dor_id: 4141330

506.#.#.a: Público

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

510.0.#.a: Consejo Nacional de Ciencia y Tecnología (CONACyT); Scientific Electronic Library Online (SciELO); SCOPUS, Dialnet, Directory of Open Access Journals (DOAJ); Geobase

561.#.#.u: https://www.geofisica.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: http://revistagi.geofisica.unam.mx/index.php/RGI

351.#.#.b: Geofísica Internacional

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: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1696/1851

100.1.#.a: Atlas, David; Hardy, Kenneth R.; Wexler, Raymond; Boucher, Roland J.

524.#.#.a: Atlas, David, et al. (1963). On the origin of hurricane spiral bands. Geofísica Internacional; Vol. 3 Núm. 4: Octubre 1, 1963; 123-132. Recuperado de https://repositorio.unam.mx/contenidos/4141330

245.1.0.a: On the origin of hurricane spiral bands

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1963

264.#.1.c: 1963-10-01

653.#.#.a: Meteorología; Bandas espiraladas; Huracanes; Meteorology; Spiral band; Hurricanes

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

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1696

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1696

041.#.7.h: spa

520.3.#.a: Vertical radar cross-sections of echo intensity in Hurricane Esther are used to build a three dimensional model of a spiral band. This model and PPI time-lapse movies show that the large persistent bands are essentially stratiform and have convective type clouds only at their upwind ends. The convective clouds are observed to develop upband outward relative to the eye, while spewing out precipitation particles which stream down-wind in plume· like fashion. The net effect is echo motion along the band in both direction; the plume extends downwind while the source cloud propagates upwind. The outward radial component of propagation of the source cloud gives the band its outward velocity. The major growth is concentrated in the stratiform region of the band at middle and low levels below 18,000 ft (0° C level at 14,000 ft). The presence of the bright band in the melting layer precludes that the moisture supply for growth occurs in the form of strong convective currents. A mechanism is proposed in which cooling by evaporation and melting snow con tributes to the establishment of a spiral line of convergence near the advancing edge of the band and gives rise to a cumuliform roll cloud. Cooling by melting snow within the core of the hand establishes a 0° C isothermal and causes instability which results in a finer scale handedness of stratocumulus below the melting level. The mechanism is consistent with direct meteorological observations; namely, that a few per cent of the precipitation area is comprised of "hot" convective towers, that the intermediate spiral bands are usually cold core, and that relatively modest turbulence is experienced within them.

773.1.#.t: Geofísica Internacional; Vol. 3 Núm. 4: Octubre 1, 1963; 123-132

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

022.#.#.a: ISSN-L: 2954-436X; ISSN impreso: 0016-7169

310.#.#.a: Trimestral

300.#.#.a: Páginas: 123-132

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

doi: https://doi.org/10.22201/igeof.2954436xe.1963.3.4.1696

handle: 4a0e6de45d4298a4

harvesting_date: 2023-06-20 17:00:00.0

856.#.0.q: application/pdf

file_creation_date: 2023-01-31 16:14:51.0

file_modification_date: 2023-04-27 20:45:10.0

file_creator: David Atlas

file_name: 3701c7f320cd1fd39ed9fc58f3db69fe49500f4fca1de1ffad4189dfc11e4c96.pdf

file_pages_number: 14

file_format_version: application/pdf; version=1.6

file_size: 1398812

245.1.0.b: Sobre el origen de las bandas espiraladas de los huracanes

last_modified: 2023-06-20 17:00:00

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

license_type: by-nc-sa

No entro en nada

No entro en nada 2