1 dataset found
  1. Permafrost and Ground Ice Map of Switzerland

    • zenodo.org
    zip
    Updated Jun 6, 2023
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    Robert Kenner; Robert Kenner (2023). Permafrost and Ground Ice Map of Switzerland [Dataset]. http://doi.org/10.5281/zenodo.1470165
    Explore at:
    zipAvailable download formats
    Dataset updated
    Jun 6, 2023
    Dataset provided by
    Zenodohttp://zenodo.org/
    Authors
    Robert Kenner; Robert Kenner
    License

    Attribution-NonCommercial-NoDerivs 4.0 (CC BY-NC-ND 4.0)https://creativecommons.org/licenses/by-nc-nd/4.0/
    License information was derived automatically

    Area covered
    Switzerland
    Description

    Save the layer file (.lyr) together with the other files (Shapefiles) in a common folder and load the layer file in a GIS or geoviewer application to see the map.

    If your GIS-Application does not support .lyr files you can define the visualization of the map by yourself using the field “indicator” in the shapefiles attribute table. This field contain the numbers -3; -2; -1; 0; 1; 5 and 9 which have the following meaning:

    -3 = permafrost < -3°C

    -2 = permafrost -2 to -3°C

    -1 = permafrost < -1 to -2°C

    0 = permafrost < 0 to -1°C

    1 = Ground temperatures 0 to +1°C (possible patchy permafrost)

    5 = potential ice-rich permafrost

    9= glacier

    The PGIM and legends can also be accessed online at www.slf.ch\pgim

    The shapefile contain a countrywide permafrost distribution map of Switzerland, indicating ground temperatures and ice content. A new representation of ground temperatures is achieved by distinguishing ice-poor and ice-rich permafrost in the modelling process. There is a very strong correlation of ground temperatures with elevation and potential incoming solar radiation in ice-poor and ice-free ground. The distribution of ice-rich permafrost was defined by modelling mass wasting processes and the integration of snow and ice into the ground caused by them. This approach yields a relatively accurate and largely unambiguous map. Permafrost occurrence is represented by two clearly defined classes: Zone 1 representing modelled ground temperatures and zone 2 indicating excess ground ice outside of zone 1. 58% of 92 validation sites could be definitively classified as having permafrost or no permafrost. If only ice-poor or –free ground is considered, this value reaches 90%.

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Share
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TwitterTwitter
Email
Click to copy link
Link copied
Close
Cite
Robert Kenner; Robert Kenner (2023). Permafrost and Ground Ice Map of Switzerland [Dataset]. http://doi.org/10.5281/zenodo.1470165
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Permafrost and Ground Ice Map of Switzerland

Explore at:
3 scholarly articles cite this dataset (View in Google Scholar)
zipAvailable download formats
Dataset updated
Jun 6, 2023
Dataset provided by
Zenodohttp://zenodo.org/
Authors
Robert Kenner; Robert Kenner
License

Attribution-NonCommercial-NoDerivs 4.0 (CC BY-NC-ND 4.0)https://creativecommons.org/licenses/by-nc-nd/4.0/
License information was derived automatically

Area covered
Switzerland
Description

Save the layer file (.lyr) together with the other files (Shapefiles) in a common folder and load the layer file in a GIS or geoviewer application to see the map.

If your GIS-Application does not support .lyr files you can define the visualization of the map by yourself using the field “indicator” in the shapefiles attribute table. This field contain the numbers -3; -2; -1; 0; 1; 5 and 9 which have the following meaning:

-3 = permafrost < -3°C

-2 = permafrost -2 to -3°C

-1 = permafrost < -1 to -2°C

0 = permafrost < 0 to -1°C

1 = Ground temperatures 0 to +1°C (possible patchy permafrost)

5 = potential ice-rich permafrost

9= glacier

The PGIM and legends can also be accessed online at www.slf.ch\pgim

The shapefile contain a countrywide permafrost distribution map of Switzerland, indicating ground temperatures and ice content. A new representation of ground temperatures is achieved by distinguishing ice-poor and ice-rich permafrost in the modelling process. There is a very strong correlation of ground temperatures with elevation and potential incoming solar radiation in ice-poor and ice-free ground. The distribution of ice-rich permafrost was defined by modelling mass wasting processes and the integration of snow and ice into the ground caused by them. This approach yields a relatively accurate and largely unambiguous map. Permafrost occurrence is represented by two clearly defined classes: Zone 1 representing modelled ground temperatures and zone 2 indicating excess ground ice outside of zone 1. 58% of 92 validation sites could be definitively classified as having permafrost or no permafrost. If only ice-poor or –free ground is considered, this value reaches 90%.

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