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EGU2015-544.pdf

EGU2015-544.pdf
Preview of EGU2015-544
🔗 Source: meetingorganizer.copernicus.org
📊 Size: 38 KB
📄 Pages: 1 page
⬇️ Downloads: 99

Summary

Soil thermal regime and geomorphogenesis at Fuentes Carrionas massif (Cantabrian Range, NW Iberian Peninsula) were studied using 14 thermometers buried at shallow depths between 2009 and 2012. Results show a permafrost-free mountain range with annual average soil temperatures between 1 and 8°C. Snow pack is a decisive factor in winter temperatures, and its cover patterns differ between southern and northern aspects, impacting geomorphological processes. A clear relation exists between spring snow melt and solifluction or channelized erosion, while snow cover prevents freeze/thaw cycles. The study identified at least 4 different geo-ecological and geomorphological belts and related thermal conditions to geomorphological processes and landform occurrence.

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Description

Soil thermal regime and geomorphogenesis at Fuentes Carrionas massif (Cantabrian Range, NW Iberian Peninsula) were studied using 14 thermometers buried at...

Technical Information

  • File Format: PDF
  • File Size: 38 KB
  • Pages: 1
  • Language: EN
  • Total Downloads: 99
  • Last Updated: 1 week ago

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