Aerosol-cloud color ratio derived from 1064 nm – 532 nm LIDAR measurements

Authors

  • Hans Walter P. Chua Physics Department, De La Salle University
  • Edgar A. Vallar Physics Department, De La Salle University
  • Ernest P. Macalalad Physics Department, De La Salle University
  • Eric B. Bangsal Physics Department, De La Salle University
  • Lance Tan Physics Department, De La Salle University
  • Jasper Feraer Physics Department, De La Salle University
  • R. Goseco Physics Department, De La Salle University
  • Maria Cecilia D. Galvez Physics Department, De La Salle University

Abstract

The aerosol and cloud color ratio from 1064 nm and 532 nm MIE LIDAR measurements was determined in this work. MIE LIDAR data was obtained for the two wavelengths using LabView VIs developed by our group. The color ratio was derived from the ratio of 1064 nm over 532 nm aerosol backscatter coefficients. Aerosol backscatter coefficients were computed using Fernald's inversion algorithm where the extinction-to-backscatter ratio (Sa) was kept at 30 sr for all altitudes. This paper presents data for June 21, 2006. Results show the capability of the color ratio to differentiate between clouds and aerosols.

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Article ID

SPP-2006-3F-03

Section

Atmospheric Physics

Published

2006-10-25

How to Cite

[1]
HWP Chua, EA Vallar, EP Macalalad, EB Bangsal, L Tan, J Feraer, R Goseco, and MCD Galvez, Aerosol-cloud color ratio derived from 1064 nm – 532 nm LIDAR measurements, Proceedings of the Samahang Pisika ng Pilipinas 24, SPP-2006-3F-03 (2006). URL: https://proceedings.spp-online.org/article/view/SPP-2006-3F-03.