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- W2188297621 abstract "Information on land use and soil characteristics served as input data and for the initialization of the model, which was then run for 12 years with the meteorological data provided from up to 44 automatic weather stations inside or close to the investigation area as driving variables. Sub-surface temperatures calculated by the model served as indicators for the likelihood of permafrost. According to the sub-surface conditions the areas situated within the potential permafrost realm are further subdivided into different zones. Areas were defined as class ‘permafrost likely’ as long as they are < -1 C for the whole calculation period. Areas which are < -1 C for at least 50 % of the calculation period are classified as ‘permafrost possible’ based on the assumption that a short term warming would not be able to totally remove existing permafrost. Our calculations for the Veneto region show that only a comparatively small fraction of the total investigation area is likely to have permafrost under the given climatic conditions. For the whole Veneto region (21283 km 2 ), a total area of 2.2 km 2 is of class ‘permafrost likely’ and additionally 5.3 km 2 are of class ‘permafrost possible’." @default.
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- W2188297621 date "2012-04-01" @default.
- W2188297621 modified "2023-09-26" @default.
- W2188297621 title "Permafrost simulations in the Dolomites using Alpine3D" @default.
- W2188297621 hasPublicationYear "2012" @default.
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