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Main Authors: Hartmann, Jörg, Haas, Christian, Hendricks, Stefan, Krumpen, Thomas
Format: Dataset Open Access
Language:en
Published: PANGAEA 2024
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Online Access:https://doi.org/10.1594/PANGAEA.970895
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author Hartmann, Jörg
Haas, Christian
Hendricks, Stefan
Krumpen, Thomas
author_facet Hartmann, Jörg
Haas, Christian
Hendricks, Stefan
Krumpen, Thomas
collection Datos científicos de ciencias marinas y ambientales
contents Sea ice surface roughness data were obtained during the REFLEX campaign in Mar, 1993 with a Single Beam Laser Altimeter (SBLA) mounted on an/a Airplane (Dornier Do-228, Polar-2) . 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 (IBEO - PS100E) are provided at a sampling rate of 200 Hz. Sensor accuracy is 3 cm with a beam diameter at surface of 11.4 cm. This dataset includes recorded altimeter readings, the derived surface elevation and width/height/spacing of detected pressure ridge sails. Note on data quality: 11.4 cm .
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_970895
institution PANGAEA
language en
publishDate 2024
publisher PANGAEA
record_format pangaea
spellingShingle Laser altimeter data obtained over sea-ice during the REFLEX campaign in Mar, 1993
Hartmann, Jörg
Haas, Christian
Hendricks, Stefan
Krumpen, Thomas
Laser Altimeter; Ridge Height; Ridge Spacing; Ridge Width; Sea Ice Surface Roughness
Sea ice surface roughness data were obtained during the REFLEX campaign in Mar, 1993 with a Single Beam Laser Altimeter (SBLA) mounted on an/a Airplane (Dornier Do-228, Polar-2) . 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 (IBEO - PS100E) are provided at a sampling rate of 200 Hz. Sensor accuracy is 3 cm with a beam diameter at surface of 11.4 cm. This dataset includes recorded altimeter readings, the derived surface elevation and width/height/spacing of detected pressure ridge sails. Note on data quality: 11.4 cm .
title Laser altimeter data obtained over sea-ice during the REFLEX campaign in Mar, 1993
topic Laser Altimeter; Ridge Height; Ridge Spacing; Ridge Width; Sea Ice Surface Roughness
url https://doi.org/10.1594/PANGAEA.970895