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

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Main Authors: Li, Na, Lei, Ruibo, Li, Bingrui
Format: Dataset Open Access
Language:en
Published: PANGAEA 2022
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author Li, Na
Lei, Ruibo
Li, Bingrui
author_facet Li, Na
Lei, Ruibo
Li, Bingrui
collection Datos científicos de ciencias marinas y ambientales
contents 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.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_950102
institution PANGAEA
language en
publishDate 2022
publisher PANGAEA
record_format pangaea
spellingShingle 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
DATE/TIME; East Antarctica; Landfast ice; Latitude of event; Longitude of event; SAMS Ice Mass Balance buoy; Sea ice mass balance; SIMBA; Temperature; Temperature, difference; ZS2013a; ZS2013a_SIMBA
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.
title Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy ZS2013a: 120 s after the heating cycle
topic DATE/TIME; East Antarctica; Landfast ice; Latitude of event; Longitude of event; SAMS Ice Mass Balance buoy; Sea ice mass balance; SIMBA; Temperature; Temperature, difference; ZS2013a; ZS2013a_SIMBA
url https://doi.org/10.1594/PANGAEA.950102