dor_id: 4132200

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/1483/1601

100.1.#.a: Galindo, I.; Chávez, A.

524.#.#.a: Galindo, I., et al. (1978). Thermal and radiational aspects of the christmas eve 1977 air pollution episode in Mexico City.. Geofísica Internacional; Vol. 17 Núm. 1: Enero 1, 1978; 71-82. Recuperado de https://repositorio.unam.mx/contenidos/4132200

245.1.0.a: Thermal and radiational aspects of the christmas eve 1977 air pollution episode in Mexico City.

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1978

264.#.1.c: 1978-01-01

653.#.#.a: Balance térmico; Radiación; Contaminación; Aire; Ciudad de México; Thermal balance; Radiation; Pollution; Air; Mexico City

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/1483

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1483

041.#.7.h: spa

520.3.#.a: During the night of Dec. 24, 1977, thousands of rubber tires were burned in the streets of Mexico City. The additional tropospheric load of particulate and gaseous matter together with meteorological conditions of stability produced a severe episode of air pollution perturbing the heat balance. On Dec. 2.5 between 0700 and 1400 hours True Solar Time (TST), horizontal visibility was reduced to less that I km, reaching its minimum < 0.1 km between 1200-1400 hours TST. Morning mixing height was 90 m with average wind velocity of 1 m sec-1. The thermal effects of the atmospheric aerosol layer produced warming at night of 2-3°C (greenhouse effect). During the day, on the contrary it was cooler by l.5°C. Duration of sunshine was reduced 1 hour. Atmospheric turbidity reached very high values. Total downward radiation was diminished by 26.8%. The ratio diffuse direct radiation " ·as inverted indicating that much of the incoming radiation was diffused in the aerosol layer. The combined action of the absorption and backscattering processes of the additional aerosol layer seems to be the responsible of the diurnal air cooling at the surface; Both effects are separately analyse on the thermal balance. Backscattering is similar to the one produced from a cloud layer. Using the Yamamoto and Tanaka model, one estimates that global albedo may be increased from 0.15 to 0.30. The above described radiative effects may be responsible for the observed diurnal cooling.

773.1.#.t: Geofísica Internacional; Vol. 17 Núm. 1: Enero 1, 1978; 71-82

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: 71-82

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

doi: https://doi.org/10.22201/igeof.00167169p.1978.17.1.976

handle: 55615fa745933a8f

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

856.#.0.q: application/pdf

file_creation_date: 2008-06-26 23:01:21.0

file_modification_date: 2023-02-01 18:12:38.0

file_creator: Galindo, I.

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245.1.0.b: Thermal and radiational aspects of the christmas eve 1977 air pollution episode in Mexico City.

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

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

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Artículo

Thermal and radiational aspects of the christmas eve 1977 air pollution episode in Mexico City.

Galindo, I.; Chávez, A.

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

Galindo, I., et al. (1978). Thermal and radiational aspects of the christmas eve 1977 air pollution episode in Mexico City.. Geofísica Internacional; Vol. 17 Núm. 1: Enero 1, 1978; 71-82. Recuperado de https://repositorio.unam.mx/contenidos/4132200

Descripción del recurso

Autor(es)
Galindo, I.; Chávez, A.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Thermal and radiational aspects of the christmas eve 1977 air pollution episode in Mexico City.
Fecha
1978-01-01
Resumen
During the night of Dec. 24, 1977, thousands of rubber tires were burned in the streets of Mexico City. The additional tropospheric load of particulate and gaseous matter together with meteorological conditions of stability produced a severe episode of air pollution perturbing the heat balance. On Dec. 2.5 between 0700 and 1400 hours True Solar Time (TST), horizontal visibility was reduced to less that I km, reaching its minimum < 0.1 km between 1200-1400 hours TST. Morning mixing height was 90 m with average wind velocity of 1 m sec-1. The thermal effects of the atmospheric aerosol layer produced warming at night of 2-3°C (greenhouse effect). During the day, on the contrary it was cooler by l.5°C. Duration of sunshine was reduced 1 hour. Atmospheric turbidity reached very high values. Total downward radiation was diminished by 26.8%. The ratio diffuse direct radiation " ·as inverted indicating that much of the incoming radiation was diffused in the aerosol layer. The combined action of the absorption and backscattering processes of the additional aerosol layer seems to be the responsible of the diurnal air cooling at the surface; Both effects are separately analyse on the thermal balance. Backscattering is similar to the one produced from a cloud layer. Using the Yamamoto and Tanaka model, one estimates that global albedo may be increased from 0.15 to 0.30. The above described radiative effects may be responsible for the observed diurnal cooling.
Tema
Balance térmico; Radiación; Contaminación; Aire; Ciudad de México; Thermal balance; Radiation; Pollution; Air; Mexico City
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces