dor_id: 11336

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)

561.#.#.u: https://www.atmosfera.unam.mx/

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/45560/42487

100.1.#.a: Zavala-hidalgo, Jorge; Romero-centeno, Rosario; Mateos-jasso, Adriana; L. Morey, Steven; Martínez-lópez, Benjamín

524.#.#.a: Zavala-hidalgo, Jorge, et al. (2014). The response of the Gulf of Mexico to wind and heat flux forcing: What has been learned in recent years?. Atmósfera; Vol. 27 No. 3, 2014. Recuperado de https://repositorio.unam.mx/contenidos/11336

720.#.#.a: PAPIIT, CONACyTPAPIIT, CONACyT

245.1.0.a: The response of the Gulf of Mexico to wind and heat flux forcing: What has been learned in recent years?

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

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

264.#.0.c: 2014

264.#.1.c: 2015-01-12

653.#.#.a: Gulf of Mexico; ocean surface forcing; upper ocean layer

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/45560

001.#.#.#: 022.oai:ojs.pkp.sfu.ca:article/45560

041.#.7.h: eng

520.3.#.a: The Loop Current and its shed eddies dominate the circulation and dynamics of the Gulf of Mexico (GoM) basin. Those eddies are strongly energetic and are the cause of intense currents that may penetrate several hundred meters deep. However, there are regions in the GoM and periods of time in which the local atmospheric forcing plays an important role in its dynamics and thermodynamics. The circulation on theshelves, and particularly on the inner shelf, is mainly wind-driven with seasonality, changing direction duringthe year with periods of favorable upwelling/downwelling conditions. The wind-driven circulation is associatedwith the transport of waters with different temperature and salinity characteristics from one region toanother. The interannual variability of the circulation on the shelves is linked to the atmospheric variability.Intraseasonal variability of the wind patterns considerably affects the likelihood and magnitude of upwellingand downwelling. The geometry of the GoM is such that large-scale winds may drive opposing upcoast/downcoast currents along different parts of the curving coast, resulting in convergence or divergence zones.The width of the shelves in the GoM is variable;while the West Florida Shelf, the Texas-Louisiana shelfand the Campeche Bank are more than 200 km wide, they are narrower near Veracruz and Tabasco. Anotherconsequence of the GoM physiography and the wind forcing is the development of cross-shelf transports inthe southern Bay of Campeche, the southern Texas shelf and southeast of the Mississippi river, which in turnvary during the year. During autumn-winter (from September to April), the GoM is affected by cold frontscoming from the northwest United States, which are associated with strong, dry, and cold winds that mixits waters and generate large sensible and latent heat fluxes from the ocean to the atmosphere. These frontalpassages also cool the GoM surface waters due to mixing with lower temperature subsurface waters. Duringsummer, tropical cyclones crossing the GoM can dramatically affect circulation and coastal upwelling.

773.1.#.t: Atmósfera; Vol. 27 No. 3 (2014)

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: 00e88eac0b22de57

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

856.#.0.q: application/pdf

245.1.0.b: The response of the Gulf of Mexico to wind and heat flux forcing: What has been learned in recent years?

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

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

license_type: by-nc

_deleted_conflicts: 2-46005d4cb22eb338e297058ed50a085f

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