERICA; TEMPERATURA SUPERFICIAL DEL MAR; VARIACION ESTACIONAL; GULF OF MÉXICO; HEAT FLUXES; NUMERICAL MODEL; SEA SURFACE TEMPERATURE; SEASONAL VARIABILITY

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

884.#.#.k: https://www.revistascca.unam.mx/atm/index.php/atm/article/view/8494

001.#.#.#: 022.oai:ojs.pkp.sfu.ca:article/8494

041.#.7.h: eng

520.3.#.a: Heat fluxes between the atmosphere and the sea surface in the Gulf of Mexico are computed using the GOADS climatology, bulk formulae, radiation estimations from satellite, and a numerical model. 9 W m-2 is the estimated mean surface heat flux into the ocean, this is higher than previous studies due to different bulk formulae and data sources. The annual cycle has an amplitude of 168 W m-2. The contribution of each term in the heat equation is computed, analyzed and compared to previous studies. A numerical model with thermodynamics is used to study the relative importance of heat advection and entrainment on the sea surface temperature. The results indicate that the entrainment is important in the winter cooling of surface waters. When entrainment, which depends on the buoyancy loss and the wind induced turbulent kinetic energy, is not included, temperatures in winter stay higher than observations, with a root mean square (RMS) difference from observations of l.5ºC. Including entrainment and detrainment the RMS decreases to 1.0 ºC.

773.1.#.t: Atmósfera; Vol. 15 No. 2 (2002)

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: 00d9c2dc522b408a

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

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245.1.0.b: Seasonal variability of the temperature and heat fluxes in the Gulf of México

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license_url: https://creativecommons.org/licenses/by-nc/4.0/legalcode.es

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Artículo

Seasonal variability of the temperature and heat fluxes in the Gulf of Mexico

Zavala Hidalgo, J.; Pares Sierra, Alejandro; Ochoa, J.

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

Zavala Hidalgo, J., et al. (2002). Seasonal variability of the temperature and heat fluxes in the Gulf of Mexico. Atmósfera; Vol. 15 No. 2, 2002. Recuperado de https://repositorio.unam.mx/contenidos/4122618

Descripción del recurso

Autor(es)
Zavala Hidalgo, J.; Pares Sierra, Alejandro; Ochoa, J.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Seasonal variability of the temperature and heat fluxes in the Gulf of Mexico
Fecha
2009-10-05
Resumen
Heat fluxes between the atmosphere and the sea surface in the Gulf of Mexico are computed using the GOADS climatology, bulk formulae, radiation estimations from satellite, and a numerical model. 9 W m-2 is the estimated mean surface heat flux into the ocean, this is higher than previous studies due to different bulk formulae and data sources. The annual cycle has an amplitude of 168 W m-2. The contribution of each term in the heat equation is computed, analyzed and compared to previous studies. A numerical model with thermodynamics is used to study the relative importance of heat advection and entrainment on the sea surface temperature. The results indicate that the entrainment is important in the winter cooling of surface waters. When entrainment, which depends on the buoyancy loss and the wind induced turbulent kinetic energy, is not included, temperatures in winter stay higher than observations, with a root mean square (RMS) difference from observations of l.5ºC. Including entrainment and detrainment the RMS decreases to 1.0 ºC.
Tema
Gulf of México; heat fluxes; numerical model; sea surface temperature; seasonal variability; GOLFO DE MÉXICO; FLUJOS DE CALOR; MODELACION NUMERICA; TEMPERATURA SUPERFICIAL DEL MAR; VARIACION ESTACIONAL; GULF OF MÉXICO; HEAT FLUXES; NUMERICAL MODEL; SEA SURFACE TEMPERATURE; SEASONAL VARIABILITY
Idioma
eng
ISSN
ISSN electrónico: 2395-8812; ISSN impreso: 0187-6236

Enlaces