dor_id: 4101882

506.#.#.a: Público

590.#.#.d: Cada artículo es evaluado mediante una revisión ciega única. Los revisores son externos nacionales e internacionales.

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)

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

336.#.#.b: info:eu-repo/semantics/article

336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

351.#.#.6: http://revistagi.geofisica.unam.mx/index.php/RGI

351.#.#.b: Geofísica Internacional

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harvesting_group: RevistasUNAM

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270.1.#.d: México

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883.#.#.a: Revistas UNAM

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

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856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1116/1095

100.1.#.a: Haggard, William H.

524.#.#.a: Haggard, William H. (1965). Clima tological-synoptic patterns associated with north atlantic tropical cyclogenesis. Geofísica Internacional; Vol. 5 No. 3, 1965. Recuperado de https://repositorio.unam.mx/contenidos/4101882

245.1.0.a: Clima tological-synoptic patterns associated with north atlantic tropical cyclogenesis

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1965

264.#.1.c: 2013-04-16

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-ND 4.0 Internacional, https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode.es, fecha de asignación de la licencia 2013-04-16, para un uso diferente consultar al responsable jurídico del repositorio por medio de revistagi@igeofisica.unam.mx

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1116

001.#.#.#: oai:ojs.ojs.geofisica.unam.mx:article/1116

041.#.7.h: spa

520.3.#.a: Several groups of North Atlantic tropical cyclogenetic situations were selected and composites of the associated synoptic patterns were developed. Each group was made as internally homogeneous as possible with respect to seasonal time and geographic location of cyclogenesis. A deliberate effort was made to obtain heterogeneity between groups and homogeneity within groups. Composite patterns of surface pressure, 500 mb. height and temperature, divergence and vorticity at these levels and surface to 500 mb. thickness were developed for the groups of storm origins selected. Similar groups of dates on which no storm development occurred were studied in the same manner. Comparisons are made between genetic and non-genetic patterns for several genetic areas and several parts of the storm season.

773.1.#.t: Geofísica Internacional; Vol. 5 No. 3 (1965)

773.1.#.o: http://revistagi.geofisica.unam.mx/index.php/RGI

046.#.#.j: 2020-10-20 00:00:00.000000

022.#.#.a: 0016-7169

310.#.#.a: Trimestral

264.#.1.b: Instituto de Geofísica, UNAM

758.#.#.1: http://revistagi.geofisica.unam.mx/index.php/RGI

handle: 00d860011e4396f5

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Artículo

Clima tological-synoptic patterns associated with north atlantic tropical cyclogenesis

Haggard, William H.

Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM

Licencia de uso

Procedencia del contenido

Entidad o dependencia
Instituto de Geofísica, UNAM
Revista
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Haggard, William H. (1965). Clima tological-synoptic patterns associated with north atlantic tropical cyclogenesis. Geofísica Internacional; Vol. 5 No. 3, 1965. Recuperado de https://repositorio.unam.mx/contenidos/4101882

Descripción del recurso

Autor(es)
Haggard, William H.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Clima tological-synoptic patterns associated with north atlantic tropical cyclogenesis
Fecha
2013-04-16
Resumen
Several groups of North Atlantic tropical cyclogenetic situations were selected and composites of the associated synoptic patterns were developed. Each group was made as internally homogeneous as possible with respect to seasonal time and geographic location of cyclogenesis. A deliberate effort was made to obtain heterogeneity between groups and homogeneity within groups. Composite patterns of surface pressure, 500 mb. height and temperature, divergence and vorticity at these levels and surface to 500 mb. thickness were developed for the groups of storm origins selected. Similar groups of dates on which no storm development occurred were studied in the same manner. Comparisons are made between genetic and non-genetic patterns for several genetic areas and several parts of the storm season.
Idioma
spa
ISSN
0016-7169

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