Measurement of wind profiles by motion-stabilised ship-borne Doppler lidar

Three months of Doppler lidar wind measurements were obtained during the Arctic Cloud Summer Experiment on the icebreaker Oden during the summer of 2014. Such ship-borne Doppler measurements require active stabilisation to remove the effects of ship motion. We demonstrate that the combination of a c...

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Published in:Atmospheric Measurement Techniques
Main Authors: P. Achtert, I. M. Brooks, B. J. Brooks, B. I. Moat, J. Prytherch, P. O. G. Persson, M. Tjernström
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2015
Subjects:
Online Access:https://doi.org/10.5194/amt-8-4993-2015
https://doaj.org/article/7ca4cad3a0c249e0b43fb0066469c83e
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author P. Achtert
I. M. Brooks
B. J. Brooks
B. I. Moat
J. Prytherch
P. O. G. Persson
M. Tjernström
author_facet P. Achtert
I. M. Brooks
B. J. Brooks
B. I. Moat
J. Prytherch
P. O. G. Persson
M. Tjernström
author_sort P. Achtert
collection Directory of Open Access Journals: DOAJ Articles
container_issue 11
container_start_page 4993
container_title Atmospheric Measurement Techniques
container_volume 8
description Three months of Doppler lidar wind measurements were obtained during the Arctic Cloud Summer Experiment on the icebreaker Oden during the summer of 2014. Such ship-borne Doppler measurements require active stabilisation to remove the effects of ship motion. We demonstrate that the combination of a commercial Doppler lidar with a custom-made motion-stabilisation platform enables the retrieval of wind profiles in the Arctic atmospheric boundary layer during both cruising and ice-breaking with statistical uncertainties comparable to land-based measurements. This held true particularly within the atmospheric boundary layer even though the overall aerosol load was very low. Motion stabilisation was successful for high wind speeds in open water and the resulting wave conditions. It allows for the retrieval of vertical winds with a random error below 0.2 m s −1 . The comparison of lidar-measured wind and radio soundings gives a mean bias of 0.3 m s −1 (2°) and a mean standard deviation of 1.1 m s −1 (12°) for wind speed (wind direction). The agreement for wind direction degrades with height. The combination of a motion-stabilised platform with a low-maintenance autonomous Doppler lidar has the potential to enable continuous long-term high-resolution ship-based wind profile measurements over the oceans.
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Icebreaker
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Icebreaker
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spelling ftdoajarticles:oai:doaj.org/article:7ca4cad3a0c249e0b43fb0066469c83e 2025-01-16T20:28:56+00:00 Measurement of wind profiles by motion-stabilised ship-borne Doppler lidar P. Achtert I. M. Brooks B. J. Brooks B. I. Moat J. Prytherch P. O. G. Persson M. Tjernström 2015-11-01T00:00:00Z https://doi.org/10.5194/amt-8-4993-2015 https://doaj.org/article/7ca4cad3a0c249e0b43fb0066469c83e EN eng Copernicus Publications http://www.atmos-meas-tech.net/8/4993/2015/amt-8-4993-2015.pdf https://doaj.org/toc/1867-1381 https://doaj.org/toc/1867-8548 1867-1381 1867-8548 doi:10.5194/amt-8-4993-2015 https://doaj.org/article/7ca4cad3a0c249e0b43fb0066469c83e Atmospheric Measurement Techniques, Vol 8, Iss 11, Pp 4993-5007 (2015) Environmental engineering TA170-171 Earthwork. Foundations TA715-787 article 2015 ftdoajarticles https://doi.org/10.5194/amt-8-4993-2015 2022-12-31T12:29:39Z Three months of Doppler lidar wind measurements were obtained during the Arctic Cloud Summer Experiment on the icebreaker Oden during the summer of 2014. Such ship-borne Doppler measurements require active stabilisation to remove the effects of ship motion. We demonstrate that the combination of a commercial Doppler lidar with a custom-made motion-stabilisation platform enables the retrieval of wind profiles in the Arctic atmospheric boundary layer during both cruising and ice-breaking with statistical uncertainties comparable to land-based measurements. This held true particularly within the atmospheric boundary layer even though the overall aerosol load was very low. Motion stabilisation was successful for high wind speeds in open water and the resulting wave conditions. It allows for the retrieval of vertical winds with a random error below 0.2 m s −1 . The comparison of lidar-measured wind and radio soundings gives a mean bias of 0.3 m s −1 (2°) and a mean standard deviation of 1.1 m s −1 (12°) for wind speed (wind direction). The agreement for wind direction degrades with height. The combination of a motion-stabilised platform with a low-maintenance autonomous Doppler lidar has the potential to enable continuous long-term high-resolution ship-based wind profile measurements over the oceans. Article in Journal/Newspaper Arctic Icebreaker oden Directory of Open Access Journals: DOAJ Articles Arctic Atmospheric Measurement Techniques 8 11 4993 5007
spellingShingle Environmental engineering
TA170-171
Earthwork. Foundations
TA715-787
P. Achtert
I. M. Brooks
B. J. Brooks
B. I. Moat
J. Prytherch
P. O. G. Persson
M. Tjernström
Measurement of wind profiles by motion-stabilised ship-borne Doppler lidar
title Measurement of wind profiles by motion-stabilised ship-borne Doppler lidar
title_full Measurement of wind profiles by motion-stabilised ship-borne Doppler lidar
title_fullStr Measurement of wind profiles by motion-stabilised ship-borne Doppler lidar
title_full_unstemmed Measurement of wind profiles by motion-stabilised ship-borne Doppler lidar
title_short Measurement of wind profiles by motion-stabilised ship-borne Doppler lidar
title_sort measurement of wind profiles by motion-stabilised ship-borne doppler lidar
topic Environmental engineering
TA170-171
Earthwork. Foundations
TA715-787
topic_facet Environmental engineering
TA170-171
Earthwork. Foundations
TA715-787
url https://doi.org/10.5194/amt-8-4993-2015
https://doaj.org/article/7ca4cad3a0c249e0b43fb0066469c83e