dor_id: 4122358

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/8315/7785

100.1.#.a: Galindo, Ignacio; Castro, S.; Valdés, M.

524.#.#.a: Galindo, Ignacio, et al. (1991). Satellite derived solar irradiance over Mexico. Atmósfera; Vol. 4 No. 3, 1991. Recuperado de https://repositorio.unam.mx/contenidos/4122358

245.1.0.a: Satellite derived solar irradiance over Mexico

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

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

264.#.0.c: 1991

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/8315

001.#.#.#: 022.oai:ojs.pkp.sfu.ca:article/8315

041.#.7.h: eng

520.3.#.a: Global solar irradiance is determined for Mexico from GOES satellite data using, the statistical method of Tarpley (1979). Seven daily digital images taken from GOES satellite over Mexico for the period July 1982 - December 1984 are analysed. Monthly and seasonal means are evaluated by computing monthly averages of the daily totals at a 1º x 1º latitude-longitude grid points. Values of the monthly average daily totals are plotted on a physiographic map of Mexico. Tridimensional surfaces of the distribution of global solar irradiance on Mexico are obtained as a function of latitude and longitude. The standard error of the estimates with respect to ground-truth data is between 3 to 5. The results show clearly the existence of two-well defined patterns of solar irradiance over Mexico from October to April the isopleths are very regular on the monthly maps whereas the latitudinal and longitudinal energy surfaces are uniform in most of the country indicating a weak cloud modulation of the radiation field denoting the so-called "dry season". The maximum value is found during April. The exception is presented at the northern part of Mexico where maximum values are reached during June and July. The other pattern of solar irradiance flux is presented from May to September, coincident with the rainy season and frequent cloudiness; the isopleths show distorsions and nodes particularly over the sierras. September reaches the minimum values; these results indicate modulation of the radiation field by an enhanced clouds amount and atmospheric water vapor absorption. As a consequence of this distribution, it is found a latitudinal solar irradiance gradient such that E/ ≥ 0 occurs during the dry season. The condition E/ ≥ 0 is fulfiled during the wet season. These facts indicate polewards transport of energy during spring and summer through a fine combination of astronomical and geographical parameters, i.e, a longer sunshine duration and absence of clouds during summer at the northern part of the country, whereas the southern part is strongly modulated through the constant presence of clouds reducing the incoming radiation flux. Finally, it is shown that the geographical distribution of the solar radiation flux strongly depends on the irregular relief of the country.

773.1.#.t: Atmósfera; Vol. 4 No. 3 (1991)

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: 2f8e18b0ce1f868a

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

856.#.0.q: application/pdf

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file_modification_date: 2003-06-19 19:04:24.0

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245.1.0.b: Satellite derived solar irradiance over México

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

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

license_type: by-nc

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