Ground thermal regime in the vicinity of relict rock glaciers (Cantabrian Mountains, NW Spain)
DOI:
https://doi.org/10.18055/Finis1375Abstract
Ground temperature data obtained from 2002 to 2007 in sites near relict rock glaciers in the cantabrian mountains, at altitudes between 1500 and 2300 meters is analysed. Snow cover lasted between 3 and 9 months and had a strong influence on the thermal regime. When snow was present, the soil was normally frozen in the first 5 to 10 cm, but daily freeze-thaw cycles were rare. In well developed soils located at sunny faces frost penetration rarely reached more than 10 cm. on the contrary in shady and windy faces with scarce snow cover, frost penetration reached, at least, 40 cm. In persistent snow patches the temperature was stable at 0 ºc, even in relict rock glaciers, where subnival winter air fluxes appear to have been very rare.Downloads
Downloads
How to Cite
Issue
Section
License
-
Authors are responsible for the opinions expressed in the texts submitted to Finisterra.
-
Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.
-
Authors must commit to complying with the “Guidelines for article submission”, on the RCAAP platform.
-
Whenever a text may require amendments based on suggestions made by the Scientific Reviewers and/or the Executive Committee, authors must agree to accept these suggestions and implement the requested changes. If authors disagree with any of the amendments suggested, they will need to provide justifications for each individual case.
-
Reproduction of materials liable to copyright laws has been granted permission in advance.
-
Texts are original, unpublished and have not been submitted to other journals.
License URL CC Attribution-NonCommercial-NoDerivatives (BY-NC-ND)
_(2).jpg)
