Three-channel single-wavelength lidar depolarization calibration

Linear depolarization measurement capabilities were added to the CANDAC Rayleigh–Mie–Raman lidar (CRL) at Eureka, Nunavut, in the Canadian High Arctic in 2010. This upgrade enables measurements of the phases (liquid versus ice) of cold and mixed-phase clouds throughout the year, including during pol...

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Published in:Atmospheric Measurement Techniques
Main Authors: McCullough, Emily M., Sica, Robert J., Drummond, James R., Nott, Graeme J., Perro, Christopher, Duck, Thomas J.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/amt-11-861-2018
https://amt.copernicus.org/articles/11/861/2018/
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spelling ftcopernicus:oai:publications.copernicus.org:amt61568 2023-05-15T15:07:33+02:00 Three-channel single-wavelength lidar depolarization calibration McCullough, Emily M. Sica, Robert J. Drummond, James R. Nott, Graeme J. Perro, Christopher Duck, Thomas J. 2018-10-26 application/pdf https://doi.org/10.5194/amt-11-861-2018 https://amt.copernicus.org/articles/11/861/2018/ eng eng doi:10.5194/amt-11-861-2018 https://amt.copernicus.org/articles/11/861/2018/ eISSN: 1867-8548 Text 2018 ftcopernicus https://doi.org/10.5194/amt-11-861-2018 2020-07-20T16:23:25Z Linear depolarization measurement capabilities were added to the CANDAC Rayleigh–Mie–Raman lidar (CRL) at Eureka, Nunavut, in the Canadian High Arctic in 2010. This upgrade enables measurements of the phases (liquid versus ice) of cold and mixed-phase clouds throughout the year, including during polar night. Depolarization measurements were calibrated according to existing methods using parallel- and perpendicular-polarized profiles as discussed in ). We present a new technique that uses the polarization-independent Rayleigh elastic channel in combination with one of the new polarization-dependent channels, and we show that for a lidar with low signal in one of the polarization-dependent channels this method is superior to the traditional method. The optimal procedure for CRL is to determine the depolarization parameter using the traditional method at low resolution (from parallel and perpendicular signals) and then to use this value to calibrate the high-resolution new measurements (from parallel and polarization-independent Rayleigh elastic signals). Due to its use of two high-signal-rate channels, the new method has lower statistical uncertainty and thus gives depolarization parameter values at higher spatial–temporal resolution by up to a factor of 20 for CRL. This method is easily adaptable to other lidar systems which are considering adding depolarization capability to existing hardware. Text Arctic Eureka Nunavut polar night Copernicus Publications: E-Journals Arctic Eureka ENVELOPE(-85.940,-85.940,79.990,79.990) Nunavut Atmospheric Measurement Techniques 11 2 861 879
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Linear depolarization measurement capabilities were added to the CANDAC Rayleigh–Mie–Raman lidar (CRL) at Eureka, Nunavut, in the Canadian High Arctic in 2010. This upgrade enables measurements of the phases (liquid versus ice) of cold and mixed-phase clouds throughout the year, including during polar night. Depolarization measurements were calibrated according to existing methods using parallel- and perpendicular-polarized profiles as discussed in ). We present a new technique that uses the polarization-independent Rayleigh elastic channel in combination with one of the new polarization-dependent channels, and we show that for a lidar with low signal in one of the polarization-dependent channels this method is superior to the traditional method. The optimal procedure for CRL is to determine the depolarization parameter using the traditional method at low resolution (from parallel and perpendicular signals) and then to use this value to calibrate the high-resolution new measurements (from parallel and polarization-independent Rayleigh elastic signals). Due to its use of two high-signal-rate channels, the new method has lower statistical uncertainty and thus gives depolarization parameter values at higher spatial–temporal resolution by up to a factor of 20 for CRL. This method is easily adaptable to other lidar systems which are considering adding depolarization capability to existing hardware.
format Text
author McCullough, Emily M.
Sica, Robert J.
Drummond, James R.
Nott, Graeme J.
Perro, Christopher
Duck, Thomas J.
spellingShingle McCullough, Emily M.
Sica, Robert J.
Drummond, James R.
Nott, Graeme J.
Perro, Christopher
Duck, Thomas J.
Three-channel single-wavelength lidar depolarization calibration
author_facet McCullough, Emily M.
Sica, Robert J.
Drummond, James R.
Nott, Graeme J.
Perro, Christopher
Duck, Thomas J.
author_sort McCullough, Emily M.
title Three-channel single-wavelength lidar depolarization calibration
title_short Three-channel single-wavelength lidar depolarization calibration
title_full Three-channel single-wavelength lidar depolarization calibration
title_fullStr Three-channel single-wavelength lidar depolarization calibration
title_full_unstemmed Three-channel single-wavelength lidar depolarization calibration
title_sort three-channel single-wavelength lidar depolarization calibration
publishDate 2018
url https://doi.org/10.5194/amt-11-861-2018
https://amt.copernicus.org/articles/11/861/2018/
long_lat ENVELOPE(-85.940,-85.940,79.990,79.990)
geographic Arctic
Eureka
Nunavut
geographic_facet Arctic
Eureka
Nunavut
genre Arctic
Eureka
Nunavut
polar night
genre_facet Arctic
Eureka
Nunavut
polar night
op_source eISSN: 1867-8548
op_relation doi:10.5194/amt-11-861-2018
https://amt.copernicus.org/articles/11/861/2018/
op_doi https://doi.org/10.5194/amt-11-861-2018
container_title Atmospheric Measurement Techniques
container_volume 11
container_issue 2
container_start_page 861
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