dor_id: 4133538

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/1581/1702

100.1.#.a: Tahnk, William R.; Newell, Reginald E.

524.#.#.a: Tahnk, William R., et al. (1975). Climatology and energy budget of the northern hemisphere middle stratosphere durind 197. Geofísica Internacional; Vol. 15 Núm. 3: Julio 1, 1975; 205-292. Recuperado de https://repositorio.unam.mx/contenidos/4133538

245.1.0.a: Climatology and energy budget of the northern hemisphere middle stratosphere durind 197

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1975

264.#.1.c: 1975-07-01

653.#.#.a: Climatología; Balance energético; Estratósfera media; Ondas estacionarias; Hemisferio norte; Climatology; Energy budget; Middle stratosphere; Standing waves; North Hemisphere

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/1581

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1581

041.#.7.h: spa

520.3.#.a: The 10-2 mb (~30.4 3 km) layer of the atmosphere in winter receives energy from two different sources: mechanical energy is carried up from the troposphere and lower stratosphere while energy is generated in situ by the gradients of radiative heating and cooling. We show here from data for 1972 that the latter primarily governs the energy budget of the middle stratosphere in early winter while the former becomes of comparable size, and often dominates, in the middle and late winter. Radiative energy sources for the summer hemisphere arc very small, as there is considerable compensation between solar heating through ozone absorption and infrared cooling by carbon dioxide and ozone. Standing and travelling waves are quite clear-cut at 5 and 2 mb in winter, as much of the chaos of lower regions is filtered out in the lower stratosphere; the standing waves at 2 mb may reflect surface properties more effectively than flow patterns at lower levels. A westward-travelling wave, with a period of about a month, was evident in early 1972.

773.1.#.t: Geofísica Internacional; Vol. 15 Núm. 3: Julio 1, 1975; 205-292

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: 205-292

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

doi: https://doi.org/10.22201/igeof.00167169p.1975.15.3.994

handle: 34300f3dd15f606a

harvesting_date: 2023-06-20 16:00:00.0

856.#.0.q: application/pdf

file_creation_date: 2008-06-30 17:44:19.0

file_modification_date: 2023-02-03 18:45:11.0

file_creator: William R. Tahnk

file_name: 8c14fc33c7e73fa75074ac51e010bd45353f347e4bc68dfd732e019d02a9c784.pdf

file_pages_number: 88

file_format_version: application/pdf; version=1.6

file_size: 21877882

245.1.0.b: Climatology and energy budget of the northern hemisphere middle stratosphere durind 1972.

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

No entro en nada

No entro en nada 2

Artículo

Climatology and energy budget of the northern hemisphere middle stratosphere durind 197

Tahnk, William R.; Newell, Reginald E.

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

Tahnk, William R., et al. (1975). Climatology and energy budget of the northern hemisphere middle stratosphere durind 197. Geofísica Internacional; Vol. 15 Núm. 3: Julio 1, 1975; 205-292. Recuperado de https://repositorio.unam.mx/contenidos/4133538

Descripción del recurso

Autor(es)
Tahnk, William R.; Newell, Reginald E.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Climatology and energy budget of the northern hemisphere middle stratosphere durind 197
Fecha
1975-07-01
Resumen
The 10-2 mb (~30.4 3 km) layer of the atmosphere in winter receives energy from two different sources: mechanical energy is carried up from the troposphere and lower stratosphere while energy is generated in situ by the gradients of radiative heating and cooling. We show here from data for 1972 that the latter primarily governs the energy budget of the middle stratosphere in early winter while the former becomes of comparable size, and often dominates, in the middle and late winter. Radiative energy sources for the summer hemisphere arc very small, as there is considerable compensation between solar heating through ozone absorption and infrared cooling by carbon dioxide and ozone. Standing and travelling waves are quite clear-cut at 5 and 2 mb in winter, as much of the chaos of lower regions is filtered out in the lower stratosphere; the standing waves at 2 mb may reflect surface properties more effectively than flow patterns at lower levels. A westward-travelling wave, with a period of about a month, was evident in early 1972.
Tema
Climatología; Balance energético; Estratósfera media; Ondas estacionarias; Hemisferio norte; Climatology; Energy budget; Middle stratosphere; Standing waves; North Hemisphere
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces