Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, R53 Harp, West Siberia 2016-2020
The Circumpolar Active Layer Monitoring (CALM) program represents the only coordinated program providing collection, standardization, open access, and dissemination of active-layer data world-wide. Widespread, systematic changes in the thickness of the active layer could have profound effects on the...
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2021
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dataone:doi:10.18739/A2H41JN8K 2024-06-03T18:46:21+00:00 Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, R53 Harp, West Siberia 2016-2020 Nikolay Shiklomanov Harp grid (R53) is located (66.723483o N, 66.080488o E) in the north of Western Siberia, about 25 km east of the Polar Ural near settlement Harp. The site is situated on a coastal-marine terrace, characterized by loamy soils and underlined by low-temperature, continuous permafrost. ENVELOPE(66.08049,66.08049,66.72348,66.72348) BEGINDATE: 2016-08-05T00:00:00Z ENDDATE: 2020-10-15T00:00:00Z 2021-01-01T00:00:00Z https://doi.org/10.18739/A2H41JN8K unknown Arctic Data Center Earth Science Cryosphere Active Layer Grid 500 Meters to 1 Kilometer Probes Field Survey Weekly to Monthly Dataset 2021 dataone:urn:node:ARCTIC https://doi.org/10.18739/A2H41JN8K 2024-06-03T18:18:12Z The Circumpolar Active Layer Monitoring (CALM) program represents the only coordinated program providing collection, standardization, open access, and dissemination of active-layer data world-wide. Widespread, systematic changes in the thickness of the active layer could have profound effects on the flux of greenhouse gases, on the human infrastructure in cold regions, and on landscape and hydrologic processes. It is therefore critical that observational and analytical procedures continue over decadal periods to assess trends and detect cumulative, long-term changes. This dataset contains active-layer observations conducted by the CALM program since the 1990s, supported by a series of National Science Foundation (NSF) awards. CALM program is an integral part of the Global Terrestrial Network for Permafrost. CALM 2020 data are significantly reduced due to pandemic-related travel restrictions. Available 2020 data are limited in terms of extent, and observations were not as controlled as previous years in terms of measurement timing or method, and therefore should be treated with caution. Dataset Active layer monitoring Global Terrestrial Network for Permafrost permafrost Siberia Arctic Data Center (via DataONE) ENVELOPE(66.08049,66.08049,66.72348,66.72348) |
institution |
Open Polar |
collection |
Arctic Data Center (via DataONE) |
op_collection_id |
dataone:urn:node:ARCTIC |
language |
unknown |
topic |
Earth Science Cryosphere Active Layer Grid 500 Meters to 1 Kilometer Probes Field Survey Weekly to Monthly |
spellingShingle |
Earth Science Cryosphere Active Layer Grid 500 Meters to 1 Kilometer Probes Field Survey Weekly to Monthly Nikolay Shiklomanov Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, R53 Harp, West Siberia 2016-2020 |
topic_facet |
Earth Science Cryosphere Active Layer Grid 500 Meters to 1 Kilometer Probes Field Survey Weekly to Monthly |
description |
The Circumpolar Active Layer Monitoring (CALM) program represents the only coordinated program providing collection, standardization, open access, and dissemination of active-layer data world-wide. Widespread, systematic changes in the thickness of the active layer could have profound effects on the flux of greenhouse gases, on the human infrastructure in cold regions, and on landscape and hydrologic processes. It is therefore critical that observational and analytical procedures continue over decadal periods to assess trends and detect cumulative, long-term changes. This dataset contains active-layer observations conducted by the CALM program since the 1990s, supported by a series of National Science Foundation (NSF) awards. CALM program is an integral part of the Global Terrestrial Network for Permafrost. CALM 2020 data are significantly reduced due to pandemic-related travel restrictions. Available 2020 data are limited in terms of extent, and observations were not as controlled as previous years in terms of measurement timing or method, and therefore should be treated with caution. |
format |
Dataset |
author |
Nikolay Shiklomanov |
author_facet |
Nikolay Shiklomanov |
author_sort |
Nikolay Shiklomanov |
title |
Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, R53 Harp, West Siberia 2016-2020 |
title_short |
Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, R53 Harp, West Siberia 2016-2020 |
title_full |
Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, R53 Harp, West Siberia 2016-2020 |
title_fullStr |
Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, R53 Harp, West Siberia 2016-2020 |
title_full_unstemmed |
Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, R53 Harp, West Siberia 2016-2020 |
title_sort |
seasonal soil active layer measurements from a circumpolar active layer monitoring (calm) grid, r53 harp, west siberia 2016-2020 |
publisher |
Arctic Data Center |
publishDate |
2021 |
url |
https://doi.org/10.18739/A2H41JN8K |
op_coverage |
Harp grid (R53) is located (66.723483o N, 66.080488o E) in the north of Western Siberia, about 25 km east of the Polar Ural near settlement Harp. The site is situated on a coastal-marine terrace, characterized by loamy soils and underlined by low-temperature, continuous permafrost. ENVELOPE(66.08049,66.08049,66.72348,66.72348) BEGINDATE: 2016-08-05T00:00:00Z ENDDATE: 2020-10-15T00:00:00Z |
long_lat |
ENVELOPE(66.08049,66.08049,66.72348,66.72348) |
genre |
Active layer monitoring Global Terrestrial Network for Permafrost permafrost Siberia |
genre_facet |
Active layer monitoring Global Terrestrial Network for Permafrost permafrost Siberia |
op_doi |
https://doi.org/10.18739/A2H41JN8K |
_version_ |
1800872513675198464 |