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...
Main Authors: | , , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2018-02-01
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Series: | Atmospheric Measurement Techniques |
Online Access: | https://www.atmos-meas-tech.net/11/861/2018/amt-11-861-2018.pdf |
Summary: | 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. |
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ISSN: | 1867-1381 1867-8548 |