Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R11) Mount Dionisya, Chukotka, Russia. 1996-2020

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: Oleg Tregubov
Format: Dataset
Language:unknown
Published: Arctic Data Center 2021
Subjects:
Online Access:https://doi.org/10.18739/A2513TX26
id dataone:doi:10.18739/A2513TX26
record_format openpolar
spelling dataone:doi:10.18739/A2513TX26 2024-06-03T18:46:21+00:00 Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R11) Mount Dionisya, Chukotka, Russia. 1996-2020 Oleg Tregubov Mt. Dionisiya» CALM site (100 ´ 100 m) is situated in Nizhneanadyrskaya Lowland in the bottom of western slope of Mt. Dionisiya (N 64°34¢31², E 177°11¢37²). The site is located 25 km south of Anadyr city and is 35 km from the Cape Rogozhny site. The area belongs to subarctic climatic belt with transitional climate from moderately continental to marine one. According to Anadyr City weather station (25 km NNE from the site) the average annual air temperature is -7,7ºС, average annual precipitations are 312 mm. ENVELOPE(177.0,177.0,64.0,64.0) BEGINDATE: 1996-01-01T00:00:00Z ENDDATE: 2020-01-01T00:00:00Z 2021-01-01T00:00:00Z https://doi.org/10.18739/A2513TX26 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/A2513TX26 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 Anadyr Anadyr' Chukotka Global Terrestrial Network for Permafrost permafrost Subarctic 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(177.0,177.0,64.0,64.0)
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, (R11) Mount Dionisya, Chukotka, Russia. 1996-2020
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, (R11) Mount Dionisya, Chukotka, Russia. 1996-2020
title_short Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R11) Mount Dionisya, Chukotka, Russia. 1996-2020
title_full Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R11) Mount Dionisya, Chukotka, Russia. 1996-2020
title_fullStr Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R11) Mount Dionisya, Chukotka, Russia. 1996-2020
title_full_unstemmed Seasonal soil active layer measurements from a Circumpolar Active Layer monitoring (CALM) grid, (R11) Mount Dionisya, Chukotka, Russia. 1996-2020
title_sort seasonal soil active layer measurements from a circumpolar active layer monitoring (calm) grid, (r11) mount dionisya, chukotka, russia. 1996-2020
publisher Arctic Data Center
publishDate 2021
url https://doi.org/10.18739/A2513TX26
op_coverage Mt. Dionisiya» CALM site (100 ´ 100 m) is situated in Nizhneanadyrskaya Lowland in the bottom of western slope of Mt. Dionisiya (N 64°34¢31², E 177°11¢37²). The site is located 25 km south of Anadyr city and is 35 km from the Cape Rogozhny site. The area belongs to subarctic climatic belt with transitional climate from moderately continental to marine one. According to Anadyr City weather station (25 km NNE from the site) the average annual air temperature is -7,7ºС, average annual precipitations are 312 mm.
ENVELOPE(177.0,177.0,64.0,64.0)
BEGINDATE: 1996-01-01T00:00:00Z 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(177.0,177.0,64.0,64.0)
geographic Anadyr
Anadyr’
geographic_facet Anadyr
Anadyr’
genre Active layer monitoring
Anadyr
Anadyr'
Chukotka
Global Terrestrial Network for Permafrost
permafrost
Subarctic
genre_facet Active layer monitoring
Anadyr
Anadyr'
Chukotka
Global Terrestrial Network for Permafrost
permafrost
Subarctic
op_doi https://doi.org/10.18739/A2513TX26
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