Laser altimeter data obtained over sea-ice during the CASIMBO campaign in May, 2018

Sea ice surface roughness data were obtained during the CASIMBO campaign in May, 2018 with a Single Beam Laser Altimeter (SBLA) mounted inside an electromagnetic system (EM-Bird) towed at 10-30 m height above surface by an Airplane (Basler BT-67). A method developed by Hibler (1972) was used to a) i...

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Bibliographic Details
Main Authors: Haas, Christian, Hendricks, Stefan, Krumpen, Thomas
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2024
Subjects:
Laser Altimeter
Ridge Height
Ridge Spacing
Ridge Width
Sea Ice Surface Roughness
Sea ice
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.970400
https://doi.org/10.1594/PANGAEA.970400
Description
Summary:Sea ice surface roughness data were obtained during the CASIMBO campaign in May, 2018 with a Single Beam Laser Altimeter (SBLA) mounted inside an electromagnetic system (EM-Bird) towed at 10-30 m height above surface by an Airplane (Basler BT-67). A method developed by Hibler (1972) was used to a) isolate the surface profile from low-frequency variations associated with the aircraft motion and b) to identify pressure ridge sails. The processing steps are described in https://epic.awi.de/id/eprint/56364/. We applied a ridge detection threshold of 0.6 m, which means that only sails higher 0.6 m are detected. Version and name of the processing routine: Laser_Altimeter_Processing_VS5_06_20.py (vers.5, Feb 22, 2024, https://gitlab.awi.de/sitem/sbla_processing.git). SBLA records (RIEGL - LD90) are provided at a sampling rate of 100 Hz. Sensor accuracy is 5 cm with a beam diameter at surface of 5.8 cm. This dataset includes recorded altimeter readings, the derived surface elevation and width/height/spacing of detected pressure ridge sails. Note on data quality: 5.8 cm .

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