Abstract

Abstract. The atmospheric boundary layer is an important atmospheric feature that affects environmental health and weather forecasting. In this study, we proposed a graphics algorithm for the derivation of atmospheric boundary layer height (BLH) from the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) data. Owing to the differences in scattering intensity between molecular and aerosol particles, the total attenuated backscatter coefficient 532 and attenuated backscatter coefficient 1064 were used simultaneously for BLH detection. The proposed algorithm transformed the gradient solution into graphics distribution solution to overcome the effects of large noise and improve the horizontal resolution. This method was then tested with real signals under different horizontal smoothing numbers (1, 3, 15 and 30). Finally, the results of BLH obtained by CALIPSO data were compared with the results retrieved by the ground-based lidar measurements. Under the horizontal smoothing number of 15, 12 and 9, the correlation coefficients between the BLH derived by the proposed algorithm and ground-based lidar were both 0.72. Under the horizontal smoothing number of 6, 3 and 1, the correlation coefficients between the BLH derived by graphics distribution method (GDM) algorithm and ground-based lidar were 0.47, 0.14 and 0.12, respectively. When the horizontal smoothing number was large (15, 12 and 9), the CALIPSO BLH derived by the proposed method demonstrated a good correlation with ground-based lidar. The algorithm provided a reliable result when the horizontal smoothing number was greater than 9. This finding indicated that the proposed algorithm can be applied to the CALIPSO satellite data with 3 and 5 km horizontal resolution.

Highlights

  • The atmospheric boundary layer is the layer of the Earth’s surface atmosphere, which is closely related to human activities (Bonin et al, 2013; Reuder et al, 2009; Flamant et al, 1997)

  • The results of boundary layer height (BLH) obtained by Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) data were compared with those retrieved by the ground-based lidar during January 2013 to December 2017

  • We proposed a graphics algorithm to obtain the BLHs from CALIPSO data

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Summary

Introduction

The atmospheric boundary layer is the layer of the Earth’s surface atmosphere, which is closely related to human activities (Bonin et al, 2013; Reuder et al, 2009; Flamant et al, 1997). It plays a crucial role in regional environmental pollution and is important in weather forecasting model The boundary layer height (BLH) is essential to atmospheric aerosol pollution and must be accurately and continuously monitored (Li et al, 2017)

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