Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R35) Omolon, Russia. 2007-2020.

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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Main Author: Denis Shmelev
Format: Dataset
Language:unknown
Published: Arctic Data Center 2021
Subjects:
Online Access:https://doi.org/10.18739/A2NZ80R32
id dataone:doi:10.18739/A2NZ80R32
record_format openpolar
spelling dataone:doi:10.18739/A2NZ80R32 2024-06-03T18:46:21+00:00 Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R35) Omolon, Russia. 2007-2020. Denis Shmelev Larch forest at the yedoma hill located near the middle reaches of the Kolyma River. Please contact site investigator (D. Shmelev, shmelevdenis@mail.ru) for more information. ENVELOPE(158.0,158.0,68.0,68.0) BEGINDATE: 2007-01-01T00:00:00Z ENDDATE: 2020-01-01T00:00:00Z 2021-01-01T00:00:00Z https://doi.org/10.18739/A2NZ80R32 unknown Arctic Data Center Permafrost 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/A2NZ80R32 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 kolyma river permafrost Arctic Data Center (via DataONE) Kolyma ENVELOPE(161.000,161.000,69.500,69.500) ENVELOPE(158.0,158.0,68.0,68.0)
institution Open Polar
collection Arctic Data Center (via DataONE)
op_collection_id dataone:urn:node:ARCTIC
language unknown
topic Permafrost
Earth Science
Cryosphere
Active Layer
Grid
500 Meters to 1 Kilometer
Probes
Field Survey
Weekly to Monthly
spellingShingle Permafrost
Earth Science
Cryosphere
Active Layer
Grid
500 Meters to 1 Kilometer
Probes
Field Survey
Weekly to Monthly
Denis Shmelev
Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R35) Omolon, Russia. 2007-2020.
topic_facet Permafrost
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 Denis Shmelev
author_facet Denis Shmelev
author_sort Denis Shmelev
title Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R35) Omolon, Russia. 2007-2020.
title_short Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R35) Omolon, Russia. 2007-2020.
title_full Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R35) Omolon, Russia. 2007-2020.
title_fullStr Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R35) Omolon, Russia. 2007-2020.
title_full_unstemmed Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R35) Omolon, Russia. 2007-2020.
title_sort seasonal soil active layer measurements from a circumpolar active layer monitoring (calm) grid, (r35) omolon, russia. 2007-2020.
publisher Arctic Data Center
publishDate 2021
url https://doi.org/10.18739/A2NZ80R32
op_coverage Larch forest at the yedoma hill located near the middle reaches of the Kolyma River. Please contact site investigator (D. Shmelev, shmelevdenis@mail.ru) for more information.
ENVELOPE(158.0,158.0,68.0,68.0)
BEGINDATE: 2007-01-01T00:00:00Z ENDDATE: 2020-01-01T00:00:00Z
long_lat ENVELOPE(161.000,161.000,69.500,69.500)
ENVELOPE(158.0,158.0,68.0,68.0)
geographic Kolyma
geographic_facet Kolyma
genre Active layer monitoring
Global Terrestrial Network for Permafrost
kolyma river
permafrost
genre_facet Active layer monitoring
Global Terrestrial Network for Permafrost
kolyma river
permafrost
op_doi https://doi.org/10.18739/A2NZ80R32
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