Abstract

Aerosol observations with ceilometers have been made worldwide recently. To use ceilometer data to retrieve aerosol profiles, raw signals should be accurately converted to the attenuated backscattering coefficient. Hence, the calibration coefficient for the system constant has to be determined correctly. We conducted a ceilometer–lidar comparative experiment to evaluate the Lufft CHM15k Nimbus product. The attenuated backscattering coefficient using CHM15k was smaller by a factor of 1.48 compared to that of lidar. The calibration coefficient should be periodically corrected using the ceilometer signal itself since lidar data are generally unavailable in the field observations. We recalibrated the product using both Rayleigh fitting and cloud attenuation methods. The correction factor, determined from the recalibration, was 15% (9%) smaller when using the Rayleigh fitting (cloud attenuation) method than the factor determined from lidar. Uncertainties from backscattering ratios at the reference height and the lidar ratio can cause systematic errors in the correction factor determined from the Rayleigh fitting method. Uncertainties due to the multiple scattering factor contribute to systematic errors for the cloud attenuation method. We propose a calibration method using depolarization ratios for future polarization-sensitive ceilometers, which can estimate the calibration coefficient without multiple scattering factors.

Highlights

  • Ceilometers are generally deployed at airports to provide cloud base heights for arriving and departing aircraft

  • CHM15k is a very useful tool to measure aerosol profiles qualitatively, and the attenuated backscattering coefficient product can be used for aerosol studies if the overlap function and calibration coefficient are corrected by users

  • This study indicates that the CHM15k attenuated backscattering coefficient was smaller by a factor of 1.48 than the lidar data

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Summary

Introduction

Ceilometers are generally deployed at airports to provide cloud base heights for arriving and departing aircraft. In addition to detecting cloud base heights,[1] ceilometers can detect the atmospheric boundary layer height[2,3] and provide radiation fog formation alerts.[4] Recently, ceilometers have been used for aerosol profile measurements worldwide. Network observations with ceilometers can capture the three-dimensional distribution of aerosols. In Europe, a ceilometer network has been developed to monitor vertical profiles of aerosols, including volcanic ash.[5,6] In Asia, continuous observations of dust with CL51 (Vaisala) has been conducted at Dalanzadgad, Mongolia, since April 2013,7 and continuous observations with CHM15k (Lufft) began in Mandalgovi, Mongolia, in April 2017

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