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650.#.4.x: Físico Matemáticas y Ciencias de la Tierra

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336.#.#.a: Artículo

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100.1.#.a: Jauregui, Ernesto; Luyando, Elda

524.#.#.a: Jauregui, Ernesto, et al. (1998). Long-term association between pan evaporation and the urban heat island in Mexico City. Atmósfera; Vol. 11 No. 1, 1998. Recuperado de https://repositorio.unam.mx/contenidos/4120331

245.1.0.a: Long-term association between pan evaporation and the urban heat island in Mexico City

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

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

264.#.0.c: 1998

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

653.#.#.a: URBAN PAN EVAPORATION; HEAT ISLAND; TROPICAL URBAN CLIMATE; urban pan evaporation; heat island; tropical urban climate

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: Using a network of 16 urban/suburban and rural pan evaporation (pe) stations in Mexico City and its environs, an attempt is made to assess the comparative evaporative characteristics of different areas in a large city located in an elevated inland valley in the tropics. Significant parallel increases in pan evaporation and heat island intensity have been observed in the central and western portions of Mexico City for the period 1967-88. It is suggested that pan evaporation increase is linked to the observed increase in the intensity of the heat island related to the accelerated urbanization of the capital City. m contrast over the eastern suburbs the establishment of a large (9500 Ha) adjacent revegetation project has apparently influenced pan evaporation to decline in spite of the increasing presence of the heat island. Association of pan evaporation to other climatic elements such as insolation, precipitation and wind velocity is also explored.

773.1.#.t: Atmósfera; Vol. 11 No. 1 (1998)

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

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

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

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245.1.0.b: Long-term association between pan evaporation and the urban heat island in México City

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Artículo

Long-term association between pan evaporation and the urban heat island in Mexico City

Jauregui, Ernesto; Luyando, Elda

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

Jauregui, Ernesto, et al. (1998). Long-term association between pan evaporation and the urban heat island in Mexico City. Atmósfera; Vol. 11 No. 1, 1998. Recuperado de https://repositorio.unam.mx/contenidos/4120331

Descripción del recurso

Autor(es)
Jauregui, Ernesto; Luyando, Elda
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Long-term association between pan evaporation and the urban heat island in Mexico City
Fecha
2009-10-05
Resumen
Using a network of 16 urban/suburban and rural pan evaporation (pe) stations in Mexico City and its environs, an attempt is made to assess the comparative evaporative characteristics of different areas in a large city located in an elevated inland valley in the tropics. Significant parallel increases in pan evaporation and heat island intensity have been observed in the central and western portions of Mexico City for the period 1967-88. It is suggested that pan evaporation increase is linked to the observed increase in the intensity of the heat island related to the accelerated urbanization of the capital City. m contrast over the eastern suburbs the establishment of a large (9500 Ha) adjacent revegetation project has apparently influenced pan evaporation to decline in spite of the increasing presence of the heat island. Association of pan evaporation to other climatic elements such as insolation, precipitation and wind velocity is also explored.
Tema
URBAN PAN EVAPORATION; HEAT ISLAND; TROPICAL URBAN CLIMATE; urban pan evaporation; heat island; tropical urban climate
Idioma
eng
ISSN
ISSN electrónico: 2395-8812; ISSN impreso: 0187-6236

Enlaces