Víctor Soto , Carlos M. Welsh-Rodriguez , Rafael Torres-Orozco , Francisco Cordoba-Montiel , Hugo Delgado-Granados
{"title":"墨西哥奥里萨巴皮科 \"北冰川 \"的缩减情况:更新至 2024 年","authors":"Víctor Soto , Carlos M. Welsh-Rodriguez , Rafael Torres-Orozco , Francisco Cordoba-Montiel , Hugo Delgado-Granados","doi":"10.1016/j.jsames.2024.105267","DOIUrl":null,"url":null,"abstract":"<div><div>Given that the “Glaciar Norte” of Pico de Orizaba is one of the last glaciers in Mexico and the only ones located at 19° north latitude in the world, it is crucial to observe its retreat and eventual disappearance to document its spatio-temporal evolution and to identify the factors that drive these changes. We update here the glacier ice areal extent up to May 2024, resulting an area of 0.37 km<sup>2</sup> and a glacier front altitude of 5130 m asl. The air temperature at the lower part of the ice body and within its accumulation zone has increased steadily, whilst precipitation has decreased during the months when solid precipitation commonly occurs in the country. Furthermore, since 2019, portions of the bedrock in the accumulation zone of the glacier have been exposed to solar radiation, resulting in the accumulation of energy. The temperature values obtained on the bare rock surface indicate that, from a thermodynamic perspective, the stored energy is causing the melting of the adjacent ice and snow through due to heat emission. This leads to the conclusion that, in addition to the retreat of the glacier front, ice melting is also occurring in what should be the solid precipitation accumulation area, resulting in an overall more pronounced retreat. The results obtained complement and update the monitoring work that has been carried out before, while also maintaining surveillance for the duration of the glacier's remaining lifespan.</div></div>","PeriodicalId":50047,"journal":{"name":"Journal of South American Earth Sciences","volume":"151 ","pages":"Article 105267"},"PeriodicalIF":1.7000,"publicationDate":"2024-11-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Retraction status of “Glaciar Norte” of Pico de Orizaba, Mexico: Update to 2024\",\"authors\":\"Víctor Soto , Carlos M. Welsh-Rodriguez , Rafael Torres-Orozco , Francisco Cordoba-Montiel , Hugo Delgado-Granados\",\"doi\":\"10.1016/j.jsames.2024.105267\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Given that the “Glaciar Norte” of Pico de Orizaba is one of the last glaciers in Mexico and the only ones located at 19° north latitude in the world, it is crucial to observe its retreat and eventual disappearance to document its spatio-temporal evolution and to identify the factors that drive these changes. We update here the glacier ice areal extent up to May 2024, resulting an area of 0.37 km<sup>2</sup> and a glacier front altitude of 5130 m asl. The air temperature at the lower part of the ice body and within its accumulation zone has increased steadily, whilst precipitation has decreased during the months when solid precipitation commonly occurs in the country. Furthermore, since 2019, portions of the bedrock in the accumulation zone of the glacier have been exposed to solar radiation, resulting in the accumulation of energy. The temperature values obtained on the bare rock surface indicate that, from a thermodynamic perspective, the stored energy is causing the melting of the adjacent ice and snow through due to heat emission. This leads to the conclusion that, in addition to the retreat of the glacier front, ice melting is also occurring in what should be the solid precipitation accumulation area, resulting in an overall more pronounced retreat. The results obtained complement and update the monitoring work that has been carried out before, while also maintaining surveillance for the duration of the glacier's remaining lifespan.</div></div>\",\"PeriodicalId\":50047,\"journal\":{\"name\":\"Journal of South American Earth Sciences\",\"volume\":\"151 \",\"pages\":\"Article 105267\"},\"PeriodicalIF\":1.7000,\"publicationDate\":\"2024-11-17\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of South American Earth Sciences\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0895981124004899\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of South American Earth Sciences","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0895981124004899","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Retraction status of “Glaciar Norte” of Pico de Orizaba, Mexico: Update to 2024
Given that the “Glaciar Norte” of Pico de Orizaba is one of the last glaciers in Mexico and the only ones located at 19° north latitude in the world, it is crucial to observe its retreat and eventual disappearance to document its spatio-temporal evolution and to identify the factors that drive these changes. We update here the glacier ice areal extent up to May 2024, resulting an area of 0.37 km2 and a glacier front altitude of 5130 m asl. The air temperature at the lower part of the ice body and within its accumulation zone has increased steadily, whilst precipitation has decreased during the months when solid precipitation commonly occurs in the country. Furthermore, since 2019, portions of the bedrock in the accumulation zone of the glacier have been exposed to solar radiation, resulting in the accumulation of energy. The temperature values obtained on the bare rock surface indicate that, from a thermodynamic perspective, the stored energy is causing the melting of the adjacent ice and snow through due to heat emission. This leads to the conclusion that, in addition to the retreat of the glacier front, ice melting is also occurring in what should be the solid precipitation accumulation area, resulting in an overall more pronounced retreat. The results obtained complement and update the monitoring work that has been carried out before, while also maintaining surveillance for the duration of the glacier's remaining lifespan.
期刊介绍:
Papers must have a regional appeal and should present work of more than local significance. Research papers dealing with the regional geology of South American cratons and mobile belts, within the following research fields:
-Economic geology, metallogenesis and hydrocarbon genesis and reservoirs.
-Geophysics, geochemistry, volcanology, igneous and metamorphic petrology.
-Tectonics, neo- and seismotectonics and geodynamic modeling.
-Geomorphology, geological hazards, environmental geology, climate change in America and Antarctica, and soil research.
-Stratigraphy, sedimentology, structure and basin evolution.
-Paleontology, paleoecology, paleoclimatology and Quaternary geology.
New developments in already established regional projects and new initiatives dealing with the geology of the continent will be summarized and presented on a regular basis. Short notes, discussions, book reviews and conference and workshop reports will also be included when relevant.