Parameterization of Centimeter-Scale Sea Ice Surface Roughness Using Terrestrial LiDAR

Microwave scattering from sea ice is partially controlled by the ice surface roughness. In this paper, we propose a technique for calculating 2-D centimeter-scale surface roughness parameters, including the rms height, correlation length, and form of autocorrelation function, from 3-D terrestrial li...

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Published in:IEEE Transactions on Geoscience and Remote Sensing
Main Authors: Landy, Jack, Isleifson, Dustin, Komarov, Alexander, Barber, David
Format: Article in Journal/Newspaper
Language:English
Published: IEEE 2020
Subjects:
Online Access:http://hdl.handle.net/1993/34870
https://doi.org/10.1109/TGRS.2014.2336833
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spelling ftunivmanitoba:oai:mspace.lib.umanitoba.ca:1993/34870 2023-06-18T03:42:56+02:00 Parameterization of Centimeter-Scale Sea Ice Surface Roughness Using Terrestrial LiDAR Landy, Jack Isleifson, Dustin Komarov, Alexander Barber, David 2020-08-18T00:21:08Z application/pdf http://hdl.handle.net/1993/34870 https://doi.org/10.1109/TGRS.2014.2336833 eng eng IEEE Landy, J. C., Isleifson, D., Komarov, A. S., Barber, D. G., 2015. Parameterization of Centimeter-Scale Sea Ice Surface Roughness Using Terrestrial LiDAR. IEEE Trans Geosci Remote Sens. 53(3):1271-1286. https://doi.org/10.1109/TGRS.2014.233683. http://hdl.handle.net/1993/34870 doi:10.1109/TGRS.2014.2336833 open access geophysical measurements ice surface laser applications measurement by laser beam radar scattering sea ice surface roughness surface topography Article 2020 ftunivmanitoba https://doi.org/10.1109/TGRS.2014.233683310.1109/TGRS.2014.233683 2023-06-04T17:45:25Z Microwave scattering from sea ice is partially controlled by the ice surface roughness. In this paper, we propose a technique for calculating 2-D centimeter-scale surface roughness parameters, including the rms height, correlation length, and form of autocorrelation function, from 3-D terrestrial light detection and ranging data. We demonstrate that a single scale of roughness can be extracted from complex sea ice surfaces, incorporating multiple scales of topography, after sophisticated 2-D detrending, and calculate roughness parameters for a wide range of artificial and natural sea ice surface types. The 2-D technique is shown to be considerably more precise than standard 1-D profiling techniques and can therefore characterize surface roughness as a stationary single-scale process, which a 1-D technique typically cannot do. Sea ice surfaces are generally found to have strongly anisotropic correlation lengths, indicating that microwave scattering models for sea ice should include surface spectra that vary as a function of the azimuthal angle of incident radiation. However, our results demonstrate that there is no fundamental relationship between the rms height and correlation length for sea ice surfaces if the sampling area is above a threshold minimum size. Article in Journal/Newspaper Sea ice MSpace at the University of Manitoba IEEE Transactions on Geoscience and Remote Sensing 53 3 1271 1286
institution Open Polar
collection MSpace at the University of Manitoba
op_collection_id ftunivmanitoba
language English
topic geophysical measurements
ice surface
laser applications
measurement by laser beam
radar scattering
sea ice
surface roughness
surface topography
spellingShingle geophysical measurements
ice surface
laser applications
measurement by laser beam
radar scattering
sea ice
surface roughness
surface topography
Landy, Jack
Isleifson, Dustin
Komarov, Alexander
Barber, David
Parameterization of Centimeter-Scale Sea Ice Surface Roughness Using Terrestrial LiDAR
topic_facet geophysical measurements
ice surface
laser applications
measurement by laser beam
radar scattering
sea ice
surface roughness
surface topography
description Microwave scattering from sea ice is partially controlled by the ice surface roughness. In this paper, we propose a technique for calculating 2-D centimeter-scale surface roughness parameters, including the rms height, correlation length, and form of autocorrelation function, from 3-D terrestrial light detection and ranging data. We demonstrate that a single scale of roughness can be extracted from complex sea ice surfaces, incorporating multiple scales of topography, after sophisticated 2-D detrending, and calculate roughness parameters for a wide range of artificial and natural sea ice surface types. The 2-D technique is shown to be considerably more precise than standard 1-D profiling techniques and can therefore characterize surface roughness as a stationary single-scale process, which a 1-D technique typically cannot do. Sea ice surfaces are generally found to have strongly anisotropic correlation lengths, indicating that microwave scattering models for sea ice should include surface spectra that vary as a function of the azimuthal angle of incident radiation. However, our results demonstrate that there is no fundamental relationship between the rms height and correlation length for sea ice surfaces if the sampling area is above a threshold minimum size.
format Article in Journal/Newspaper
author Landy, Jack
Isleifson, Dustin
Komarov, Alexander
Barber, David
author_facet Landy, Jack
Isleifson, Dustin
Komarov, Alexander
Barber, David
author_sort Landy, Jack
title Parameterization of Centimeter-Scale Sea Ice Surface Roughness Using Terrestrial LiDAR
title_short Parameterization of Centimeter-Scale Sea Ice Surface Roughness Using Terrestrial LiDAR
title_full Parameterization of Centimeter-Scale Sea Ice Surface Roughness Using Terrestrial LiDAR
title_fullStr Parameterization of Centimeter-Scale Sea Ice Surface Roughness Using Terrestrial LiDAR
title_full_unstemmed Parameterization of Centimeter-Scale Sea Ice Surface Roughness Using Terrestrial LiDAR
title_sort parameterization of centimeter-scale sea ice surface roughness using terrestrial lidar
publisher IEEE
publishDate 2020
url http://hdl.handle.net/1993/34870
https://doi.org/10.1109/TGRS.2014.2336833
genre Sea ice
genre_facet Sea ice
op_relation Landy, J. C., Isleifson, D., Komarov, A. S., Barber, D. G., 2015. Parameterization of Centimeter-Scale Sea Ice Surface Roughness Using Terrestrial LiDAR. IEEE Trans Geosci Remote Sens. 53(3):1271-1286. https://doi.org/10.1109/TGRS.2014.233683.
http://hdl.handle.net/1993/34870
doi:10.1109/TGRS.2014.2336833
op_rights open access
op_doi https://doi.org/10.1109/TGRS.2014.233683310.1109/TGRS.2014.233683
container_title IEEE Transactions on Geoscience and Remote Sensing
container_volume 53
container_issue 3
container_start_page 1271
op_container_end_page 1286
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