Soilsurface temperatures in 2 cm depth between summer 2018 and 2019 with iButton-sensor 145 in Churchill, Canada
Soil surface temperatures were collected with help of iButtons along different transects and clusters around Churchill (Canada). The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
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Language: | English |
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PANGAEA
2020
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.915407 https://doi.org/10.1594/PANGAEA.915407 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.915407 2023-05-15T14:53:30+02:00 Soilsurface temperatures in 2 cm depth between summer 2018 and 2019 with iButton-sensor 145 in Churchill, Canada Langer, Moritz Kaiser, Soraya Stuenzi, Simone Maria Schneider von Deimling, Thomas Oehme, Alexander Jacobi, Stephan LATITUDE: 58.184556 * LONGITUDE: -94.145649 * DATE/TIME START: 2018-08-04T11:47:00 * DATE/TIME END: 2019-07-30T07:47:00 * MINIMUM DEPTH, soil: 0.02 m * MAXIMUM DEPTH, soil: 0.02 m 2020-04-23 text/tab-separated-values, 2033 data points https://doi.pangaea.de/10.1594/PANGAEA.915407 https://doi.org/10.1594/PANGAEA.915407 en eng PANGAEA https://doi.org/10.1594/PANGAEA.914327 https://doi.pangaea.de/10.1594/PANGAEA.915407 https://doi.org/10.1594/PANGAEA.915407 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY AWI_Envi AWI_Perma AWI Arctic Land Expedition CA-Land_2019_Churchill Churchill_2019 Churchill Canada Churchill-iButton145 DATE/TIME DEPTH soil ibuttons iButton sensor MULT Multiple investigations Permafrost Research PermaRisk Polar Terrestrial Environmental Systems @ AWI Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic soil surface temperature Temperature Dataset 2020 ftpangaea https://doi.org/10.1594/PANGAEA.915407 https://doi.org/10.1594/PANGAEA.914327 2023-01-20T10:02:42Z Soil surface temperatures were collected with help of iButtons along different transects and clusters around Churchill (Canada). The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment. Dataset Arctic permafrost PANGAEA - Data Publisher for Earth & Environmental Science Arctic Canada ENVELOPE(-94.145649,-94.145649,58.184556,58.184556) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
AWI_Envi AWI_Perma AWI Arctic Land Expedition CA-Land_2019_Churchill Churchill_2019 Churchill Canada Churchill-iButton145 DATE/TIME DEPTH soil ibuttons iButton sensor MULT Multiple investigations Permafrost Research PermaRisk Polar Terrestrial Environmental Systems @ AWI Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic soil surface temperature Temperature |
spellingShingle |
AWI_Envi AWI_Perma AWI Arctic Land Expedition CA-Land_2019_Churchill Churchill_2019 Churchill Canada Churchill-iButton145 DATE/TIME DEPTH soil ibuttons iButton sensor MULT Multiple investigations Permafrost Research PermaRisk Polar Terrestrial Environmental Systems @ AWI Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic soil surface temperature Temperature Langer, Moritz Kaiser, Soraya Stuenzi, Simone Maria Schneider von Deimling, Thomas Oehme, Alexander Jacobi, Stephan Soilsurface temperatures in 2 cm depth between summer 2018 and 2019 with iButton-sensor 145 in Churchill, Canada |
topic_facet |
AWI_Envi AWI_Perma AWI Arctic Land Expedition CA-Land_2019_Churchill Churchill_2019 Churchill Canada Churchill-iButton145 DATE/TIME DEPTH soil ibuttons iButton sensor MULT Multiple investigations Permafrost Research PermaRisk Polar Terrestrial Environmental Systems @ AWI Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic soil surface temperature Temperature |
description |
Soil surface temperatures were collected with help of iButtons along different transects and clusters around Churchill (Canada). The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment. |
format |
Dataset |
author |
Langer, Moritz Kaiser, Soraya Stuenzi, Simone Maria Schneider von Deimling, Thomas Oehme, Alexander Jacobi, Stephan |
author_facet |
Langer, Moritz Kaiser, Soraya Stuenzi, Simone Maria Schneider von Deimling, Thomas Oehme, Alexander Jacobi, Stephan |
author_sort |
Langer, Moritz |
title |
Soilsurface temperatures in 2 cm depth between summer 2018 and 2019 with iButton-sensor 145 in Churchill, Canada |
title_short |
Soilsurface temperatures in 2 cm depth between summer 2018 and 2019 with iButton-sensor 145 in Churchill, Canada |
title_full |
Soilsurface temperatures in 2 cm depth between summer 2018 and 2019 with iButton-sensor 145 in Churchill, Canada |
title_fullStr |
Soilsurface temperatures in 2 cm depth between summer 2018 and 2019 with iButton-sensor 145 in Churchill, Canada |
title_full_unstemmed |
Soilsurface temperatures in 2 cm depth between summer 2018 and 2019 with iButton-sensor 145 in Churchill, Canada |
title_sort |
soilsurface temperatures in 2 cm depth between summer 2018 and 2019 with ibutton-sensor 145 in churchill, canada |
publisher |
PANGAEA |
publishDate |
2020 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.915407 https://doi.org/10.1594/PANGAEA.915407 |
op_coverage |
LATITUDE: 58.184556 * LONGITUDE: -94.145649 * DATE/TIME START: 2018-08-04T11:47:00 * DATE/TIME END: 2019-07-30T07:47:00 * MINIMUM DEPTH, soil: 0.02 m * MAXIMUM DEPTH, soil: 0.02 m |
long_lat |
ENVELOPE(-94.145649,-94.145649,58.184556,58.184556) |
geographic |
Arctic Canada |
geographic_facet |
Arctic Canada |
genre |
Arctic permafrost |
genre_facet |
Arctic permafrost |
op_relation |
https://doi.org/10.1594/PANGAEA.914327 https://doi.pangaea.de/10.1594/PANGAEA.915407 https://doi.org/10.1594/PANGAEA.915407 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.915407 https://doi.org/10.1594/PANGAEA.914327 |
_version_ |
1766325089904623616 |