Snow height on sea ice and sea ice drift from autonomous measurements from buoy 2018S75, deployed during AKADEMIK TRYOSHNIKOV cruise TRANSDRIFT XXIV / TICE

Snow height was measured by the Snow Depth Buoy 2018S75, an autonomous platform, drifting on Arctic sea ice, deployed during AKADEMIK TRYOSHNIKOV cruise TRANSDRIFT XXIV (TICE). The resulting time series describes the evolution of snow depth as a function of place and time between 13 September 2018 a...

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Bibliographic Details
Main Authors: Nicolaus, Marcel, Belter, Hans Jakob, Hummel, Simon, Hansen, Miriam Lea Sarah, Rabe, Benjamin, Tippenhauer, Sandra, Vredenborg, Myriel, Hoppmann, Mario
Format: Dataset
Language:English
Published: PANGAEA 2021
Subjects:
2018S75
Akademik Tryoshnikov
AT2018
TICE
NABOS
autonomous platform
AWI_SeaIce
buoy
BUOY_SNOW
Current sea ice maps for Arctic and Antarctic
DATE/TIME
drift
LATITUDE
LONGITUDE
meereisportal.de
MIDO
Multidisciplinary Ice-based Distributed Observatory
Pressure
atmospheric
Sea Ice Physics @ AWI
Snow buoy
snow depth
Snow height
Temperature
air
technical
Transdrift-XXIV
WMO-ID 2501647
Antarc*
Antarctic
Sea ice
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.927561
https://doi.org/10.1594/PANGAEA.927561
Description
Summary:Snow height was measured by the Snow Depth Buoy 2018S75, an autonomous platform, drifting on Arctic sea ice, deployed during AKADEMIK TRYOSHNIKOV cruise TRANSDRIFT XXIV (TICE). The resulting time series describes the evolution of snow depth as a function of place and time between 13 September 2018 and 15 August 2020 in sample intervals of 1 hour. The Snow Depth Buoy consists of four independent sonar measurements representing the area (approx. 10 m**2) around the buoy. The buoy was installed on multi year ice. In addition to snow depth, geographic position (GPS), barometric pressure, air temperature, and an internal ice temperature were measured. Negative values of snow height occur if surface ablation continues into the sea ice. Thus, these measurements describe the position of the sea ice surface relative to the original snow-ice interface. Differences between single sensors indicate small-scale variability of the snow pack around the buoy. The data set has been processed, including the removal of obvious inconsistencies (missing values). Records without any snow depth may still be used for sea ice drift analyses.

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