dor_id: 4132817

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

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: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/116/112

100.1.#.a: Soto Molina, Víctor Hugo; Delgado-granados, Hugo

524.#.#.a: Soto Molina, Víctor Hugo, et al. (2021). Distribution and current status of permafrost in the highest volcano in North America: Citlaltepetl (Pico de Orizaba), Mexico. Geofísica Internacional; Vol. 59 Núm. 1: Enero 1, 2020; 39-53. Recuperado de https://repositorio.unam.mx/contenidos/4132817

245.1.0.a: Distribution and current status of permafrost in the highest volcano in North America: Citlaltepetl (Pico de Orizaba), Mexico

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2021

264.#.1.c: 2020-01-01

653.#.#.a: Permafrost; Citlaltépetl; Cambio climático; Temperatura del aire; Temperatura del suelo; Regresión lineal; Permafrost; Citlaltepetl; Climate Change; Air temperature; Ground temperature; Linear regression

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/116

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/116

041.#.7.h: spa

520.3.#.a: The occurrence of permafrost in the Citlaltepetl volcano was emphasized and its coverage was updated. Through an empirical and statistical analysis of topo-climatic variables and based on linear regression it was found that the lower limit of continuous permafrost is positioned above 4,880 masl on its northern slope and at 4,963 on the southern slope; on the other hand, discontinuous and isolated patches start at 4,780 and 4,863 meters in the north and south respectively. A high correlation was found between the temperature of the ground profiles and the air temperature at their corresponding altitude. The temperature found in the permafrost classifies it as “warm” permafrost as in most mountains of medium and low latitude and at the same time it is classified as “compromised” and potentially unstable. In spite of the degradation observed from its first estimation during the 1970s, it is estimated that this indicator of climatic change in high mountains will remain at least for a few decades after the Citlaltepetl´s glacier has been extinguished.doi: https://doi.org/10.22201/igeof.00167169p.2020.59.1.2079                      

773.1.#.t: Geofísica Internacional; Vol. 59 Núm. 1: Enero 1, 2020; 39-53

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: 39-53

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

doi: https://doi.org/10.22201/igeof.00167169p.2020.59.1.2079

handle: 0091af4357973a98

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

856.#.0.q: application/pdf

file_creation_date: 2020-01-21 19:57:44.0

file_modification_date: 2022-04-12 02:51:18.0

file_creator: Víctor Hugo Soto Molina

file_name: 1301c464bd78c63f3792f70f70298eedc7f922d7df66a1bf1cd699d41a674a64.pdf

file_pages_number: 15

file_format_version: application/pdf; version=1.4

file_size: 6301409

245.1.0.b: Distribution and current status of permafrost in the highest volcano in North America: Citlaltepetl (Pico de Orizaba), Mexico

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

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

license_type: by-nc-sa

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Artículo

Distribution and current status of permafrost in the highest volcano in North America: Citlaltepetl (Pico de Orizaba), Mexico

Soto Molina, Víctor Hugo; Delgado-granados, Hugo

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

Soto Molina, Víctor Hugo, et al. (2021). Distribution and current status of permafrost in the highest volcano in North America: Citlaltepetl (Pico de Orizaba), Mexico. Geofísica Internacional; Vol. 59 Núm. 1: Enero 1, 2020; 39-53. Recuperado de https://repositorio.unam.mx/contenidos/4132817

Descripción del recurso

Autor(es)
Soto Molina, Víctor Hugo; Delgado-granados, Hugo
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Distribution and current status of permafrost in the highest volcano in North America: Citlaltepetl (Pico de Orizaba), Mexico
Fecha
2020-01-01
Resumen
The occurrence of permafrost in the Citlaltepetl volcano was emphasized and its coverage was updated. Through an empirical and statistical analysis of topo-climatic variables and based on linear regression it was found that the lower limit of continuous permafrost is positioned above 4,880 masl on its northern slope and at 4,963 on the southern slope; on the other hand, discontinuous and isolated patches start at 4,780 and 4,863 meters in the north and south respectively. A high correlation was found between the temperature of the ground profiles and the air temperature at their corresponding altitude. The temperature found in the permafrost classifies it as “warm” permafrost as in most mountains of medium and low latitude and at the same time it is classified as “compromised” and potentially unstable. In spite of the degradation observed from its first estimation during the 1970s, it is estimated that this indicator of climatic change in high mountains will remain at least for a few decades after the Citlaltepetl´s glacier has been extinguished.doi: https://doi.org/10.22201/igeof.00167169p.2020.59.1.2079                      
Tema
Permafrost; Citlaltépetl; Cambio climático; Temperatura del aire; Temperatura del suelo; Regresión lineal; Permafrost; Citlaltepetl; Climate Change; Air temperature; Ground temperature; Linear regression
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces