Distribution and current status of permafrost in the highest volcano in North America: Citlaltepetl (Pico de Orizaba), Mexico
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 i...
| Autores: | , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2020 |
| País: | México |
| Institución: | Universidad Nacional Autónoma de México |
| Repositorio: | Redalyc-UNAM |
| OAI Identifier: | oai:redalyc.org:56872303004 |
| Acceso en línea: | https://www.redalyc.org/articulo.oa?id=56872303004 https://www.redalyc.org/journal/568/56872303004/ https://www.redalyc.org/journal/568/56872303004/html/ https://www.redalyc.org/journal/568/56872303004/56872303004.epub https://www.redalyc.org/journal/568/56872303004/movil |
| Access Level: | acceso abierto |
| Palabra clave: | Ciencias de la Tierra Permafrost Citlaltepetl Climate Change Air temperature Linear regression |
| Sumario: | 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. |
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