Ground temperatures, landforms and processes in an Atlantic mountain. Cantabrian Mountains (Northern Spain)

Producción Científica Ground temperatures determine significant geomorphological processes in a wet and temperate mountain with a narrow high elevation range belt. Twenty five temperature data loggers were buried at a shallow depth in different locations and altitudes and at specifically cold locati...

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Published in:CATENA
Main Authors: Pisabarro Pérez, Alfonso, Pellitero Ondicol, Ramón, Serrano Cañadas, Enrique, Gómez Lende, Manuel, González Trueba, Juan José
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2017
Subjects:
Online Access:http://uvadoc.uva.es/handle/10324/40681
https://doi.org/10.1016/j.catena.2016.07.051
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author Pisabarro Pérez, Alfonso
Pellitero Ondicol, Ramón
Serrano Cañadas, Enrique
Gómez Lende, Manuel
González Trueba, Juan José
author_facet Pisabarro Pérez, Alfonso
Pellitero Ondicol, Ramón
Serrano Cañadas, Enrique
Gómez Lende, Manuel
González Trueba, Juan José
author_sort Pisabarro Pérez, Alfonso
collection UVaDOC - Repositorio Documental de la Universidad de Valladolid
container_start_page 623
container_title CATENA
container_volume 149
description Producción Científica Ground temperatures determine significant geomorphological processes in a wet and temperate mountain with a narrow high elevation range belt. Twenty five temperature data loggers were buried at a shallow depth in different locations and altitudes and at specifically cold locations at two massifs in the Cantabrian Mountains (North Spain), Picos de Europa and Fuentes Carrionas. This paper analyses the ground thermal regime and associated parameters (e.g. freeze index, duration and depth of freeze, freeze and thaw cycles) and correlates them with active geomorphological processes and landforms. The thermal regime varies in accordance to the topoclimatic conditions, and it was possible to determinate annual phases in function of snow cover behaviour. Main active processes and landforms stop their activity with a large snow cover which thermally protects the ground and in consequence, avoids the freeze and thaw cycles. During this period, the records allow to asseverate the evidence of seasonal freeze grounds in several locations. Permafrost was not discover on the ground at any of the thermometers except one located at the vicinity of a relict ice patch. With the help of geomorphological maps and previous works, we got to establish the relation between geomorphological processes, landforms, snow cover and ground thermal regime. Ministerio de Educación y Formación Profesional (project FPU13/05837) Organismo Autónomo Parques Nacionales - Ministerio de Agricultura y Pesca, Alimentación y Medio Ambiente (project OAPN 053/2010) Ministerio de Economía, Industria y Competitividad (project CGL2015-68144-R) Leverhulme Trust International Network (grant IN-2012-140)
format Article in Journal/Newspaper
genre Ice
permafrost
genre_facet Ice
permafrost
id ftunivvalladolid:oai:uvadoc.uva.es:10324/40681
institution Open Polar
language English
op_collection_id ftunivvalladolid
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op_doi https://doi.org/10.1016/j.catena.2016.07.051
op_relation https://www.sciencedirect.com/science/article/abs/pii/S0341816216303101
https://doi.org/10.1016/j.catena.2016.07.051
http://uvadoc.uva.es/handle/10324/40681
op_rights Attribution-NonCommercial-NoDerivatives 4.0 Internacional
info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by-nc-nd/4.0/
© 2017 Elsevier
publishDate 2017
publisher Elsevier
record_format openpolar
spelling ftunivvalladolid:oai:uvadoc.uva.es:10324/40681 2025-04-13T14:20:30+00:00 Ground temperatures, landforms and processes in an Atlantic mountain. Cantabrian Mountains (Northern Spain) Pisabarro Pérez, Alfonso Pellitero Ondicol, Ramón Serrano Cañadas, Enrique Gómez Lende, Manuel González Trueba, Juan José 2017 application/pdf http://uvadoc.uva.es/handle/10324/40681 https://doi.org/10.1016/j.catena.2016.07.051 eng eng Elsevier https://www.sciencedirect.com/science/article/abs/pii/S0341816216303101 https://doi.org/10.1016/j.catena.2016.07.051 http://uvadoc.uva.es/handle/10324/40681 Attribution-NonCommercial-NoDerivatives 4.0 Internacional info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc-nd/4.0/ © 2017 Elsevier Geomorfología - España - Cordillera Cantábrica Ground thermal regime Régimen térmico de suelos Landforms Accidentes geográficos Geomorphological processes Procesos geomorfológicos info:eu-repo/semantics/article info:eu-repo/semantics/submittedVersion 2017 ftunivvalladolid https://doi.org/10.1016/j.catena.2016.07.051 2025-03-20T12:27:38Z Producción Científica Ground temperatures determine significant geomorphological processes in a wet and temperate mountain with a narrow high elevation range belt. Twenty five temperature data loggers were buried at a shallow depth in different locations and altitudes and at specifically cold locations at two massifs in the Cantabrian Mountains (North Spain), Picos de Europa and Fuentes Carrionas. This paper analyses the ground thermal regime and associated parameters (e.g. freeze index, duration and depth of freeze, freeze and thaw cycles) and correlates them with active geomorphological processes and landforms. The thermal regime varies in accordance to the topoclimatic conditions, and it was possible to determinate annual phases in function of snow cover behaviour. Main active processes and landforms stop their activity with a large snow cover which thermally protects the ground and in consequence, avoids the freeze and thaw cycles. During this period, the records allow to asseverate the evidence of seasonal freeze grounds in several locations. Permafrost was not discover on the ground at any of the thermometers except one located at the vicinity of a relict ice patch. With the help of geomorphological maps and previous works, we got to establish the relation between geomorphological processes, landforms, snow cover and ground thermal regime. Ministerio de Educación y Formación Profesional (project FPU13/05837) Organismo Autónomo Parques Nacionales - Ministerio de Agricultura y Pesca, Alimentación y Medio Ambiente (project OAPN 053/2010) Ministerio de Economía, Industria y Competitividad (project CGL2015-68144-R) Leverhulme Trust International Network (grant IN-2012-140) Article in Journal/Newspaper Ice permafrost UVaDOC - Repositorio Documental de la Universidad de Valladolid CATENA 149 623 636
spellingShingle Geomorfología - España - Cordillera Cantábrica
Ground thermal regime
Régimen térmico de suelos
Landforms
Accidentes geográficos
Geomorphological processes
Procesos geomorfológicos
Pisabarro Pérez, Alfonso
Pellitero Ondicol, Ramón
Serrano Cañadas, Enrique
Gómez Lende, Manuel
González Trueba, Juan José
Ground temperatures, landforms and processes in an Atlantic mountain. Cantabrian Mountains (Northern Spain)
title Ground temperatures, landforms and processes in an Atlantic mountain. Cantabrian Mountains (Northern Spain)
title_full Ground temperatures, landforms and processes in an Atlantic mountain. Cantabrian Mountains (Northern Spain)
title_fullStr Ground temperatures, landforms and processes in an Atlantic mountain. Cantabrian Mountains (Northern Spain)
title_full_unstemmed Ground temperatures, landforms and processes in an Atlantic mountain. Cantabrian Mountains (Northern Spain)
title_short Ground temperatures, landforms and processes in an Atlantic mountain. Cantabrian Mountains (Northern Spain)
title_sort ground temperatures, landforms and processes in an atlantic mountain. cantabrian mountains (northern spain)
topic Geomorfología - España - Cordillera Cantábrica
Ground thermal regime
Régimen térmico de suelos
Landforms
Accidentes geográficos
Geomorphological processes
Procesos geomorfológicos
topic_facet Geomorfología - España - Cordillera Cantábrica
Ground thermal regime
Régimen térmico de suelos
Landforms
Accidentes geográficos
Geomorphological processes
Procesos geomorfológicos
url http://uvadoc.uva.es/handle/10324/40681
https://doi.org/10.1016/j.catena.2016.07.051