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856.4.0.u: https://www.revistascca.unam.mx/atm/index.php/atm/article/view/ATM.2014.27.04.03/42481

100.1.#.a: Bravo, José Luis; Azpra, Enrique; Zarraluqui, Víctor; Gay, Carlos

524.#.#.a: Bravo, José Luis, et al. (2014). Some variations of the rainfall in Mexico City from 1954 to 1988 and their statistical significance. Atmósfera; Vol. 27 No. 4, 2014; 367-376. Recuperado de https://repositorio.unam.mx/contenidos/11064

245.1.0.a: Some variations of the rainfall in Mexico City from 1954 to 1988 and their statistical significance

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

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

264.#.0.c: 2014

264.#.1.c: 2015-01-13

653.#.#.a: Rainy season; beginning; end; spatial distribution

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

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041.#.7.h: eng

520.3.#.a: Some characteristics of the precipitation such as the beginning and end of the rainy season, as well as their spatial and temporal distributions are studied. The study included data from 23 climatological stations located in the Federal District for the period 1954-1988. Four variables related to the beginning and end of the rainy season were defined, namely the day of the first and last event with 10 mm of accumulated precipitation and the percentage of accumulated precipitation until Julian days 150 and 275. An analysis of variance and principal components was made with these variables, establishing that rainfall in the Federal District (which includes part of Mexico City and its surrounding areas) responds homogeneously through time to the presence of mesoscale meteorological phenomena. The results indicate that precipitation was lower at the beginning and end of the study period, and higher in the middle; additionally, the rainy season starts from west to east and ends from east to west, causing a longer season in the southwest than in the northeast. The spatial distribution shows the greatest rainfall in the southwest due to the effect of the nearby mountains, and the lowest in the northeast.

773.1.#.t: Atmósfera; Vol. 27 No. 4 (2014); 367-376

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

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300.#.#.a: Páginas: 367-376

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

doi: https://doi.org/10.20937/ATM.2014.27.04.03

handle: 7bd8a4b01e8ea3d4

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

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245.1.0.b: Some variations of the rainfall in Mexico City from 1954 to 1988 and their statistical significance

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

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Artículo

Some variations of the rainfall in Mexico City from 1954 to 1988 and their statistical significance

Bravo, José Luis; Azpra, Enrique; Zarraluqui, Víctor; Gay, Carlos

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

Bravo, José Luis, et al. (2014). Some variations of the rainfall in Mexico City from 1954 to 1988 and their statistical significance. Atmósfera; Vol. 27 No. 4, 2014; 367-376. Recuperado de https://repositorio.unam.mx/contenidos/11064

Descripción del recurso

Autor(es)
Bravo, José Luis; Azpra, Enrique; Zarraluqui, Víctor; Gay, Carlos
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Some variations of the rainfall in Mexico City from 1954 to 1988 and their statistical significance
Fecha
2015-01-13
Resumen
Some characteristics of the precipitation such as the beginning and end of the rainy season, as well as their spatial and temporal distributions are studied. The study included data from 23 climatological stations located in the Federal District for the period 1954-1988. Four variables related to the beginning and end of the rainy season were defined, namely the day of the first and last event with 10 mm of accumulated precipitation and the percentage of accumulated precipitation until Julian days 150 and 275. An analysis of variance and principal components was made with these variables, establishing that rainfall in the Federal District (which includes part of Mexico City and its surrounding areas) responds homogeneously through time to the presence of mesoscale meteorological phenomena. The results indicate that precipitation was lower at the beginning and end of the study period, and higher in the middle; additionally, the rainy season starts from west to east and ends from east to west, causing a longer season in the southwest than in the northeast. The spatial distribution shows the greatest rainfall in the southwest due to the effect of the nearby mountains, and the lowest in the northeast.
Tema
Rainy season; beginning; end; spatial distribution
Idioma
eng
ISSN
ISSN electrónico: 2395-8812; ISSN impreso: 0187-6236

Enlaces