Active Layer Depth MISP (Mobile Instrumented System Platform) and CALM (Circumpolar Active Layer Monitoring) grids in Barrow and Atqasuk, Alaska, 2018
Active layer depth measurements were collected during the 2018 growing season at each Circumpolar Active Layer Monitoring (CALM) grid subset plot (30) and at each Mobile Instrumented System Platform (MISP). Both of these grids are located at Utqiaġvik (formerly Barrow), Alaska as well as in Atqasuk,...
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Arctic Data Center
2019
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Online Access: | https://doi.org/10.18739/A23T9D63W |
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dataone:doi:10.18739/A23T9D63W 2024-06-03T18:46:21+00:00 Active Layer Depth MISP (Mobile Instrumented System Platform) and CALM (Circumpolar Active Layer Monitoring) grids in Barrow and Atqasuk, Alaska, 2018 Sergio Vargas Utqiaġvik, Alaska Atqasuk, Alaska ENVELOPE(-156.6,-156.5,71.5,71.0) BEGINDATE: 2018-06-25T00:00:00Z ENDDATE: 2018-08-13T00:00:00Z 2019-01-01T00:00:00Z https://doi.org/10.18739/A23T9D63W unknown Arctic Data Center EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > ACTIVE LAYER GRID 500 METERS TO 1 KILOMETER IN SITU/LABORATORY INSTRUMENTS > PROBES > PROBES FIELD SURVEY WEEKLY TO MONTHLY geoscientificInformation Dataset 2019 dataone:urn:node:ARCTIC https://doi.org/10.18739/A23T9D63W 2024-06-03T18:12:10Z Active layer depth measurements were collected during the 2018 growing season at each Circumpolar Active Layer Monitoring (CALM) grid subset plot (30) and at each Mobile Instrumented System Platform (MISP). Both of these grids are located at Utqiaġvik (formerly Barrow), Alaska as well as in Atqasuk, Alaska. For CALM measurements, at each plot two active layer depth measurements were acquired, the date, start and end times, and the people present were also recorded. Active layer depth measurements were taken outside of every plot on the northeastern most corner in order to reduce disturbance of vegetation. For MISP measurements, at each grid meter two active layer depth measurement were acquired, the date, start and end times, and the people present were also recorded. Active layer depth measurements were taken on the north side of the grid in order to reduce disturbance of vegetation. These measurements are part of the Arctic Observing Network (AON) - International Tundra Experiment (ITEX) initiative and help to document seasonal changes in surface moisture and structure at high spatial scales. Dataset Active layer monitoring Arctic Barrow Tundra Alaska Arctic Data Center (via DataONE) Arctic ENVELOPE(-156.6,-156.5,71.5,71.0) |
institution |
Open Polar |
collection |
Arctic Data Center (via DataONE) |
op_collection_id |
dataone:urn:node:ARCTIC |
language |
unknown |
topic |
EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > ACTIVE LAYER GRID 500 METERS TO 1 KILOMETER IN SITU/LABORATORY INSTRUMENTS > PROBES > PROBES FIELD SURVEY WEEKLY TO MONTHLY geoscientificInformation |
spellingShingle |
EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > ACTIVE LAYER GRID 500 METERS TO 1 KILOMETER IN SITU/LABORATORY INSTRUMENTS > PROBES > PROBES FIELD SURVEY WEEKLY TO MONTHLY geoscientificInformation Sergio Vargas Active Layer Depth MISP (Mobile Instrumented System Platform) and CALM (Circumpolar Active Layer Monitoring) grids in Barrow and Atqasuk, Alaska, 2018 |
topic_facet |
EARTH SCIENCE > CRYOSPHERE > FROZEN GROUND > ACTIVE LAYER GRID 500 METERS TO 1 KILOMETER IN SITU/LABORATORY INSTRUMENTS > PROBES > PROBES FIELD SURVEY WEEKLY TO MONTHLY geoscientificInformation |
description |
Active layer depth measurements were collected during the 2018 growing season at each Circumpolar Active Layer Monitoring (CALM) grid subset plot (30) and at each Mobile Instrumented System Platform (MISP). Both of these grids are located at Utqiaġvik (formerly Barrow), Alaska as well as in Atqasuk, Alaska. For CALM measurements, at each plot two active layer depth measurements were acquired, the date, start and end times, and the people present were also recorded. Active layer depth measurements were taken outside of every plot on the northeastern most corner in order to reduce disturbance of vegetation. For MISP measurements, at each grid meter two active layer depth measurement were acquired, the date, start and end times, and the people present were also recorded. Active layer depth measurements were taken on the north side of the grid in order to reduce disturbance of vegetation. These measurements are part of the Arctic Observing Network (AON) - International Tundra Experiment (ITEX) initiative and help to document seasonal changes in surface moisture and structure at high spatial scales. |
format |
Dataset |
author |
Sergio Vargas |
author_facet |
Sergio Vargas |
author_sort |
Sergio Vargas |
title |
Active Layer Depth MISP (Mobile Instrumented System Platform) and CALM (Circumpolar Active Layer Monitoring) grids in Barrow and Atqasuk, Alaska, 2018 |
title_short |
Active Layer Depth MISP (Mobile Instrumented System Platform) and CALM (Circumpolar Active Layer Monitoring) grids in Barrow and Atqasuk, Alaska, 2018 |
title_full |
Active Layer Depth MISP (Mobile Instrumented System Platform) and CALM (Circumpolar Active Layer Monitoring) grids in Barrow and Atqasuk, Alaska, 2018 |
title_fullStr |
Active Layer Depth MISP (Mobile Instrumented System Platform) and CALM (Circumpolar Active Layer Monitoring) grids in Barrow and Atqasuk, Alaska, 2018 |
title_full_unstemmed |
Active Layer Depth MISP (Mobile Instrumented System Platform) and CALM (Circumpolar Active Layer Monitoring) grids in Barrow and Atqasuk, Alaska, 2018 |
title_sort |
active layer depth misp (mobile instrumented system platform) and calm (circumpolar active layer monitoring) grids in barrow and atqasuk, alaska, 2018 |
publisher |
Arctic Data Center |
publishDate |
2019 |
url |
https://doi.org/10.18739/A23T9D63W |
op_coverage |
Utqiaġvik, Alaska Atqasuk, Alaska ENVELOPE(-156.6,-156.5,71.5,71.0) BEGINDATE: 2018-06-25T00:00:00Z ENDDATE: 2018-08-13T00:00:00Z |
long_lat |
ENVELOPE(-156.6,-156.5,71.5,71.0) |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Active layer monitoring Arctic Barrow Tundra Alaska |
genre_facet |
Active layer monitoring Arctic Barrow Tundra Alaska |
op_doi |
https://doi.org/10.18739/A23T9D63W |
_version_ |
1800872026952433664 |