Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy ZS2013a: 120 s after the heating cycle ...

Temperature and heating-induced temperature differences were measured along a chain of thermistors. SIMBA ZS2013a is an autonomous instrument that was installed on landfast ice in Prydz Bay, East Antarctica, in May 2013. The buoy was deployed at 69.37°S; 76.36°E, ~100 m from the coast of Chinese Sta...

Full description

Bibliographic Details
Main Authors: Li, Na, Lei, Ruibo, Li, Bingrui
Format: Dataset
Language:English
Published: PANGAEA 2022
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.950102
https://doi.pangaea.de/10.1594/PANGAEA.950102
id ftdatacite:10.1594/pangaea.950102
record_format openpolar
spelling ftdatacite:10.1594/pangaea.950102 2024-09-15T17:42:14+00:00 Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy ZS2013a: 120 s after the heating cycle ... Li, Na Lei, Ruibo Li, Bingrui 2022 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.950102 https://doi.pangaea.de/10.1594/PANGAEA.950102 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.950095 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.95010210.1594/pangaea.950095 2024-07-03T10:20:00Z Temperature and heating-induced temperature differences were measured along a chain of thermistors. SIMBA ZS2013a is an autonomous instrument that was installed on landfast ice in Prydz Bay, East Antarctica, in May 2013. The buoy was deployed at 69.37°S; 76.36°E, ~100 m from the coast of Chinese Station Zhongshan with initial thicknesses of snow and ice of 0.02 and 0.69 m, respectively, on 15 May 2013. The thermistor chain was 4.5 m long and included 108 sensors with a regular spacing of 4cm. 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 15 May and 27 November 2013 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
Li, Bingrui
Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy ZS2013a: 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 ZS2013a is an autonomous instrument that was installed on landfast ice in Prydz Bay, East Antarctica, in May 2013. The buoy was deployed at 69.37°S; 76.36°E, ~100 m from the coast of Chinese Station Zhongshan with initial thicknesses of snow and ice of 0.02 and 0.69 m, respectively, on 15 May 2013. The thermistor chain was 4.5 m long and included 108 sensors with a regular spacing of 4cm. 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 15 May and 27 November 2013 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
Li, Bingrui
author_facet Li, Na
Lei, Ruibo
Li, Bingrui
author_sort Li, Na
title Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy ZS2013a: 120 s after the heating cycle ...
title_short Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy ZS2013a: 120 s after the heating cycle ...
title_full Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy ZS2013a: 120 s after the heating cycle ...
title_fullStr Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy ZS2013a: 120 s after the heating cycle ...
title_full_unstemmed Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy ZS2013a: 120 s after the heating cycle ...
title_sort heating induced temperature difference measurements from simba-type sea ice mass balance buoy zs2013a: 120 s after the heating cycle ...
publisher PANGAEA
publishDate 2022
url https://dx.doi.org/10.1594/pangaea.950102
https://doi.pangaea.de/10.1594/PANGAEA.950102
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.950095
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.95010210.1594/pangaea.950095
_version_ 1810488755765641216