dor_id: 4120422

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/8403/7873

100.1.#.a: Sánchez Santillán, Norma; De La Lanza Espino, Guadalupe

524.#.#.a: Sánchez Santillán, Norma, et al. (1996). The influence of the regional climate in a lagoon in northeastern Mexico. Atmósfera; Vol. 9 No. 3, 1996. Recuperado de https://repositorio.unam.mx/contenidos/4120422

245.1.0.a: The influence of the regional climate in a lagoon in northeastern Mexico

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

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

264.#.0.c: 1996

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/8403

001.#.#.#: 022.oai:ojs.pkp.sfu.ca:article/8403

041.#.7.h: eng

520.3.#.a: The climate affects the Earth at three levels: the relationships between the Sun-Earth energy interaction, the regional climate by the troposphere-Earth relationship (basins) and the local climate by the climatic gradients in endo and exorreic basins. The information on coastal lagoons provided by the last two is scarce and has only been used to define local descriptive frameworks for particular study areas. As a result of this, this paper aims to determine the qualitative and quantitative influence of regional climate on the three local climates defined in an exorreic basin in the northwestern Gulf of Mexico at the level of regional climate. The coastal lagoon of Tampamachoco is located in one of these local climates. The regional climate affects the local climate and defines the seasons in tropical latitudes (the Gulf of Mexico), in accordance with the origin and amount of the rain. The seasons are defined with respect to the rainfall regimes presented in Köppen"s classification, later modified by Garcia (1964), and corroborated with the frequency and intensity of the prevailing winds from 1922 to 1994. These are: 1) the season of northers: from November to February with an average of 222 mm, 2) the dry season: in March and April with an average of 92 mm and 3) the rainy season: from May to October with an average of 1071 mm. Three local climates are defined in response to an orographical factor, as BS1, Aw1 and Aw2. Type Aw1 corresponds to 35% of the basin and is located over the whole coastal plain, type Aw2 makes up 55% over the leeward portion of the Sierra Madre Oriental and the Sierra de Tantima mountain ranges and type BS1 makes up 10% over the windward portion of the Sierra de Tantima. The spatial and temporal differences in the rainfall over the whole basin produce two waterways with multiple sources as a result of the regional climate over the local climate, that affect the shape and hydrological behaviour of the lagoon. The Tuxpam River originates in the most humid climatic area and is a permanent supply to the lagoon with changes in discharge related to the seasons (March 695 m3/s, July 965 m3/s and September 1825 m3/s). The Santiago River, of which the supply is registered only in the rainy season, has its origin in a dry climatic area.

773.1.#.t: Atmósfera; Vol. 9 No. 3 (1996)

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: 00a79ccf074b5d5c

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

856.#.0.q: application/pdf

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file_modification_date: 2001-08-31 21:49:53.0

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245.1.0.b: The influence of the regional climate in a lagoon in northeastern 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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