dor_id: 4141229

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/1689/1843

100.1.#.a: Riehl, Herbert

524.#.#.a: Riehl, Herbert (1963). Inaugural address. Stationary aspects of the tropical general circulation.. Geofísica Internacional; Vol. 3 Núm. 3: Julio 1, 1963; 53-68. Recuperado de https://repositorio.unam.mx/contenidos/4141229

245.1.0.a: Inaugural address. Stationary aspects of the tropical general circulation.

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1963

264.#.1.c: 1963-07-01

653.#.#.a: Meteorología; Alisio del Atlántico; Alisio del Pacífico; Monson; Circulación de verano media; Meteorology; Atlantic trade; Pacific trade; Monsoon; Mean summer circulation

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/1689

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1689

041.#.7.h: spa

520.3.#.a: At first, the mean summer circulation is surveyed for three meteorological regimes near the surface and at 200 mb: the Atlantic trade, the Pacific trade and the Asiatic monsoon. There is a complete inversion of atmospheric structure comparing the trades with the monsoon. In the trades the lower winds are steady and diverging; at 200-mb high cyclonic vorticity along narrow shearlines with convergence is found. The air is cold relative to the surroundings in these shearlines. Frequently the flow is quite unsteady, with large or small cyclonic vortices travelling west along the shear line. The monsoon has the same structure, inverted. Here the steady easterlies with divergent anticyclonic flow are found in the high troposphere above the well known monsoon or equatorial low pressure trough with strong cyclonic shear and moving disturbances. Temperatures in the trough are very high, especially in the upper troposphere. Computations are performed to determine whether the stationary part of trade and monsoon regimes can provide for balance of heat, moisture and kinetic energy. It is found that this is the case and that unsteady flow features or forcing from extra tropical latitude~ need not be invoked to maintain the tropical summer circulation systems. In particular, the efficiency of conversion of latent heat release to production of kinetic energy by the mean circulation is found to be 2.5 per cent, about the same as computed for conversion of potential to kinetic energy in extratropical disturbances.

773.1.#.t: Geofísica Internacional; Vol. 3 Núm. 3: Julio 1, 1963; 53-68

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: 53-68

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

doi: https://doi.org/10.22201/igeof.2954436xe.1963.3.3.1689

handle: 3e57b1d182b52dfd

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

856.#.0.q: application/pdf

file_creation_date: 2023-01-31 15:45:06.0

file_modification_date: 2023-04-25 22:37:44.0

file_creator: Herbert Riehl

file_name: 15445a02165701390edb38ae3f10a5d16865137764e67a4a6b385c23bb2f76cc.pdf

file_pages_number: 16

file_format_version: application/pdf; version=1.6

file_size: 1415464

245.1.0.b: Discurso inaugural. Aspectos estacionarios de la circulación general tropical

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

Inaugural address. Stationary aspects of the tropical general circulation.

Riehl, Herbert

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

Riehl, Herbert (1963). Inaugural address. Stationary aspects of the tropical general circulation.. Geofísica Internacional; Vol. 3 Núm. 3: Julio 1, 1963; 53-68. Recuperado de https://repositorio.unam.mx/contenidos/4141229

Descripción del recurso

Autor(es)
Riehl, Herbert
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Inaugural address. Stationary aspects of the tropical general circulation.
Fecha
1963-07-01
Resumen
At first, the mean summer circulation is surveyed for three meteorological regimes near the surface and at 200 mb: the Atlantic trade, the Pacific trade and the Asiatic monsoon. There is a complete inversion of atmospheric structure comparing the trades with the monsoon. In the trades the lower winds are steady and diverging; at 200-mb high cyclonic vorticity along narrow shearlines with convergence is found. The air is cold relative to the surroundings in these shearlines. Frequently the flow is quite unsteady, with large or small cyclonic vortices travelling west along the shear line. The monsoon has the same structure, inverted. Here the steady easterlies with divergent anticyclonic flow are found in the high troposphere above the well known monsoon or equatorial low pressure trough with strong cyclonic shear and moving disturbances. Temperatures in the trough are very high, especially in the upper troposphere. Computations are performed to determine whether the stationary part of trade and monsoon regimes can provide for balance of heat, moisture and kinetic energy. It is found that this is the case and that unsteady flow features or forcing from extra tropical latitude~ need not be invoked to maintain the tropical summer circulation systems. In particular, the efficiency of conversion of latent heat release to production of kinetic energy by the mean circulation is found to be 2.5 per cent, about the same as computed for conversion of potential to kinetic energy in extratropical disturbances.
Tema
Meteorología; Alisio del Atlántico; Alisio del Pacífico; Monson; Circulación de verano media; Meteorology; Atlantic trade; Pacific trade; Monsoon; Mean summer circulation
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces