Albedo of ice types in northeast Greenland's ablation zone, Version 1.0
Ice types, albedos and impurity content are characterized for the ablation zone of the Greenland ice sheet in Kronprinz Christians Land (808 N, 248 W). Along this ice margin the width of the ablation zone is only about 8 km. The emergence and melting of old ice in the ablation zone creates a surface...
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UCAR/NCAR - Earth Observing Laboratory
2011
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ftdatacite:10.5065/d6b27sd8 2023-05-15T13:10:36+02:00 Albedo of ice types in northeast Greenland's ablation zone, Version 1.0 Warren, S. Grenfell, T. Clarke, A. 2011 PDF: Portable Document Format (application/pdf) ASCII: ASCII Text (text/plain) https://dx.doi.org/10.5065/d6b27sd8 https://arcticdata.io/catalog/#view/doi:10.5065/D6B27SD8 en eng UCAR/NCAR - Earth Observing Laboratory http://data.eol.ucar.edu/datafile/nph-get/106.334/2010KPCL_readme.html These data are available to be used subject to the University Corporation for Atmospheric Research ("UCAR") terms and conditions. http://www2.ucar.edu/terms-of-use climatologyMeteorologyAtmosphere Arctic ARCSS NSF Arctic System Science ACADIS Advanced Cooperative Arctic Data and Information Service dataset Dataset scientific data 2011 ftdatacite https://doi.org/10.5065/d6b27sd8 2021-11-05T12:55:41Z Ice types, albedos and impurity content are characterized for the ablation zone of the Greenland ice sheet in Kronprinz Christians Land (808 N, 248 W). Along this ice margin the width of the ablation zone is only about 8 km. The emergence and melting of old ice in the ablation zone creates a surface layer of dust that was originally deposited with snowfall high on the ice sheet. This debris cover is augmented by locally derived wind-blown sediment. Subsequently, the surface dust particles often aggregate together to form centimetre-scale clumps that melt into the ice, creating cryoconite holes. The debris in the cryoconite holes becomes hidden from sunlight, raising the area-averaged albedo relative to surfaces with uniform debris cover. Spectral and broadband albedos were obtained for snow, ice hummocks, debris-covered ice, cryoconite-studded ice and barren tundra surfaces. Broadband ice albedos varied from 0.2 (for ice with heavy loading of uniform debris) to 0.6 (for ice hummocks with cryoconite holes). The cryoconite material itself has albedo 0.1 when wet. Dataset albedo Arctic Greenland Ice Sheet Tundra DataCite Metadata Store (German National Library of Science and Technology) Arctic Greenland |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
climatologyMeteorologyAtmosphere Arctic ARCSS NSF Arctic System Science ACADIS Advanced Cooperative Arctic Data and Information Service |
spellingShingle |
climatologyMeteorologyAtmosphere Arctic ARCSS NSF Arctic System Science ACADIS Advanced Cooperative Arctic Data and Information Service Warren, S. Grenfell, T. Clarke, A. Albedo of ice types in northeast Greenland's ablation zone, Version 1.0 |
topic_facet |
climatologyMeteorologyAtmosphere Arctic ARCSS NSF Arctic System Science ACADIS Advanced Cooperative Arctic Data and Information Service |
description |
Ice types, albedos and impurity content are characterized for the ablation zone of the Greenland ice sheet in Kronprinz Christians Land (808 N, 248 W). Along this ice margin the width of the ablation zone is only about 8 km. The emergence and melting of old ice in the ablation zone creates a surface layer of dust that was originally deposited with snowfall high on the ice sheet. This debris cover is augmented by locally derived wind-blown sediment. Subsequently, the surface dust particles often aggregate together to form centimetre-scale clumps that melt into the ice, creating cryoconite holes. The debris in the cryoconite holes becomes hidden from sunlight, raising the area-averaged albedo relative to surfaces with uniform debris cover. Spectral and broadband albedos were obtained for snow, ice hummocks, debris-covered ice, cryoconite-studded ice and barren tundra surfaces. Broadband ice albedos varied from 0.2 (for ice with heavy loading of uniform debris) to 0.6 (for ice hummocks with cryoconite holes). The cryoconite material itself has albedo 0.1 when wet. |
format |
Dataset |
author |
Warren, S. Grenfell, T. Clarke, A. |
author_facet |
Warren, S. Grenfell, T. Clarke, A. |
author_sort |
Warren, S. |
title |
Albedo of ice types in northeast Greenland's ablation zone, Version 1.0 |
title_short |
Albedo of ice types in northeast Greenland's ablation zone, Version 1.0 |
title_full |
Albedo of ice types in northeast Greenland's ablation zone, Version 1.0 |
title_fullStr |
Albedo of ice types in northeast Greenland's ablation zone, Version 1.0 |
title_full_unstemmed |
Albedo of ice types in northeast Greenland's ablation zone, Version 1.0 |
title_sort |
albedo of ice types in northeast greenland's ablation zone, version 1.0 |
publisher |
UCAR/NCAR - Earth Observing Laboratory |
publishDate |
2011 |
url |
https://dx.doi.org/10.5065/d6b27sd8 https://arcticdata.io/catalog/#view/doi:10.5065/D6B27SD8 |
geographic |
Arctic Greenland |
geographic_facet |
Arctic Greenland |
genre |
albedo Arctic Greenland Ice Sheet Tundra |
genre_facet |
albedo Arctic Greenland Ice Sheet Tundra |
op_relation |
http://data.eol.ucar.edu/datafile/nph-get/106.334/2010KPCL_readme.html |
op_rights |
These data are available to be used subject to the University Corporation for Atmospheric Research ("UCAR") terms and conditions. http://www2.ucar.edu/terms-of-use |
op_doi |
https://doi.org/10.5065/d6b27sd8 |
_version_ |
1766235621458706432 |