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...
Published in: | CATENA |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Elsevier
2017
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Subjects: | |
Online Access: | http://uvadoc.uva.es/handle/10324/40681 https://doi.org/10.1016/j.catena.2016.07.051 |
_version_ | 1829309615781707776 |
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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 |
op_container_end_page | 636 |
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 |