dor_id: 10754

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

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351.#.#.a: Artículos

harvesting_group: RevistasUNAM

270.1.#.p: Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

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270.#.#.d: MX

270.1.#.d: México

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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/ATM.2015.28.02.04/43372

100.1.#.a: Giaccone, Elisa; Colombo, Nicola; Acquaotta, Fiorella; Paro, Luca; Fratianni, Simona

524.#.#.a: Giaccone, Elisa, et al. (2015). CLIMATE VARIATIONS IN A HIGH ALTITUDE ALPINE BASIN AND THEIR EFFECTS ON A GLACIAL ENVIRONMENT (ITALIAN WESTERN ALPS). Atmósfera; Vol. 28 No. 2, 2015; 117-128. Recuperado de https://repositorio.unam.mx/contenidos/10754

245.1.0.a: CLIMATE VARIATIONS IN A HIGH ALTITUDE ALPINE BASIN AND THEIR EFFECTS ON A GLACIAL ENVIRONMENT (ITALIAN WESTERN ALPS)

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

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

264.#.0.c: 2015

264.#.1.c: 2015-03-27

653.#.#.a: Climate change; glacial decline; permafrost; Italian Western Alps

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/ATM.2015.28.02.04

001.#.#.#: 022.oai:ojs.pkp.sfu.ca:article/46008

041.#.7.h: eng

520.3.#.a: The main objective of this study is to evaluate the variations of climatic parameters (temperature, rain and snow) measured by two weather stations (Formazza and Sabbione) that have never been analyzed before, located in a high glacial catchment (the Sabbione basin in the Italian Western Alps). The study highlights the climatic evolution of the Alpine basin during the last 60 years (1950-2012): climate change has caused a pronounced glacial decline originated by ablation augmentation, due mainly to increasing air temperatures and to reduced alimentation caused by a fresh snow decrease. The cross-correlation test shows that temperatures affect the glacial retreat dynamics more than snowfall. Periglacial and permafrost landforms (e.g., patterned grounds, rock glaciers) have been identified within the Little Ice Age (LIA) glacial deposits, which indicate the ongoing transition from glacial/proglacial to periglacial environments. Furthermore, in order to better identify the periglacial domain in the basin, a map of mean annual air temperature (MAAT) was produced based on climatic analysis.

773.1.#.t: Atmósfera; Vol. 28 No. 2 (2015); 117-128

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

300.#.#.a: Páginas: 117-128

264.#.1.b: Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM

doi: https://doi.org/10.20937/ATM.2015.28.02.04

handle: 00ae24f3fe5723a7

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

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

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No entro en nada

No entro en nada 2

Artículo

CLIMATE VARIATIONS IN A HIGH ALTITUDE ALPINE BASIN AND THEIR EFFECTS ON A GLACIAL ENVIRONMENT (ITALIAN WESTERN ALPS)

Giaccone, Elisa; Colombo, Nicola; Acquaotta, Fiorella; Paro, Luca; Fratianni, Simona

Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM, publicado en Atmósfera, y cosechado de Revistas UNAM

Licencia de uso

Procedencia del contenido

Entidad o dependencia
Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM
Revista
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Giaccone, Elisa, et al. (2015). CLIMATE VARIATIONS IN A HIGH ALTITUDE ALPINE BASIN AND THEIR EFFECTS ON A GLACIAL ENVIRONMENT (ITALIAN WESTERN ALPS). Atmósfera; Vol. 28 No. 2, 2015; 117-128. Recuperado de https://repositorio.unam.mx/contenidos/10754

Descripción del recurso

Autor(es)
Giaccone, Elisa; Colombo, Nicola; Acquaotta, Fiorella; Paro, Luca; Fratianni, Simona
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
CLIMATE VARIATIONS IN A HIGH ALTITUDE ALPINE BASIN AND THEIR EFFECTS ON A GLACIAL ENVIRONMENT (ITALIAN WESTERN ALPS)
Fecha
2015-03-27
Resumen
The main objective of this study is to evaluate the variations of climatic parameters (temperature, rain and snow) measured by two weather stations (Formazza and Sabbione) that have never been analyzed before, located in a high glacial catchment (the Sabbione basin in the Italian Western Alps). The study highlights the climatic evolution of the Alpine basin during the last 60 years (1950-2012): climate change has caused a pronounced glacial decline originated by ablation augmentation, due mainly to increasing air temperatures and to reduced alimentation caused by a fresh snow decrease. The cross-correlation test shows that temperatures affect the glacial retreat dynamics more than snowfall. Periglacial and permafrost landforms (e.g., patterned grounds, rock glaciers) have been identified within the Little Ice Age (LIA) glacial deposits, which indicate the ongoing transition from glacial/proglacial to periglacial environments. Furthermore, in order to better identify the periglacial domain in the basin, a map of mean annual air temperature (MAAT) was produced based on climatic analysis.
Tema
Climate change; glacial decline; permafrost; Italian Western Alps
Idioma
eng
ISSN
ISSN electrónico: 2395-8812; ISSN impreso: 0187-6236

Enlaces