dor_id: 4119840

506.#.#.a: Público

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

510.0.#.a: Consejo Nacional de Ciencia y Tecnología (CONACyT); Sistema Regional de Información en Línea para Revistas Científicas de América Latina, el Caribe, España y Portugal (Latindex); Scientific Electronic Library Online (SciELO); SCOPUS, Web Of Science (WoS); SCImago Journal Rank (SJR)

561.#.#.u: https://www.atmosfera.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: https://www.revistascca.unam.mx/atm/index.php/atm/index

351.#.#.b: Atmósfera

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: https://www.revistascca.unam.mx/atm/index.php/atm/article/view/8392/7862

100.1.#.a: Wiin Nielsen, A.

524.#.#.a: Wiin Nielsen, A. (1995). On stability of jetstreams. Atmósfera; Vol. 8 No. 4, 1995. Recuperado de https://repositorio.unam.mx/contenidos/4119840

245.1.0.a: On stability of jetstreams

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

561.1.#.a: Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM

264.#.0.c: 1995

264.#.1.c: 2009-10-05

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

884.#.#.k: https://www.revistascca.unam.mx/atm/index.php/atm/article/view/8392

001.#.#.#: 022.oai:ojs.pkp.sfu.ca:article/8392

041.#.7.h: eng

520.3.#.a: The quasi-geostrophic, baroclinic stability problem is solved using vertical structure functions corresponding to a vertical variation of the static stability parameter which is inversely proportional to the square of the pressure. Due to this assumption it is necessary to apply the upper boundary condition at a pressure level different from the outer limit of the atmosphere. While this technique has been used earlier, the emphasis in this paper is on the stability of jet profiles. Various jet-like profiles of the zonal wind are defined mathematically, and they are used to investigate how the stability depends on the maximum wind, the position of the jet maximum, the sharpness of the jet, and also the position of the upper boundary. A comparison is made with the stability of the advective model for which the stability may be obtained analytically. From the general, quasi-geostrophic model it is found that a short-wave cut-off exists, while instability exists for all wavelenghts larger than the cut-off wavelength, i.e. no long-wave cut-off exists. Smaller instabilities occurs when the maximum wind is around 300 hPa, when the top level is located at 30 hPa, and when the jet profiles are well rounded. A wind profile with "stratospheric easterlies" has about the same stability for Rossby waves of a few thousand kilometers as a profile with westerlies at all levels. However, for very long waves the profile with easterlies is more unstable.

773.1.#.t: Atmósfera; Vol. 8 No. 4 (1995)

773.1.#.o: https://www.revistascca.unam.mx/atm/index.php/atm/index

046.#.#.j: 2021-10-20 00:00:00.000000

022.#.#.a: ISSN electrónico: 2395-8812; ISSN impreso: 0187-6236

310.#.#.a: Trimestral

264.#.1.b: Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM

handle: 00c4b60d5eb2dd39

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

856.#.0.q: application/pdf

file_creation_date: 2001-08-31 22:48:36.0

file_modification_date: 2001-08-31 22:50:32.0

file_name: cc8b37692f7e1207bb10006ca6d9fbb6dc21f44f03a9d4f17d5043e17288338a.pdf

file_pages_number: 13

file_format_version: application/pdf; version=1.3

file_size: 946004

245.1.0.b: On the stability of jetstreams

last_modified: 2023-06-20 16:00:00

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

license_type: by-nc

No entro en nada

No entro en nada 2

Artículo

On stability of jetstreams

Wiin Nielsen, A.

Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM, publicado en Atmósfera, y cosechado de Revistas UNAM

Licencia de uso

Procedencia del contenido

Entidad o dependencia
Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM
Revista
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Wiin Nielsen, A. (1995). On stability of jetstreams. Atmósfera; Vol. 8 No. 4, 1995. Recuperado de https://repositorio.unam.mx/contenidos/4119840

Descripción del recurso

Autor(es)
Wiin Nielsen, A.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
On stability of jetstreams
Fecha
2009-10-05
Resumen
The quasi-geostrophic, baroclinic stability problem is solved using vertical structure functions corresponding to a vertical variation of the static stability parameter which is inversely proportional to the square of the pressure. Due to this assumption it is necessary to apply the upper boundary condition at a pressure level different from the outer limit of the atmosphere. While this technique has been used earlier, the emphasis in this paper is on the stability of jet profiles. Various jet-like profiles of the zonal wind are defined mathematically, and they are used to investigate how the stability depends on the maximum wind, the position of the jet maximum, the sharpness of the jet, and also the position of the upper boundary. A comparison is made with the stability of the advective model for which the stability may be obtained analytically. From the general, quasi-geostrophic model it is found that a short-wave cut-off exists, while instability exists for all wavelenghts larger than the cut-off wavelength, i.e. no long-wave cut-off exists. Smaller instabilities occurs when the maximum wind is around 300 hPa, when the top level is located at 30 hPa, and when the jet profiles are well rounded. A wind profile with "stratospheric easterlies" has about the same stability for Rossby waves of a few thousand kilometers as a profile with westerlies at all levels. However, for very long waves the profile with easterlies is more unstable.
Idioma
eng
ISSN
ISSN electrónico: 2395-8812; ISSN impreso: 0187-6236

Enlaces