dor_id: 4120156

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/8307/7777

100.1.#.a: Zehnder, Joshep A.; Gall, Robert L.

524.#.#.a: Zehnder, Joshep A., et al. (1991). Alternative mechanisms of tropical cyclone formation in the Eastern North Pacific. Atmósfera; Vol. 4 No. 1, 1991. Recuperado de https://repositorio.unam.mx/contenidos/4120156

245.1.0.a: Alternative mechanisms of tropical cyclone formation in the Eastern North Pacific

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

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

264.#.0.c: 1991

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

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/8307

001.#.#.#: 022.oai:ojs.pkp.sfu.ca:article/8307

041.#.7.h: eng

520.3.#.a: It has been known for some time that the subtropical Eastern North Pacific Ocean, just west of the coast of Mexico experiences a high incidence of tropical cylone formation. One currently accepted mechanism for tropical cyclone initiation in the Eastern Pacific involves easterly waves that originate over Africa and propagate across the Atlantic. Recent investigations indicate that other mechanisms, such as the interaction of the large scale flow with the topography or the formation of mesoscale convective systems (MCSs), may also be important in initiating tropical cyclones in this region. Infrared satellite imagery is used to illustrate specific examples of the alternative mechanisms described above that occurred during the 1989 hurricane season. Hurricane Lorena and Tropical Storm Manuel appear to have originated from a single region of disturbed weather associated with flow over the Sierra Madres and Tropical Storm Priscilla appears to have formed from an MCS that first appeared over Mexico. Conventional sounding and wind data are used to demostrate that the incident flow present was favorable for the generation of orographic cyclones during the formation of Lorena and Manuel and that the environment was conditioned for MCS formation prior to the development of Priscilla.

773.1.#.t: Atmósfera; Vol. 4 No. 1 (1991)

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

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

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245.1.0.b: Alternative mechanisms of tropical cyclone formation in the Eastern North Pacific

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