Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R9) Cape Rogozhny; Chukotka, Russia. 1994-2020
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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dataone:doi:10.18739/A2W950P63 2024-06-03T18:46:21+00:00 Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R9) Cape Rogozhny; Chukotka, Russia. 1994-2020 Oleg Tregubov The grid “Cape Rogozhny”, 100x100 m, is located on Lower-Anadyr (Nizhneanadyrskaya) Lowland at the northern coast of Onemen bay (64°47¢ North and 176°58¢ East). Relief of the area is hilly plain with altitudes 5 to 30 m above the water level in the Bay. CALM grid is set at the flat hilltop slightly (at 0-3o) inclined southwestward. The surface is represented by typical hummocky-moss tundra. Hummocks are formed of cotton grass (Erioophorum vaginatum) dominating throughout the plain. ENVELOPE(176.0,176.0,64.0,64.0) BEGINDATE: 1994-01-01T00:00:00Z ENDDATE: 2020-01-01T00:00:00Z 2021-01-01T00:00:00Z https://doi.org/10.18739/A2W950P63 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/A2W950P63 2024-06-03T18:17:39Z 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 Anadyr Anadyr' Chukotka Global Terrestrial Network for Permafrost permafrost Tundra Cotton-grass Arctic Data Center (via DataONE) Anadyr ENVELOPE(177.510,177.510,64.734,64.734) Anadyr’ ENVELOPE(176.233,176.233,64.882,64.882) ENVELOPE(176.0,176.0,64.0,64.0) |
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 Oleg Tregubov Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R9) Cape Rogozhny; Chukotka, Russia. 1994-2020 |
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 |
Oleg Tregubov |
author_facet |
Oleg Tregubov |
author_sort |
Oleg Tregubov |
title |
Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R9) Cape Rogozhny; Chukotka, Russia. 1994-2020 |
title_short |
Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R9) Cape Rogozhny; Chukotka, Russia. 1994-2020 |
title_full |
Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R9) Cape Rogozhny; Chukotka, Russia. 1994-2020 |
title_fullStr |
Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R9) Cape Rogozhny; Chukotka, Russia. 1994-2020 |
title_full_unstemmed |
Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R9) Cape Rogozhny; Chukotka, Russia. 1994-2020 |
title_sort |
seasonal soil active layer measurements from a circumpolar active layer monitoring (calm) grid, (r9) cape rogozhny; chukotka, russia. 1994-2020 |
publisher |
Arctic Data Center |
publishDate |
2021 |
url |
https://doi.org/10.18739/A2W950P63 |
op_coverage |
The grid “Cape Rogozhny”, 100x100 m, is located on Lower-Anadyr (Nizhneanadyrskaya) Lowland at the northern coast of Onemen bay (64°47¢ North and 176°58¢ East). Relief of the area is hilly plain with altitudes 5 to 30 m above the water level in the Bay. CALM grid is set at the flat hilltop slightly (at 0-3o) inclined southwestward. The surface is represented by typical hummocky-moss tundra. Hummocks are formed of cotton grass (Erioophorum vaginatum) dominating throughout the plain. ENVELOPE(176.0,176.0,64.0,64.0) BEGINDATE: 1994-01-01T00:00:00Z ENDDATE: 2020-01-01T00:00:00Z |
long_lat |
ENVELOPE(177.510,177.510,64.734,64.734) ENVELOPE(176.233,176.233,64.882,64.882) ENVELOPE(176.0,176.0,64.0,64.0) |
geographic |
Anadyr Anadyr’ |
geographic_facet |
Anadyr Anadyr’ |
genre |
Active layer monitoring Anadyr Anadyr' Chukotka Global Terrestrial Network for Permafrost permafrost Tundra Cotton-grass |
genre_facet |
Active layer monitoring Anadyr Anadyr' Chukotka Global Terrestrial Network for Permafrost permafrost Tundra Cotton-grass |
op_doi |
https://doi.org/10.18739/A2W950P63 |
_version_ |
1800873305520996352 |