An autonomous Doppler Sodar wind profiling system

An autonomous Doppler sodar wind profiling system has been designed, built, tested, and then deployed for 2 years at a remote site in Coats Land, Antarctica. The system is designed around a commercially available phased-array sodar (a Scintec flat-array sodar, FAS64) and powered from five modular po...

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Published in:Journal of Atmospheric and Oceanic Technology
Main Authors: Anderson, Philip S., Ladkin, Russell S., Renfrew, Ian A.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Meteorological Society 2005
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/1615/
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spelling ftnerc:oai:nora.nerc.ac.uk:1615 2024-06-09T07:39:14+00:00 An autonomous Doppler Sodar wind profiling system Anderson, Philip S. Ladkin, Russell S. Renfrew, Ian A. 2005 http://nora.nerc.ac.uk/id/eprint/1615/ unknown American Meteorological Society Anderson, Philip S.; Ladkin, Russell S.; Renfrew, Ian A. 2005 An autonomous Doppler Sodar wind profiling system. Journal of Atmospheric and Oceanic Technology, 22 (9). 1309-1325. https://doi.org/10.1175/JTECH1779.1 <https://doi.org/10.1175/JTECH1779.1> Atmospheric Sciences Electronics Engineering and Technology Publication - Article PeerReviewed 2005 ftnerc https://doi.org/10.1175/JTECH1779.1 2024-05-15T08:42:16Z An autonomous Doppler sodar wind profiling system has been designed, built, tested, and then deployed for 2 years at a remote site in Coats Land, Antarctica. The system is designed around a commercially available phased-array sodar (a Scintec flat-array sodar, FAS64) and powered from five modular power system units. Each power unit comprises two batteries, two photovoltaic solar panels, and two vertical axis wind generators, plus charging control and isolation circuitry. The sodar’s main processing unit is located at the antenna, but is controlled from a manned research station 50 km distant, in real time, by a line-of-sight UHF radio link. Data from an integral automatic weather station (AWS) are also transmitted over the radio link, allowing meteorologically informed decisions on whether or not to operate the Doppler sodar. Over the 2-yr experiment dozens of sounding episodes, lasting from a few hours to a few days, were obtained. Successful soundings were obtained in temperatures down to −33°C, and wind speeds up to 12 m s−1. In general, the wind data quality was good, but the range was disappointing, probably as a result of the strongly stable atmospheric conditions that were experienced. The wind profiling system that is described has been used to obtain the first remote wintertime observations of katabatic winds over the Antarctic continent. Article in Journal/Newspaper Antarc* Antarctic Antarctica Natural Environment Research Council: NERC Open Research Archive Antarctic Coats Land ENVELOPE(-27.500,-27.500,-77.000,-77.000) The Antarctic Journal of Atmospheric and Oceanic Technology 22 9 1309 1325
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language unknown
topic Atmospheric Sciences
Electronics
Engineering and Technology
spellingShingle Atmospheric Sciences
Electronics
Engineering and Technology
Anderson, Philip S.
Ladkin, Russell S.
Renfrew, Ian A.
An autonomous Doppler Sodar wind profiling system
topic_facet Atmospheric Sciences
Electronics
Engineering and Technology
description An autonomous Doppler sodar wind profiling system has been designed, built, tested, and then deployed for 2 years at a remote site in Coats Land, Antarctica. The system is designed around a commercially available phased-array sodar (a Scintec flat-array sodar, FAS64) and powered from five modular power system units. Each power unit comprises two batteries, two photovoltaic solar panels, and two vertical axis wind generators, plus charging control and isolation circuitry. The sodar’s main processing unit is located at the antenna, but is controlled from a manned research station 50 km distant, in real time, by a line-of-sight UHF radio link. Data from an integral automatic weather station (AWS) are also transmitted over the radio link, allowing meteorologically informed decisions on whether or not to operate the Doppler sodar. Over the 2-yr experiment dozens of sounding episodes, lasting from a few hours to a few days, were obtained. Successful soundings were obtained in temperatures down to −33°C, and wind speeds up to 12 m s−1. In general, the wind data quality was good, but the range was disappointing, probably as a result of the strongly stable atmospheric conditions that were experienced. The wind profiling system that is described has been used to obtain the first remote wintertime observations of katabatic winds over the Antarctic continent.
format Article in Journal/Newspaper
author Anderson, Philip S.
Ladkin, Russell S.
Renfrew, Ian A.
author_facet Anderson, Philip S.
Ladkin, Russell S.
Renfrew, Ian A.
author_sort Anderson, Philip S.
title An autonomous Doppler Sodar wind profiling system
title_short An autonomous Doppler Sodar wind profiling system
title_full An autonomous Doppler Sodar wind profiling system
title_fullStr An autonomous Doppler Sodar wind profiling system
title_full_unstemmed An autonomous Doppler Sodar wind profiling system
title_sort autonomous doppler sodar wind profiling system
publisher American Meteorological Society
publishDate 2005
url http://nora.nerc.ac.uk/id/eprint/1615/
long_lat ENVELOPE(-27.500,-27.500,-77.000,-77.000)
geographic Antarctic
Coats Land
The Antarctic
geographic_facet Antarctic
Coats Land
The Antarctic
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_relation Anderson, Philip S.; Ladkin, Russell S.; Renfrew, Ian A. 2005 An autonomous Doppler Sodar wind profiling system. Journal of Atmospheric and Oceanic Technology, 22 (9). 1309-1325. https://doi.org/10.1175/JTECH1779.1 <https://doi.org/10.1175/JTECH1779.1>
op_doi https://doi.org/10.1175/JTECH1779.1
container_title Journal of Atmospheric and Oceanic Technology
container_volume 22
container_issue 9
container_start_page 1309
op_container_end_page 1325
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