dor_id: 4141350

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

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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)

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856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1604/1716

100.1.#.a: Kessler Iii., Edwin

524.#.#.a: Kessler Iii., Edwin (1965). Microphysical parameters in relation to tropical cloud and precipitation distributions and their modification. Geofísica Internacional; Vol. 5 Núm. 3: Julio 1, 1965; 79-88. Recuperado de https://repositorio.unam.mx/contenidos/4141350

245.1.0.a: Microphysical parameters in relation to tropical cloud and precipitation distributions and their modification

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1965

264.#.1.c: 1965-07-01

653.#.#.a: Precipitación tropical; Parámetros microfísicos; Ciclo hidrológico; Tropical precipitation; Microphysical parameters; Hydrological cycle

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/1604

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1604

041.#.7.h: spa

520.3.#.a: Microphysical parameters and the vertical wind profile are considered in relation to the shapes of spatial and temporal distributions of tropical rainfall. For a particular vertical velocity field, the precipitation beneath an updraft center is concentrated relative to that away from the center by increasing relative numbers of small drops in the distribution of rain particles. Increased collection efficiency of rain for cloud and a faster rate of growth of cloud particles reduces the amount of condensate which is carried to high levels and lost by effects of horizontal divergence to the immediate precipitation at the ground. The time of precipitation onset at the ground is related to updraft speed, drop distribution parameters, collection efficiencies, and cloud conversion rates. Relatively large changes of the microphysical parameters are required to alter the rain distribution at the ground appreciably, because the responses of water distribution in the model system usually tend to offset the effects of the microphysical changes. Possible responses of cloudiness and precipitation to modification of the microphysical parameters are discussed in the light of the model, with the assumption that the updraft distribution is unaffected by variations of the vertical profiles of cloud and precipitation. The possible of the Earth is also noted.

773.1.#.t: Geofísica Internacional; Vol. 5 Núm. 3: Julio 1, 1965; 79-88

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: 79-88

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

doi: https://doi.org/10.22201/igeof.00167169p.1965.5.3.1114

handle: 00f5c68e7b16aa45

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

856.#.0.q: application/pdf

file_creation_date: 2008-07-03 21:38:36.0

file_modification_date: 2022-06-16 17:51:06.0

file_creator: Edwin Kessler III.

file_name: 17c75134b954127de7ea0190cd6601e89880680c594e345b5f9114c391a9965f.pdf

file_pages_number: 10

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245.1.0.b: Parámetros microfísicos en relación con la distribución y precipitación de nubes tropicales y su modificación

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

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Artículo

Microphysical parameters in relation to tropical cloud and precipitation distributions and their modification

Kessler Iii., Edwin

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

Kessler Iii., Edwin (1965). Microphysical parameters in relation to tropical cloud and precipitation distributions and their modification. Geofísica Internacional; Vol. 5 Núm. 3: Julio 1, 1965; 79-88. Recuperado de https://repositorio.unam.mx/contenidos/4141350

Descripción del recurso

Autor(es)
Kessler Iii., Edwin
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Microphysical parameters in relation to tropical cloud and precipitation distributions and their modification
Fecha
1965-07-01
Resumen
Microphysical parameters and the vertical wind profile are considered in relation to the shapes of spatial and temporal distributions of tropical rainfall. For a particular vertical velocity field, the precipitation beneath an updraft center is concentrated relative to that away from the center by increasing relative numbers of small drops in the distribution of rain particles. Increased collection efficiency of rain for cloud and a faster rate of growth of cloud particles reduces the amount of condensate which is carried to high levels and lost by effects of horizontal divergence to the immediate precipitation at the ground. The time of precipitation onset at the ground is related to updraft speed, drop distribution parameters, collection efficiencies, and cloud conversion rates. Relatively large changes of the microphysical parameters are required to alter the rain distribution at the ground appreciably, because the responses of water distribution in the model system usually tend to offset the effects of the microphysical changes. Possible responses of cloudiness and precipitation to modification of the microphysical parameters are discussed in the light of the model, with the assumption that the updraft distribution is unaffected by variations of the vertical profiles of cloud and precipitation. The possible of the Earth is also noted.
Tema
Precipitación tropical; Parámetros microfísicos; Ciclo hidrológico; Tropical precipitation; Microphysical parameters; Hydrological cycle
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces