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...

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Main Authors: E. M. McCullough, R. J. Sica, J. R. Drummond, G. J. Nott, C. Perro, T. J. Duck
Format: Article
Language:English
Published: Copernicus Publications 2018-02-01
Series:Atmospheric Measurement Techniques
Online Access:https://www.atmos-meas-tech.net/11/861/2018/amt-11-861-2018.pdf
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spelling doaj-1efffe5071984a438fc443a58865de672020-11-24T21:42:16ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482018-02-011186187910.5194/amt-11-861-2018Three-channel single-wavelength lidar depolarization calibrationE. M. McCullough0E. M. McCullough1R. J. Sica2J. R. Drummond3G. J. Nott4G. J. Nott5C. Perro6T. J. Duck7Department of Physics and Astronomy, The University of Western Ontario, 1151 Richmond St., London, ON, N6A 3K7, CanadaDepartment of Physics and Atmospheric Science, Dalhousie University, 6310 Coburg Rd., P.O. Box 15000, Halifax, NS, B3H 4R2, CanadaDepartment of Physics and Astronomy, The University of Western Ontario, 1151 Richmond St., London, ON, N6A 3K7, CanadaDepartment of Physics and Atmospheric Science, Dalhousie University, 6310 Coburg Rd., P.O. Box 15000, Halifax, NS, B3H 4R2, CanadaDepartment of Physics and Atmospheric Science, Dalhousie University, 6310 Coburg Rd., P.O. Box 15000, Halifax, NS, B3H 4R2, Canadacurrently at: Facility for Airborne Atmospheric Measurements, Building 146, Cranfield University, Cranfield, MK43 0AL, UKDepartment of Physics and Atmospheric Science, Dalhousie University, 6310 Coburg Rd., P.O. Box 15000, Halifax, NS, B3H 4R2, CanadaDepartment of Physics and Atmospheric Science, Dalhousie University, 6310 Coburg Rd., P.O. Box 15000, Halifax, NS, B3H 4R2, CanadaLinear 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.https://www.atmos-meas-tech.net/11/861/2018/amt-11-861-2018.pdf
collection DOAJ
language English
format Article
sources DOAJ
author E. M. McCullough
E. M. McCullough
R. J. Sica
J. R. Drummond
G. J. Nott
G. J. Nott
C. Perro
T. J. Duck
spellingShingle E. M. McCullough
E. M. McCullough
R. J. Sica
J. R. Drummond
G. J. Nott
G. J. Nott
C. Perro
T. J. Duck
Three-channel single-wavelength lidar depolarization calibration
Atmospheric Measurement Techniques
author_facet E. M. McCullough
E. M. McCullough
R. J. Sica
J. R. Drummond
G. J. Nott
G. J. Nott
C. Perro
T. J. Duck
author_sort E. M. McCullough
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
publisher Copernicus Publications
series Atmospheric Measurement Techniques
issn 1867-1381
1867-8548
publishDate 2018-02-01
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.
url https://www.atmos-meas-tech.net/11/861/2018/amt-11-861-2018.pdf
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