Snow height on sea ice and sea ice drift from autonomous measurements from buoy 2014S13, deployed during the CryoVEx2014 field campaign

Snow height was measured by the Snow Depth Buoy 2014S13, an autonomous platform, drifting on Arctic sea ice, deployed during the CryoVEx2014 field campaign. The resulting time series describes the evolution of snow height as a function of place and time between 30 Mar 2014 and 20 Jul 2014 in sample...

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Bibliographic Details
Main Authors: Nicolaus, Marcel, Haas, Christian
Format: Dataset
Language:English
Published: PANGAEA 2014
Subjects:
2014S13
Arctic Ocean
AWI_SeaIce
BUOY_SNOW
DATE/TIME
LATITUDE
LONGITUDE
Pressure
atmospheric
Sea Ice Physics @ AWI
Snow buoy
Snow height
relative
Temperature
air
technical
Sea ice
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.839958
https://doi.org/10.1594/PANGAEA.839958
Description
Summary:Snow height was measured by the Snow Depth Buoy 2014S13, an autonomous platform, drifting on Arctic sea ice, deployed during the CryoVEx2014 field campaign. The resulting time series describes the evolution of snow height as a function of place and time between 30 Mar 2014 and 20 Jul 2014 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 height, geographic position (GPS), barometric pressure, air temperature, and ice surface 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 height may still be used for sea ice drift analyses. Note: This data set contains only relative changes in snow height, because no initial readings of absolute snow height are available.

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