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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Bibliographic Details
Main Authors: Miesner, Frederieke, Cable, William L, Boike, Julia
Format: Dataset
Language:English
Published: PANGAEA 2022
Subjects:
Ice
Online Access:https://dx.doi.org/10.1594/pangaea.950782
https://doi.pangaea.de/10.1594/PANGAEA.950782
id ftdatacite:10.1594/pangaea.950782
record_format openpolar
spelling 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
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