Sea ice thickness and snow depth measurements from sea ice mass balance buoy ZS2009 ...

CRREL-type IMB ZS2009 is an autonomous instrument that was installed on the landfast sea ice in Prydz Bay, east Antarctica in July 2009. The buoy was deployed at 69.36°S; 76.42°E, ~3 km from the coast of Station Zhongshan with initial thicknesses of snow and ice of 0.01 and 1.00 m, respectively, on...

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.950180
https://doi.pangaea.de/10.1594/PANGAEA.950180
id ftdatacite:10.1594/pangaea.950180
record_format openpolar
spelling ftdatacite:10.1594/pangaea.950180 2024-09-15T17:46:32+00:00 Sea ice thickness and snow depth measurements from sea ice mass balance buoy ZS2009 ... Li, Na Lei, Ruibo Li, Bingrui 2022 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.950180 https://doi.pangaea.de/10.1594/PANGAEA.950180 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.950178 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 Temperature DATE/TIME Latitude of event Longitude of event Snow depth Sea ice thickness CRREL Ice Mass Balance buoy Dataset dataset 2022 ftdatacite https://doi.org/10.1594/pangaea.95018010.1594/pangaea.950178 2024-07-03T10:20:00Z CRREL-type IMB ZS2009 is an autonomous instrument that was installed on the landfast sea ice in Prydz Bay, east Antarctica in July 2009. The buoy was deployed at 69.36°S; 76.42°E, ~3 km from the coast of Station Zhongshan with initial thicknesses of snow and ice of 0.01 and 1.00 m, respectively, on 10 July 2009. Snow/Ice temperature and mass balance were measured along a chain of thermistors and via acoustic rangefinder sounders. The thermistor chain was 4.5 m long and included 45 sensors with a regular spacing of 10cm. The acoustic sensors were located above and below the ice surface, monitoring the position of the top and bottom surfaces of the ice. The resulting time series describes the evolution of temperature and snow/ice mass balance as a function of time between 10 July and 12 December 2009 in sample intervals of 2 hours. The data from the underwater acoustic sounder were available only from 10 July to 2 August 2009 because of a sensor failure. ... : 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
Temperature
DATE/TIME
Latitude of event
Longitude of event
Snow depth
Sea ice thickness
CRREL Ice Mass Balance buoy
spellingShingle East Antarctica
Landfast ice
Sea ice mass balance
Temperature
DATE/TIME
Latitude of event
Longitude of event
Snow depth
Sea ice thickness
CRREL Ice Mass Balance buoy
Li, Na
Lei, Ruibo
Li, Bingrui
Sea ice thickness and snow depth measurements from sea ice mass balance buoy ZS2009 ...
topic_facet East Antarctica
Landfast ice
Sea ice mass balance
Temperature
DATE/TIME
Latitude of event
Longitude of event
Snow depth
Sea ice thickness
CRREL Ice Mass Balance buoy
description CRREL-type IMB ZS2009 is an autonomous instrument that was installed on the landfast sea ice in Prydz Bay, east Antarctica in July 2009. The buoy was deployed at 69.36°S; 76.42°E, ~3 km from the coast of Station Zhongshan with initial thicknesses of snow and ice of 0.01 and 1.00 m, respectively, on 10 July 2009. Snow/Ice temperature and mass balance were measured along a chain of thermistors and via acoustic rangefinder sounders. The thermistor chain was 4.5 m long and included 45 sensors with a regular spacing of 10cm. The acoustic sensors were located above and below the ice surface, monitoring the position of the top and bottom surfaces of the ice. The resulting time series describes the evolution of temperature and snow/ice mass balance as a function of time between 10 July and 12 December 2009 in sample intervals of 2 hours. The data from the underwater acoustic sounder were available only from 10 July to 2 August 2009 because of a sensor failure. ... : 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 Sea ice thickness and snow depth measurements from sea ice mass balance buoy ZS2009 ...
title_short Sea ice thickness and snow depth measurements from sea ice mass balance buoy ZS2009 ...
title_full Sea ice thickness and snow depth measurements from sea ice mass balance buoy ZS2009 ...
title_fullStr Sea ice thickness and snow depth measurements from sea ice mass balance buoy ZS2009 ...
title_full_unstemmed Sea ice thickness and snow depth measurements from sea ice mass balance buoy ZS2009 ...
title_sort sea ice thickness and snow depth measurements from sea ice mass balance buoy zs2009 ...
publisher PANGAEA
publishDate 2022
url https://dx.doi.org/10.1594/pangaea.950180
https://doi.pangaea.de/10.1594/PANGAEA.950180
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.950178
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.95018010.1594/pangaea.950178
_version_ 1810494773129117696