Calibration and validation of the advanced E-Region Wind Interferometer

The advanced E-Region Wind Interferometer (ERWIN II) combines the imaging capabilities of a CCD detector with the wide field associated with field-widened Michelson interferometry. This instrument is capable of simultaneous multi-directional wind observations for three different airglow emissions (o...

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Published in:Atmospheric Measurement Techniques
Main Authors: Kristoffersen, S. K., Ward, W. E., Brown, S., Drummond, J. R.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/amt-6-1761-2013
https://amt.copernicus.org/articles/6/1761/2013/
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spelling ftcopernicus:oai:publications.copernicus.org:amt17702 2023-05-15T16:08:36+02:00 Calibration and validation of the advanced E-Region Wind Interferometer Kristoffersen, S. K. Ward, W. E. Brown, S. Drummond, J. R. 2018-01-15 application/pdf https://doi.org/10.5194/amt-6-1761-2013 https://amt.copernicus.org/articles/6/1761/2013/ eng eng doi:10.5194/amt-6-1761-2013 https://amt.copernicus.org/articles/6/1761/2013/ eISSN: 1867-8548 Text 2018 ftcopernicus https://doi.org/10.5194/amt-6-1761-2013 2020-07-20T16:25:24Z The advanced E-Region Wind Interferometer (ERWIN II) combines the imaging capabilities of a CCD detector with the wide field associated with field-widened Michelson interferometry. This instrument is capable of simultaneous multi-directional wind observations for three different airglow emissions (oxygen green line (O( 1 S)) at a height of ~97 km, the P Q(7) and P (7) emission lines in the O 2 (0–1) atmospheric band at ~93 km and P 1 (3) emission line in the (6, 2) hydroxyl Meinel band at ~87 km) on a three minute cadence. In each direction, for 45 s measurements for typical airglow volume emission rates, the instrument is capable of line-of-sight wind precisions of ~1 m s −1 for hydroxyl and O( 1 S) and ~4 m s −1 for O 2 . This precision is achieved using a new data analysis algorithm which takes advantage of the imaging capabilities of the CCD detector along with knowledge of the instrument phase variation as a function of pixel location across the detector. This instrument is currently located in Eureka, Nunavut as part of the Polar Environment Atmospheric Research Laboratory (PEARL) (80°N, 86° W). The details of the physical configuration, the data analysis algorithm, the measurement calibration and validation of the observations from December 2008 and January 2009 are described. Field measurements which demonstrate the capabilities of this instrument are presented. To our knowledge, the wind determinations with this instrument are the most accurate and have the highest observational cadence for airglow wind observations of this region of the atmosphere and match the capabilities of other wind-measuring techniques. Text Eureka Nunavut Copernicus Publications: E-Journals Eureka ENVELOPE(-85.940,-85.940,79.990,79.990) Nunavut Atmospheric Measurement Techniques 6 7 1761 1776
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The advanced E-Region Wind Interferometer (ERWIN II) combines the imaging capabilities of a CCD detector with the wide field associated with field-widened Michelson interferometry. This instrument is capable of simultaneous multi-directional wind observations for three different airglow emissions (oxygen green line (O( 1 S)) at a height of ~97 km, the P Q(7) and P (7) emission lines in the O 2 (0–1) atmospheric band at ~93 km and P 1 (3) emission line in the (6, 2) hydroxyl Meinel band at ~87 km) on a three minute cadence. In each direction, for 45 s measurements for typical airglow volume emission rates, the instrument is capable of line-of-sight wind precisions of ~1 m s −1 for hydroxyl and O( 1 S) and ~4 m s −1 for O 2 . This precision is achieved using a new data analysis algorithm which takes advantage of the imaging capabilities of the CCD detector along with knowledge of the instrument phase variation as a function of pixel location across the detector. This instrument is currently located in Eureka, Nunavut as part of the Polar Environment Atmospheric Research Laboratory (PEARL) (80°N, 86° W). The details of the physical configuration, the data analysis algorithm, the measurement calibration and validation of the observations from December 2008 and January 2009 are described. Field measurements which demonstrate the capabilities of this instrument are presented. To our knowledge, the wind determinations with this instrument are the most accurate and have the highest observational cadence for airglow wind observations of this region of the atmosphere and match the capabilities of other wind-measuring techniques.
format Text
author Kristoffersen, S. K.
Ward, W. E.
Brown, S.
Drummond, J. R.
spellingShingle Kristoffersen, S. K.
Ward, W. E.
Brown, S.
Drummond, J. R.
Calibration and validation of the advanced E-Region Wind Interferometer
author_facet Kristoffersen, S. K.
Ward, W. E.
Brown, S.
Drummond, J. R.
author_sort Kristoffersen, S. K.
title Calibration and validation of the advanced E-Region Wind Interferometer
title_short Calibration and validation of the advanced E-Region Wind Interferometer
title_full Calibration and validation of the advanced E-Region Wind Interferometer
title_fullStr Calibration and validation of the advanced E-Region Wind Interferometer
title_full_unstemmed Calibration and validation of the advanced E-Region Wind Interferometer
title_sort calibration and validation of the advanced e-region wind interferometer
publishDate 2018
url https://doi.org/10.5194/amt-6-1761-2013
https://amt.copernicus.org/articles/6/1761/2013/
long_lat ENVELOPE(-85.940,-85.940,79.990,79.990)
geographic Eureka
Nunavut
geographic_facet Eureka
Nunavut
genre Eureka
Nunavut
genre_facet Eureka
Nunavut
op_source eISSN: 1867-8548
op_relation doi:10.5194/amt-6-1761-2013
https://amt.copernicus.org/articles/6/1761/2013/
op_doi https://doi.org/10.5194/amt-6-1761-2013
container_title Atmospheric Measurement Techniques
container_volume 6
container_issue 7
container_start_page 1761
op_container_end_page 1776
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