Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy 2019T56: 30 s after the heating cycle ...
Temperature rising around the thermistors after a weak heating applied to each sensor daily after 30 s ... : The data set has been processed and contains quality flags for different kinds for erroneous data. Flag values are the sum of individual error codes. The value of 0 refers to no error. Qualit...
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Online Access: | https://dx.doi.org/10.1594/pangaea.940379 https://doi.pangaea.de/10.1594/PANGAEA.940379 |
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ftdatacite:10.1594/pangaea.940379 2024-09-15T17:53:46+00:00 Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy 2019T56: 30 s after the heating cycle ... Lei, Ruibo Cheng, Bin Hoppmann, Mario Haapala, Jari Lan, Musheng 2022 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.940379 https://doi.pangaea.de/10.1594/PANGAEA.940379 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.940360 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Arctic Ocean Heating rise MOSAiC-ICE Sea ice mass balance SIMBA Temperature DATE/TIME LATITUDE LONGITUDE Quality flag, position Temperature, difference SAMS Ice Mass Balance buoy PS122/1 Polarstern Integrated Arctic observation system INTAROS Multidisciplinary drifting Observatory for the Study of Arctic Climate MOSAiC Dataset dataset 2022 ftdatacite https://doi.org/10.1594/pangaea.94037910.1594/pangaea.940360 2024-07-03T10:20:00Z Temperature rising around the thermistors after a weak heating applied to each sensor daily after 30 s ... : The data set has been processed and contains quality flags for different kinds for erroneous data. Flag values are the sum of individual error codes. The value of 0 refers to no error. Quality flag, position: The geographic position is flagged +1 if the drift velocity, as derived from the GPS longitude and latitude, exceeds a threshold of 10 deg latitude or 50 deg longitude per time step; +2 if the position exceeds extreme values, such as longitude > 360 deg; +4 if the position is exactly 0.0. ... Dataset Arctic Ocean Sea ice DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Arctic Ocean Heating rise MOSAiC-ICE Sea ice mass balance SIMBA Temperature DATE/TIME LATITUDE LONGITUDE Quality flag, position Temperature, difference SAMS Ice Mass Balance buoy PS122/1 Polarstern Integrated Arctic observation system INTAROS Multidisciplinary drifting Observatory for the Study of Arctic Climate MOSAiC |
spellingShingle |
Arctic Ocean Heating rise MOSAiC-ICE Sea ice mass balance SIMBA Temperature DATE/TIME LATITUDE LONGITUDE Quality flag, position Temperature, difference SAMS Ice Mass Balance buoy PS122/1 Polarstern Integrated Arctic observation system INTAROS Multidisciplinary drifting Observatory for the Study of Arctic Climate MOSAiC Lei, Ruibo Cheng, Bin Hoppmann, Mario Haapala, Jari Lan, Musheng Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy 2019T56: 30 s after the heating cycle ... |
topic_facet |
Arctic Ocean Heating rise MOSAiC-ICE Sea ice mass balance SIMBA Temperature DATE/TIME LATITUDE LONGITUDE Quality flag, position Temperature, difference SAMS Ice Mass Balance buoy PS122/1 Polarstern Integrated Arctic observation system INTAROS Multidisciplinary drifting Observatory for the Study of Arctic Climate MOSAiC |
description |
Temperature rising around the thermistors after a weak heating applied to each sensor daily after 30 s ... : The data set has been processed and contains quality flags for different kinds for erroneous data. Flag values are the sum of individual error codes. The value of 0 refers to no error. Quality flag, position: The geographic position is flagged +1 if the drift velocity, as derived from the GPS longitude and latitude, exceeds a threshold of 10 deg latitude or 50 deg longitude per time step; +2 if the position exceeds extreme values, such as longitude > 360 deg; +4 if the position is exactly 0.0. ... |
format |
Dataset |
author |
Lei, Ruibo Cheng, Bin Hoppmann, Mario Haapala, Jari Lan, Musheng |
author_facet |
Lei, Ruibo Cheng, Bin Hoppmann, Mario Haapala, Jari Lan, Musheng |
author_sort |
Lei, Ruibo |
title |
Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy 2019T56: 30 s after the heating cycle ... |
title_short |
Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy 2019T56: 30 s after the heating cycle ... |
title_full |
Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy 2019T56: 30 s after the heating cycle ... |
title_fullStr |
Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy 2019T56: 30 s after the heating cycle ... |
title_full_unstemmed |
Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy 2019T56: 30 s after the heating cycle ... |
title_sort |
heating induced temperature difference measurements from simba-type sea ice mass balance buoy 2019t56: 30 s after the heating cycle ... |
publisher |
PANGAEA |
publishDate |
2022 |
url |
https://dx.doi.org/10.1594/pangaea.940379 https://doi.pangaea.de/10.1594/PANGAEA.940379 |
genre |
Arctic Ocean Sea ice |
genre_facet |
Arctic Ocean Sea ice |
op_relation |
https://dx.doi.org/10.1594/pangaea.940360 |
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.94037910.1594/pangaea.940360 |
_version_ |
1810429822272274432 |