Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy DS2015: 120 s after the heating cycle ...

Temperature and heating-induced temperature differences were measured along a chain of thermistors. SIMBA DS2015 is an autonomous instrument that was installed on landfast ice in Prydz Bay, East Antarctica, in May 2015. The buoy was deployed at 68.57°S; 77.93°E, ~1.5 km northwest of Australian Stati...

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Bibliographic Details
Main Authors: Li, Na, Lei, Ruibo, Heil, Petra
Format: Dataset
Language:English
Published: PANGAEA 2022
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.950137
https://doi.pangaea.de/10.1594/PANGAEA.950137
id ftdatacite:10.1594/pangaea.950137
record_format openpolar
spelling ftdatacite:10.1594/pangaea.950137 2024-09-15T17:46:33+00:00 Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy DS2015: 120 s after the heating cycle ... Li, Na Lei, Ruibo Heil, Petra 2022 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.950137 https://doi.pangaea.de/10.1594/PANGAEA.950137 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.950131 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 East Antarctica Landfast ice Sea ice mass balance SIMBA Temperature DATE/TIME Latitude of event Longitude of event Temperature, difference SAMS Ice Mass Balance buoy Dataset dataset 2022 ftdatacite https://doi.org/10.1594/pangaea.95013710.1594/pangaea.950131 2024-07-03T10:20:00Z Temperature and heating-induced temperature differences were measured along a chain of thermistors. SIMBA DS2015 is an autonomous instrument that was installed on landfast ice in Prydz Bay, East Antarctica, in May 2015. The buoy was deployed at 68.57°S; 77.93°E, ~1.5 km northwest of Australian Station Davis with initial thicknesses of snow and ice of 0.10 and 0.88 m, respectively, on 26 May 2015. The thermistor chain was 5 m long and included 240 sensors with a regular spacing of 2cm. Because of a sensor failure, only data from the upper 213 sensors is included here. The resulting time series describes the evolution of temperature and temperature differences after two heating cycles of 30 and 120 s as a function of depth and time between 26 May and 8 December 2015 in sample intervals of 2~6 hours for temperature and 24 hours for temperature differences. ... : The data set has been processed as follows: obvious inconsistencies (missing values) and and unrealistic values have been removed. ... Dataset Antarc* Antarctica East Antarctica Prydz Bay Sea ice DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic East Antarctica
Landfast ice
Sea ice mass balance
SIMBA
Temperature
DATE/TIME
Latitude of event
Longitude of event
Temperature, difference
SAMS Ice Mass Balance buoy
spellingShingle East Antarctica
Landfast ice
Sea ice mass balance
SIMBA
Temperature
DATE/TIME
Latitude of event
Longitude of event
Temperature, difference
SAMS Ice Mass Balance buoy
Li, Na
Lei, Ruibo
Heil, Petra
Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy DS2015: 120 s after the heating cycle ...
topic_facet East Antarctica
Landfast ice
Sea ice mass balance
SIMBA
Temperature
DATE/TIME
Latitude of event
Longitude of event
Temperature, difference
SAMS Ice Mass Balance buoy
description Temperature and heating-induced temperature differences were measured along a chain of thermistors. SIMBA DS2015 is an autonomous instrument that was installed on landfast ice in Prydz Bay, East Antarctica, in May 2015. The buoy was deployed at 68.57°S; 77.93°E, ~1.5 km northwest of Australian Station Davis with initial thicknesses of snow and ice of 0.10 and 0.88 m, respectively, on 26 May 2015. The thermistor chain was 5 m long and included 240 sensors with a regular spacing of 2cm. Because of a sensor failure, only data from the upper 213 sensors is included here. The resulting time series describes the evolution of temperature and temperature differences after two heating cycles of 30 and 120 s as a function of depth and time between 26 May and 8 December 2015 in sample intervals of 2~6 hours for temperature and 24 hours for temperature differences. ... : The data set has been processed as follows: obvious inconsistencies (missing values) and and unrealistic values have been removed. ...
format Dataset
author Li, Na
Lei, Ruibo
Heil, Petra
author_facet Li, Na
Lei, Ruibo
Heil, Petra
author_sort Li, Na
title Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy DS2015: 120 s after the heating cycle ...
title_short Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy DS2015: 120 s after the heating cycle ...
title_full Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy DS2015: 120 s after the heating cycle ...
title_fullStr Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy DS2015: 120 s after the heating cycle ...
title_full_unstemmed Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy DS2015: 120 s after the heating cycle ...
title_sort heating induced temperature difference measurements from simba-type sea ice mass balance buoy ds2015: 120 s after the heating cycle ...
publisher PANGAEA
publishDate 2022
url https://dx.doi.org/10.1594/pangaea.950137
https://doi.pangaea.de/10.1594/PANGAEA.950137
genre Antarc*
Antarctica
East Antarctica
Prydz Bay
Sea ice
genre_facet Antarc*
Antarctica
East Antarctica
Prydz Bay
Sea ice
op_relation https://dx.doi.org/10.1594/pangaea.950131
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.95013710.1594/pangaea.950131
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