A note on the cisk mechanism in the tropics and its role in disturbance formation and maintenance
Simpson, Joanne
Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM
dor_id: 4133114
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351.#.#.b: Geofísica Internacional
351.#.#.a: Artículos
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856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1510/1629
100.1.#.a: Simpson, Joanne
524.#.#.a: Simpson, Joanne (1975). A note on the cisk mechanism in the tropics and its role in disturbance formation and maintenance. Geofísica Internacional; Vol. 15 Núm. 2: Abril 1, 1975; 89-101. Recuperado de https://repositorio.unam.mx/contenidos/4133114
245.1.0.a: A note on the cisk mechanism in the tropics and its role in disturbance formation and maintenance
502.#.#.c: Universidad Nacional Autónoma de México
561.1.#.a: Instituto de Geofísica, UNAM
264.#.0.c: 1975
264.#.1.c: 1975-04-01
653.#.#.a: CISK; Sistemas de cúmulos; Tormentas tropicales; Trópico; Huracanes; Cumulus systems; Tropical storms; Tropics; Hurricanes
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884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1510
001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1510
041.#.7.h: spa
520.3.#.a: The concept of CISK, or "conditional instability of the second kind" has been advanced to explain the growth of cumulus systems and the intensification of tropical disturbances to storm or hurricane intensity. CISK has also been postulated as a basis for parameterization of cumulus processes in large-scale models. Its investigation played a role in the design and planned analyses of the 1974 GATE experiment. The heart of the CISK concept involves frictionally driven convergence in an Ekman boundary layer, which is supposed to intensify convection, which in turn enhances the boundary layer convergence. Many CISK models equate the Ekman friction layer with the layer below cumulus base in the tropics. This paper corrects this error by showing that the frictional boundary layer in the tropics extends to cumulus tops. Several different types of scale interactions in the tropics are examined. Specific suggestions for broadening the CISK concept are made relative both to tropical storm deepening and to the parameterization of cumulus processes.
773.1.#.t: Geofísica Internacional; Vol. 15 Núm. 2: Abril 1, 1975; 89-101
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: 89-101
264.#.1.b: Instituto de Geofísica, UNAM
doi: https://doi.org/10.22201/igeof.00167169p.1975.15.2.1136
handle: 00c8be0dacebb1ce
harvesting_date: 2023-06-20 16:00:00.0
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file_creation_date: 2008-06-30 15:14:36.0
file_modification_date: 2023-02-03 18:01:57.0
file_creator: Joanne Simpson
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245.1.0.b: A note on the cisk mechanism in the tropics and its role in disturbance formation and maintenance
last_modified: 2023-06-20 16:00:00
license_url: https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es
license_type: by-nc-sa
Simpson, Joanne
Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM
Simpson, Joanne (1975). A note on the cisk mechanism in the tropics and its role in disturbance formation and maintenance. Geofísica Internacional; Vol. 15 Núm. 2: Abril 1, 1975; 89-101. Recuperado de https://repositorio.unam.mx/contenidos/4133114