Northern and Mid-Latitude Soil Database, Version 1, R1

The U.S. Department of Agriculture, Agriculture and Agri-Food Canada, the Russian Academy of Agricultural Sciences, the University of Copenhagen Institute of Geography, the European Soil Bureau, the University of Manchester Institute of Landscape Ecology, MTT Agrifood Research Finland, and the Agric...

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Main Author: CRYOSOL WORKING GROUP
Format: Article in Journal/Newspaper
Language:English
Published: ORNL Distributed Active Archive Center 2004
Subjects:
Ice
Online Access:https://dx.doi.org/10.3334/ornldaac/705
http://daac.ornl.gov/cgi-bin/dsviewer.pl?ds_id=705
id ftdatacite:10.3334/ornldaac/705
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spelling ftdatacite:10.3334/ornldaac/705 2023-05-15T16:22:24+02:00 Northern and Mid-Latitude Soil Database, Version 1, R1 CRYOSOL WORKING GROUP 2004 https://dx.doi.org/10.3334/ornldaac/705 http://daac.ornl.gov/cgi-bin/dsviewer.pl?ds_id=705 en eng ORNL Distributed Active Archive Center Collection article Data Files 2004 ftdatacite https://doi.org/10.3334/ornldaac/705 2021-11-05T12:55:41Z The U.S. Department of Agriculture, Agriculture and Agri-Food Canada, the Russian Academy of Agricultural Sciences, the University of Copenhagen Institute of Geography, the European Soil Bureau, the University of Manchester Institute of Landscape Ecology, MTT Agrifood Research Finland, and the Agricultural Research Institute Iceland have shared data and expertise in order to develop the Northern and Mid Latitude Soil Database (Cryosol Working Group, 2001). This database was the source of data for the current product. The spatial coverage of the Northern and Mid Latitude Soil Database is the polar and mid-latitude regions of the northern hemisphere: Alaska, Canada, Conterminous United States, Eurasia (except Italy), Greenland, Iceland, Kazakstan, Mexico, Mongolia, Italy, and Svalbard. The Northern and Mid Latitude Soil Database represents the proportion (percentage) of polygon encompassed by the dominant soil or nonsoil. Soils include turbels, orthels, histels, histosols, mollisols, vertisols, aridisols, andisols, entisols, spodosols, inceptisols (and hapludolls), alfisols (cryalf and udalf), natric great groups, aqu-suborders, glaciers, and rocklands. Also included are data on the circumpolar distribution of gelisols (turbels, orthels, and histels), and the ice content (low, medium, or high) of circumpolar soil materials (from the International Permafrost Association, 1997). The resulting maps show the dominant soil of the spatial polygon unless the polygon is over 90 percent rock or ice. Data are in the U.S. soil classification system and includes the distribution of soil types (%) within a map unit (polygon). Data are available in ESRI shapefile format and include the same attribute values with the exception of Italy, which does not contain distribution values. Article in Journal/Newspaper glacier* glaciers Greenland Ice Iceland International Permafrost Association permafrost Svalbard Alaska DataCite Metadata Store (German National Library of Science and Technology) Canada Greenland Svalbard
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
description The U.S. Department of Agriculture, Agriculture and Agri-Food Canada, the Russian Academy of Agricultural Sciences, the University of Copenhagen Institute of Geography, the European Soil Bureau, the University of Manchester Institute of Landscape Ecology, MTT Agrifood Research Finland, and the Agricultural Research Institute Iceland have shared data and expertise in order to develop the Northern and Mid Latitude Soil Database (Cryosol Working Group, 2001). This database was the source of data for the current product. The spatial coverage of the Northern and Mid Latitude Soil Database is the polar and mid-latitude regions of the northern hemisphere: Alaska, Canada, Conterminous United States, Eurasia (except Italy), Greenland, Iceland, Kazakstan, Mexico, Mongolia, Italy, and Svalbard. The Northern and Mid Latitude Soil Database represents the proportion (percentage) of polygon encompassed by the dominant soil or nonsoil. Soils include turbels, orthels, histels, histosols, mollisols, vertisols, aridisols, andisols, entisols, spodosols, inceptisols (and hapludolls), alfisols (cryalf and udalf), natric great groups, aqu-suborders, glaciers, and rocklands. Also included are data on the circumpolar distribution of gelisols (turbels, orthels, and histels), and the ice content (low, medium, or high) of circumpolar soil materials (from the International Permafrost Association, 1997). The resulting maps show the dominant soil of the spatial polygon unless the polygon is over 90 percent rock or ice. Data are in the U.S. soil classification system and includes the distribution of soil types (%) within a map unit (polygon). Data are available in ESRI shapefile format and include the same attribute values with the exception of Italy, which does not contain distribution values.
format Article in Journal/Newspaper
author CRYOSOL WORKING GROUP
spellingShingle CRYOSOL WORKING GROUP
Northern and Mid-Latitude Soil Database, Version 1, R1
author_facet CRYOSOL WORKING GROUP
author_sort CRYOSOL WORKING GROUP
title Northern and Mid-Latitude Soil Database, Version 1, R1
title_short Northern and Mid-Latitude Soil Database, Version 1, R1
title_full Northern and Mid-Latitude Soil Database, Version 1, R1
title_fullStr Northern and Mid-Latitude Soil Database, Version 1, R1
title_full_unstemmed Northern and Mid-Latitude Soil Database, Version 1, R1
title_sort northern and mid-latitude soil database, version 1, r1
publisher ORNL Distributed Active Archive Center
publishDate 2004
url https://dx.doi.org/10.3334/ornldaac/705
http://daac.ornl.gov/cgi-bin/dsviewer.pl?ds_id=705
geographic Canada
Greenland
Svalbard
geographic_facet Canada
Greenland
Svalbard
genre glacier*
glaciers
Greenland
Ice
Iceland
International Permafrost Association
permafrost
Svalbard
Alaska
genre_facet glacier*
glaciers
Greenland
Ice
Iceland
International Permafrost Association
permafrost
Svalbard
Alaska
op_doi https://doi.org/10.3334/ornldaac/705
_version_ 1766010378727194624