Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy DS2016: 30 s after the heating cycle ...

Temperature and heating-induced temperature differences were measured along a chain of thermistors. SIMBA DS2016 is an autonomous instrument that was installed on landfast ice in Prydz Bay, East Antarctica, in May 2016. The buoy was deployed at 68.57°S; 77.95°E, ~1 km northwest off Australian Statio...

Full description

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.950036
https://doi.pangaea.de/10.1594/PANGAEA.950036
id ftdatacite:10.1594/pangaea.950036
record_format openpolar
spelling ftdatacite:10.1594/pangaea.950036 2024-09-15T17:47:50+00:00 Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy DS2016: 30 s after the heating cycle ... Li, Na Lei, Ruibo Heil, Petra 2022 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.950036 https://doi.pangaea.de/10.1594/PANGAEA.950036 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.950044 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.95003610.1594/pangaea.950044 2024-07-03T10:20:00Z Temperature and heating-induced temperature differences were measured along a chain of thermistors. SIMBA DS2016 is an autonomous instrument that was installed on landfast ice in Prydz Bay, East Antarctica, in May 2016. The buoy was deployed at 68.57°S; 77.95°E, ~1 km northwest off Australian Station Davis Coast with initial thicknesses of snow and ice of 0.06 and 0.80 m, respectively, on 23 May 2016. The thermistor chain was 5 m long and included 240 sensors with a regular spacing of 2cm. 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 23 May and 27 October 2016 in sample intervals of 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 DS2016: 30 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 DS2016 is an autonomous instrument that was installed on landfast ice in Prydz Bay, East Antarctica, in May 2016. The buoy was deployed at 68.57°S; 77.95°E, ~1 km northwest off Australian Station Davis Coast with initial thicknesses of snow and ice of 0.06 and 0.80 m, respectively, on 23 May 2016. The thermistor chain was 5 m long and included 240 sensors with a regular spacing of 2cm. 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 23 May and 27 October 2016 in sample intervals of 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 DS2016: 30 s after the heating cycle ...
title_short Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy DS2016: 30 s after the heating cycle ...
title_full Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy DS2016: 30 s after the heating cycle ...
title_fullStr Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy DS2016: 30 s after the heating cycle ...
title_full_unstemmed Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy DS2016: 30 s after the heating cycle ...
title_sort heating induced temperature difference measurements from simba-type sea ice mass balance buoy ds2016: 30 s after the heating cycle ...
publisher PANGAEA
publishDate 2022
url https://dx.doi.org/10.1594/pangaea.950036
https://doi.pangaea.de/10.1594/PANGAEA.950036
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.950044
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.95003610.1594/pangaea.950044
_version_ 1810497486397112320