In situ sea ice temperature and relative conductivity measurements from Microstructure and In situ Salinity and Temperature buoy in Elson Lagoon, October 2017-March 2018
Two Microstructure and In situ Salinity and Temperature (MIST) buoys were deployed in Elson Lagoon in October, 2017. They each consist of two vertical sets of 32 temperature sensors colocated with pairs of exposed wires, between which the electrical impedance of the ice/water in between can be measu...
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2020
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dataone:doi:10.18739/A26W9696T 2024-10-03T18:46:25+00:00 In situ sea ice temperature and relative conductivity measurements from Microstructure and In situ Salinity and Temperature buoy in Elson Lagoon, October 2017-March 2018 Alice Bradley Rachel Obbard Ignatius Rigor Elson Lagoon, Utqiagvik, Alaska ENVELOPE(-156.565,-156.41,71.37,71.35) BEGINDATE: 2017-10-16T00:00:00Z ENDDATE: 2018-03-01T00:00:00Z 2020-01-01T00:00:00Z https://doi.org/10.18739/A26W9696T unknown Arctic Data Center EARTH SCIENCE > CRYOSPHERE > SEA ICE EARTH SCIENCE > CRYOSPHERE > SEA ICE > ICE DEPTH/THICKNESS EARTH SCIENCE > CRYOSPHERE > SEA ICE > ICE GROWTH/MELT EARTH SCIENCE > CRYOSPHERE > SEA ICE > ICE TEMPERATURE EARTH SCIENCE > CRYOSPHERE > SEA ICE > SALINITY Dataset 2020 dataone:urn:node:ARCTIC https://doi.org/10.18739/A26W9696T 2024-10-03T18:16:41Z Two Microstructure and In situ Salinity and Temperature (MIST) buoys were deployed in Elson Lagoon in October, 2017. They each consist of two vertical sets of 32 temperature sensors colocated with pairs of exposed wires, between which the electrical impedance of the ice/water in between can be measured (see Notz, 2005). These sensor pairs are located every 3 centimeters (cm) from slightly (~3 cm) above the water line to ~87 cm below. The buoys were each additionally equipped with air temperature, Global Positioning System (GPS), and x-y tilt sensors. Each sensor is sampled every hour, at which point data was both stored locally and sent back via Iridium short burst data link. The buoys were deployed in open water at the beginning of the ice growth season so that the sea ice grows down around the sensors. The electrical impedance of the water and ice, combined with the temperature, can be used to find solid fraction and bulk salinity of the ice as it grows and evolves over the winter season. These buoys were a new design, using a sensor system that had not been run unattended in the field for long periods of time before. Several channels on the sensors stopped reporting over the course of the season, so missing measurements in this dataset are filled in with "NaN". The only vertical profile that continued making measurements throughout a full ice growth season is the left side of buoy E. This was however an abbreviated season, with the buoy having been run over by an ice floe shortly after deployment and was chipped out of the ice and righted in early December (see Sampling, Study Extent section). Notz, D., Wettlaufer, J.S. and Worster, M.G., 2005. A non-destructive method for measuring the salinity and solid fraction of growing sea ice in situ. Journal of Glaciology, 51(172), pp.159-166. Dataset Sea ice Alaska Arctic Data Center (via DataONE) ENVELOPE(-156.565,-156.41,71.37,71.35) |
institution |
Open Polar |
collection |
Arctic Data Center (via DataONE) |
op_collection_id |
dataone:urn:node:ARCTIC |
language |
unknown |
topic |
EARTH SCIENCE > CRYOSPHERE > SEA ICE EARTH SCIENCE > CRYOSPHERE > SEA ICE > ICE DEPTH/THICKNESS EARTH SCIENCE > CRYOSPHERE > SEA ICE > ICE GROWTH/MELT EARTH SCIENCE > CRYOSPHERE > SEA ICE > ICE TEMPERATURE EARTH SCIENCE > CRYOSPHERE > SEA ICE > SALINITY |
spellingShingle |
EARTH SCIENCE > CRYOSPHERE > SEA ICE EARTH SCIENCE > CRYOSPHERE > SEA ICE > ICE DEPTH/THICKNESS EARTH SCIENCE > CRYOSPHERE > SEA ICE > ICE GROWTH/MELT EARTH SCIENCE > CRYOSPHERE > SEA ICE > ICE TEMPERATURE EARTH SCIENCE > CRYOSPHERE > SEA ICE > SALINITY Alice Bradley Rachel Obbard Ignatius Rigor In situ sea ice temperature and relative conductivity measurements from Microstructure and In situ Salinity and Temperature buoy in Elson Lagoon, October 2017-March 2018 |
topic_facet |
EARTH SCIENCE > CRYOSPHERE > SEA ICE EARTH SCIENCE > CRYOSPHERE > SEA ICE > ICE DEPTH/THICKNESS EARTH SCIENCE > CRYOSPHERE > SEA ICE > ICE GROWTH/MELT EARTH SCIENCE > CRYOSPHERE > SEA ICE > ICE TEMPERATURE EARTH SCIENCE > CRYOSPHERE > SEA ICE > SALINITY |
description |
Two Microstructure and In situ Salinity and Temperature (MIST) buoys were deployed in Elson Lagoon in October, 2017. They each consist of two vertical sets of 32 temperature sensors colocated with pairs of exposed wires, between which the electrical impedance of the ice/water in between can be measured (see Notz, 2005). These sensor pairs are located every 3 centimeters (cm) from slightly (~3 cm) above the water line to ~87 cm below. The buoys were each additionally equipped with air temperature, Global Positioning System (GPS), and x-y tilt sensors. Each sensor is sampled every hour, at which point data was both stored locally and sent back via Iridium short burst data link. The buoys were deployed in open water at the beginning of the ice growth season so that the sea ice grows down around the sensors. The electrical impedance of the water and ice, combined with the temperature, can be used to find solid fraction and bulk salinity of the ice as it grows and evolves over the winter season. These buoys were a new design, using a sensor system that had not been run unattended in the field for long periods of time before. Several channels on the sensors stopped reporting over the course of the season, so missing measurements in this dataset are filled in with "NaN". The only vertical profile that continued making measurements throughout a full ice growth season is the left side of buoy E. This was however an abbreviated season, with the buoy having been run over by an ice floe shortly after deployment and was chipped out of the ice and righted in early December (see Sampling, Study Extent section). Notz, D., Wettlaufer, J.S. and Worster, M.G., 2005. A non-destructive method for measuring the salinity and solid fraction of growing sea ice in situ. Journal of Glaciology, 51(172), pp.159-166. |
format |
Dataset |
author |
Alice Bradley Rachel Obbard Ignatius Rigor |
author_facet |
Alice Bradley Rachel Obbard Ignatius Rigor |
author_sort |
Alice Bradley |
title |
In situ sea ice temperature and relative conductivity measurements from Microstructure and In situ Salinity and Temperature buoy in Elson Lagoon, October 2017-March 2018 |
title_short |
In situ sea ice temperature and relative conductivity measurements from Microstructure and In situ Salinity and Temperature buoy in Elson Lagoon, October 2017-March 2018 |
title_full |
In situ sea ice temperature and relative conductivity measurements from Microstructure and In situ Salinity and Temperature buoy in Elson Lagoon, October 2017-March 2018 |
title_fullStr |
In situ sea ice temperature and relative conductivity measurements from Microstructure and In situ Salinity and Temperature buoy in Elson Lagoon, October 2017-March 2018 |
title_full_unstemmed |
In situ sea ice temperature and relative conductivity measurements from Microstructure and In situ Salinity and Temperature buoy in Elson Lagoon, October 2017-March 2018 |
title_sort |
in situ sea ice temperature and relative conductivity measurements from microstructure and in situ salinity and temperature buoy in elson lagoon, october 2017-march 2018 |
publisher |
Arctic Data Center |
publishDate |
2020 |
url |
https://doi.org/10.18739/A26W9696T |
op_coverage |
Elson Lagoon, Utqiagvik, Alaska ENVELOPE(-156.565,-156.41,71.37,71.35) BEGINDATE: 2017-10-16T00:00:00Z ENDDATE: 2018-03-01T00:00:00Z |
long_lat |
ENVELOPE(-156.565,-156.41,71.37,71.35) |
genre |
Sea ice Alaska |
genre_facet |
Sea ice Alaska |
op_doi |
https://doi.org/10.18739/A26W9696T |
_version_ |
1811928261229281280 |