Temperature measurements at Brandallaguna in March 2021 ...
Bottom water temperatures in lakes and the near-shore Arctic Ocean are usually below 4°C. If the water depth is shallow enough, the sea/lake ice freezes to the sea/lake bed and may significantly shift the mean annual temperature below zero. The temperature regime below the water is therefore directl...
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Online Access: | https://dx.doi.org/10.1594/pangaea.950782 https://doi.pangaea.de/10.1594/PANGAEA.950782 |
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ftdatacite:10.1594/pangaea.950782 2023-10-01T03:54:05+02:00 Temperature measurements at Brandallaguna in March 2021 ... Miesner, Frederieke Cable, William L Boike, Julia 2022 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.950782 https://doi.pangaea.de/10.1594/PANGAEA.950782 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.951082 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 active layer Permafrost Svalbard talik Temperature Event label DATE/TIME LATITUDE LONGITUDE ELEVATION Temperature, soil Temperature Lance Modular Observation Solutions for Earth Systems MOSES Permafrost Research AWI_Perma Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn Dataset dataset 2022 ftdatacite https://doi.org/10.1594/pangaea.95078210.1594/pangaea.951082 2023-09-04T15:20:01Z Bottom water temperatures in lakes and the near-shore Arctic Ocean are usually below 4°C. If the water depth is shallow enough, the sea/lake ice freezes to the sea/lake bed and may significantly shift the mean annual temperature below zero. The temperature regime below the water is therefore directly dependent on the water depth and small changes can have ahuge impact.Measurements of the sediment temperature below shallow water bodies, however, are scarce, and single temperature-chains in boreholes are not sufficient to map the spatial variability. As part of the testing phase of the MOSES project, we tested a new temperature lance to measure temperature profiles in lake sediments. The device is a 1.5m steel lancewith 30 sensors at 5cm spacing that can be pushed or hammered into the sediment. The sensors equilibrate to the surrounding sediment or water within 10min, allowing for repeat measurements to cover the spatial variability. During the spring expedition to the Bayelva long-term observatory near Ny ... Dataset Arctic Arctic Ocean Ice permafrost Svalbard Talik DataCite Metadata Store (German National Library of Science and Technology) Arctic Arctic Ocean Svalbard Moses ENVELOPE(-99.183,-99.183,-74.550,-74.550) Talik ENVELOPE(146.601,146.601,59.667,59.667) Bayelva ENVELOPE(11.898,11.898,78.933,78.933) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
active layer Permafrost Svalbard talik Temperature Event label DATE/TIME LATITUDE LONGITUDE ELEVATION Temperature, soil Temperature Lance Modular Observation Solutions for Earth Systems MOSES Permafrost Research AWI_Perma Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn |
spellingShingle |
active layer Permafrost Svalbard talik Temperature Event label DATE/TIME LATITUDE LONGITUDE ELEVATION Temperature, soil Temperature Lance Modular Observation Solutions for Earth Systems MOSES Permafrost Research AWI_Perma Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn Miesner, Frederieke Cable, William L Boike, Julia Temperature measurements at Brandallaguna in March 2021 ... |
topic_facet |
active layer Permafrost Svalbard talik Temperature Event label DATE/TIME LATITUDE LONGITUDE ELEVATION Temperature, soil Temperature Lance Modular Observation Solutions for Earth Systems MOSES Permafrost Research AWI_Perma Permafrost Research Periglacial Dynamics @ AWI AWI_PerDyn |
description |
Bottom water temperatures in lakes and the near-shore Arctic Ocean are usually below 4°C. If the water depth is shallow enough, the sea/lake ice freezes to the sea/lake bed and may significantly shift the mean annual temperature below zero. The temperature regime below the water is therefore directly dependent on the water depth and small changes can have ahuge impact.Measurements of the sediment temperature below shallow water bodies, however, are scarce, and single temperature-chains in boreholes are not sufficient to map the spatial variability. As part of the testing phase of the MOSES project, we tested a new temperature lance to measure temperature profiles in lake sediments. The device is a 1.5m steel lancewith 30 sensors at 5cm spacing that can be pushed or hammered into the sediment. The sensors equilibrate to the surrounding sediment or water within 10min, allowing for repeat measurements to cover the spatial variability. During the spring expedition to the Bayelva long-term observatory near Ny ... |
format |
Dataset |
author |
Miesner, Frederieke Cable, William L Boike, Julia |
author_facet |
Miesner, Frederieke Cable, William L Boike, Julia |
author_sort |
Miesner, Frederieke |
title |
Temperature measurements at Brandallaguna in March 2021 ... |
title_short |
Temperature measurements at Brandallaguna in March 2021 ... |
title_full |
Temperature measurements at Brandallaguna in March 2021 ... |
title_fullStr |
Temperature measurements at Brandallaguna in March 2021 ... |
title_full_unstemmed |
Temperature measurements at Brandallaguna in March 2021 ... |
title_sort |
temperature measurements at brandallaguna in march 2021 ... |
publisher |
PANGAEA |
publishDate |
2022 |
url |
https://dx.doi.org/10.1594/pangaea.950782 https://doi.pangaea.de/10.1594/PANGAEA.950782 |
long_lat |
ENVELOPE(-99.183,-99.183,-74.550,-74.550) ENVELOPE(146.601,146.601,59.667,59.667) ENVELOPE(11.898,11.898,78.933,78.933) |
geographic |
Arctic Arctic Ocean Svalbard Moses Talik Bayelva |
geographic_facet |
Arctic Arctic Ocean Svalbard Moses Talik Bayelva |
genre |
Arctic Arctic Ocean Ice permafrost Svalbard Talik |
genre_facet |
Arctic Arctic Ocean Ice permafrost Svalbard Talik |
op_relation |
https://dx.doi.org/10.1594/pangaea.951082 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.95078210.1594/pangaea.951082 |
_version_ |
1778521400149016576 |