The diurnal evolution of oceanic boundary layer beneath early-frozen landfast ice in Prydz Bay, East Antarctica
The ice–ocean boundary layer parameters are one of the main drivers of sea ice mass balance in the Polar Regions. To investigate the oceanic contribution to the landfast ice evolution, an integrated ocean observation system, including Acoustic Doppler Velocimeter, COMPACT-CTD, and Sea Ice Mass Balan...
Main Authors: | , , , , , |
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Format: | Text |
Language: | English |
Published: |
2022
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-2022-125 https://tc.copernicus.org/preprints/tc-2022-125/ |