dor_id: 4132135

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

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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/457/471

100.1.#.a: Ontiveros-gonzález, Guillermo; Delgado Granados, Hugo; Cortés-ramos, Jorge

524.#.#.a: Ontiveros-gonzález, Guillermo, et al. (2007). Surface Energy Balance model for high-altitude glacial system at 19°N on Glaciar Norte, Mexico. Geofísica Internacional; Vol. 54 Núm. 4: Octubre 1, 2015; 299-314. Recuperado de https://repositorio.unam.mx/contenidos/4132135

245.1.0.a: Surface Energy Balance model for high-altitude glacial system at 19°N on Glaciar Norte, Mexico

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2007

264.#.1.c: 2015-10-01

653.#.#.a: glaciares mexicanos; balance de energía; flujo radiativo; balance radiativo; régimen climatico; Mexican glaciers; energy balance; radiative fluxes; radiative balance; climate regime

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/457

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/457

041.#.7.h: spa

520.3.#.a: The glaciers of Mexico are very small ice bodies located on top of the highest mountains of Mexico. They represent a natural gauge for the climatic changes at the 19°N latitude where no other ice bodies are located around the world. Glaciar Norte glacier on Citlaltépetl Volcano, Mexico, has been retreating in a huge scale, just like other glaciers close to the tropics. Following the current trend of the small glaciers around the world, this glacier will probably disappear before mid-century and with its disappearance an important climatic gauge at this latitude will be gone. Therefore, it is important to identify the factors influencing the retreat and eventual demise of the glaciers. This study focuses on the analysis of the energy fluxes of Glaciar Norte"s surface on the northern flank of Citlaltépetl Volcano, Mexico. From this, it was calculated the energy balance for a single point on the glacier surface. Here, the glacio-meteorological study is described using data from automatic weather stations installed at >5100 masl with the energy balance model developed from this data. The results suggest that net radiation is the main component responsible for the retreat of Mexican glaciers since this parameter controls the energy balance variability. This situation was compared to the energy balance regime present on other tropical and mid-latitude glaciers and it was possible to establish a first approximation of the energy balance regime on glaciers near 19N latitude based on energy balance variability.doi: https://doi.org/10.22201/igeof.00167169p.2015.54.4.1697

773.1.#.t: Geofísica Internacional; Vol. 54 Núm. 4: Octubre 1, 2015; 299-314

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: 299-314

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

doi: https://doi.org/10.22201/igeof.00167169p.2015.54.4.1697

handle: 00bb88509df935d6

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

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file_creation_date: 2017-04-07 16:37:40.0

file_modification_date: 2022-07-05 21:26:09.0

file_creator: Ontiveros-González G.

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245.1.0.b: Surface Energy Balance model for high-altitude glacial system at 19°N on Glaciar Norte, Mexico

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

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Artículo

Surface Energy Balance model for high-altitude glacial system at 19°N on Glaciar Norte, Mexico

Ontiveros-gonzález, Guillermo; Delgado Granados, Hugo; Cortés-ramos, Jorge

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

Ontiveros-gonzález, Guillermo, et al. (2007). Surface Energy Balance model for high-altitude glacial system at 19°N on Glaciar Norte, Mexico. Geofísica Internacional; Vol. 54 Núm. 4: Octubre 1, 2015; 299-314. Recuperado de https://repositorio.unam.mx/contenidos/4132135

Descripción del recurso

Autor(es)
Ontiveros-gonzález, Guillermo; Delgado Granados, Hugo; Cortés-ramos, Jorge
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Surface Energy Balance model for high-altitude glacial system at 19°N on Glaciar Norte, Mexico
Fecha
2015-10-01
Resumen
The glaciers of Mexico are very small ice bodies located on top of the highest mountains of Mexico. They represent a natural gauge for the climatic changes at the 19°N latitude where no other ice bodies are located around the world. Glaciar Norte glacier on Citlaltépetl Volcano, Mexico, has been retreating in a huge scale, just like other glaciers close to the tropics. Following the current trend of the small glaciers around the world, this glacier will probably disappear before mid-century and with its disappearance an important climatic gauge at this latitude will be gone. Therefore, it is important to identify the factors influencing the retreat and eventual demise of the glaciers. This study focuses on the analysis of the energy fluxes of Glaciar Norte"s surface on the northern flank of Citlaltépetl Volcano, Mexico. From this, it was calculated the energy balance for a single point on the glacier surface. Here, the glacio-meteorological study is described using data from automatic weather stations installed at >5100 masl with the energy balance model developed from this data. The results suggest that net radiation is the main component responsible for the retreat of Mexican glaciers since this parameter controls the energy balance variability. This situation was compared to the energy balance regime present on other tropical and mid-latitude glaciers and it was possible to establish a first approximation of the energy balance regime on glaciers near 19N latitude based on energy balance variability.doi: https://doi.org/10.22201/igeof.00167169p.2015.54.4.1697
Tema
glaciares mexicanos; balance de energía; flujo radiativo; balance radiativo; régimen climatico; Mexican glaciers; energy balance; radiative fluxes; radiative balance; climate regime
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces