ArcticRIMS: Daily Thaw Depth and Frozen Ground Depth, Based on ERA-40 2-meter
Daily thaw depth and frozen ground depth are calculated using a frozen ground model. Oelke et al. [2004] provide details, while also referring to [Oelke et al., 2003]. Thaw depth and frozen ground are calculated using different initial model settings. In the first case, all soil down to the lower mo...
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Arctic Data Center
2016
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dataone:urn:uuid:c9a7a726-eb5b-4a84-8d43-f4e173dfe20f 2024-06-03T18:46:40+00:00 ArcticRIMS: Daily Thaw Depth and Frozen Ground Depth, Based on ERA-40 2-meter ENVELOPE(-180.0,180.0,90.0,45.0) BEGINDATE: 1970-01-01T00:00:00Z ENDDATE: 2001-12-31T00:00:00Z 2016-02-25T00:00:00Z https://search.dataone.org/view/urn:uuid:c9a7a726-eb5b-4a84-8d43-f4e173dfe20f unknown Arctic Data Center Arctic Land Character. Dataset 2016 dataone:urn:node:ARCTIC 2024-06-03T18:07:04Z Daily thaw depth and frozen ground depth are calculated using a frozen ground model. Oelke et al. [2004] provide details, while also referring to [Oelke et al., 2003]. Thaw depth and frozen ground are calculated using different initial model settings. In the first case, all soil down to the lower model boundary is set to sub-freezing initial temperatures. Thawing during the summer months caused the development of a thawed layer at the top with the thaw depth again decreasing during freeze-up of the thawed layer in fall. Frozen ground depth on the other hand is calculated with soil temperatures at all depths above-freezing at the beginning. Here the frozen depth increased during winter, and spring thawing eventually decreases its value. The data is presented in 24 sub-datasets of different spatial and temporal aggregations. Dataset Arctic Arctic Data Center (via DataONE) Arctic ENVELOPE(-180.0,180.0,90.0,45.0) |
institution |
Open Polar |
collection |
Arctic Data Center (via DataONE) |
op_collection_id |
dataone:urn:node:ARCTIC |
language |
unknown |
topic |
Arctic Land Character. |
spellingShingle |
Arctic Land Character. ArcticRIMS: Daily Thaw Depth and Frozen Ground Depth, Based on ERA-40 2-meter |
topic_facet |
Arctic Land Character. |
description |
Daily thaw depth and frozen ground depth are calculated using a frozen ground model. Oelke et al. [2004] provide details, while also referring to [Oelke et al., 2003]. Thaw depth and frozen ground are calculated using different initial model settings. In the first case, all soil down to the lower model boundary is set to sub-freezing initial temperatures. Thawing during the summer months caused the development of a thawed layer at the top with the thaw depth again decreasing during freeze-up of the thawed layer in fall. Frozen ground depth on the other hand is calculated with soil temperatures at all depths above-freezing at the beginning. Here the frozen depth increased during winter, and spring thawing eventually decreases its value. The data is presented in 24 sub-datasets of different spatial and temporal aggregations. |
format |
Dataset |
title |
ArcticRIMS: Daily Thaw Depth and Frozen Ground Depth, Based on ERA-40 2-meter |
title_short |
ArcticRIMS: Daily Thaw Depth and Frozen Ground Depth, Based on ERA-40 2-meter |
title_full |
ArcticRIMS: Daily Thaw Depth and Frozen Ground Depth, Based on ERA-40 2-meter |
title_fullStr |
ArcticRIMS: Daily Thaw Depth and Frozen Ground Depth, Based on ERA-40 2-meter |
title_full_unstemmed |
ArcticRIMS: Daily Thaw Depth and Frozen Ground Depth, Based on ERA-40 2-meter |
title_sort |
arcticrims: daily thaw depth and frozen ground depth, based on era-40 2-meter |
publisher |
Arctic Data Center |
publishDate |
2016 |
url |
https://search.dataone.org/view/urn:uuid:c9a7a726-eb5b-4a84-8d43-f4e173dfe20f |
op_coverage |
ENVELOPE(-180.0,180.0,90.0,45.0) BEGINDATE: 1970-01-01T00:00:00Z ENDDATE: 2001-12-31T00:00:00Z |
long_lat |
ENVELOPE(-180.0,180.0,90.0,45.0) |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
_version_ |
1800869543038418944 |