Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy DS2016: 120 s after the heating cycle

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Autori principali: Li, Na, Lei, Ruibo, Heil, Petra
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 2022
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author Li, Na
Lei, Ruibo
Heil, Petra
author_facet Li, Na
Lei, Ruibo
Heil, Petra
collection Datos científicos de ciencias marinas y ambientales
contents 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.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_950038
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 DS2016: 120 s after the heating cycle
Li, Na
Lei, Ruibo
Heil, Petra
DATE/TIME; DS2016; DS2016_SIMBA; East Antarctica; Landfast ice; Latitude of event; Longitude of event; SAMS Ice Mass Balance buoy; Sea ice mass balance; SIMBA; Temperature; Temperature, difference
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.
title Heating induced temperature difference measurements from SIMBA-type sea ice mass balance buoy DS2016: 120 s after the heating cycle
topic DATE/TIME; DS2016; DS2016_SIMBA; East Antarctica; Landfast ice; Latitude of event; Longitude of event; SAMS Ice Mass Balance buoy; Sea ice mass balance; SIMBA; Temperature; Temperature, difference
url https://doi.org/10.1594/PANGAEA.950038