Vertical profiling of optical and physical particle properties over the tropical Indian Ocean with six-wavelength lidar 2. Case studies

Citation
D. Muller et al., Vertical profiling of optical and physical particle properties over the tropical Indian Ocean with six-wavelength lidar 2. Case studies, J GEO RES-A, 106(D22), 2001, pp. 28577-28595
Citations number
93
Categorie Soggetti
Earth Sciences
Volume
106
Issue
D22
Year of publication
2001
Pages
28577 - 28595
Database
ISI
SICI code
Abstract
We present the seasonal cycle of optical and physical particle properties o ver the Indian Ocean based on case studies of six-wavelength aerosol lidar observations performed in the framework of the Indian Ocean Experiment. Fro m February 1999 to March 2000 the lidar system made routine measurements at the International Airport of the Maldives on Hulule island (4.1 degreesN, 73.3 degreesE). The measurement from February 18, 1999, during the northeas t monsoon showed high optical depths of 0.27 at 532 mn. Lidar ratios of 40- 45 sr at 532 nm indicated the long-range transport of well-aged polluted ai r from Southeast Asia. Effective radii of <0.14 mum, complex refractive ind ices >1.6-0.01i, and single-scattering albedos of 0.86-0.93 at 532 nm were retrieved for the pollution layer above 1000 m height. Similar physical par ticle properties followed from the measurement on March 22, 2000. Optical d epths were 0.4; lidar ratios of 60 sr at 1000 m height indicated anthropoge nic pollution from India. Values of 45 sr at 3000 m height indicated a cons iderable influence by clean-continental particles from Africa and Arabia. A ccordingly, the single-scattering albedo ranged from 0.85-0.9. During the s outhwest monsoon in July, air was advected from the western Indian Ocean, e astern Africa, and Arabia. Particles were transported into maximum heights of 5 km from these regions on July 12, 1999. Small effective radii of 0.18- 0.3 mum, considerably lower mean complex refractive indices of <1.6-0.02i, and single-scattering albedos >0.88 indicated the prevailing clean-marine a nd clean-continental conditions. The intermonsoon season was characterized by strong washout processes during the crossover of the Intertropical Conve rgence Zone. On October 16, 1999, low optical depths of 0.13 and lidar rati os from 20-35 sr indicated clean-marine conditions. Accordingly, large effe ctive radii of 0.2-0.35 mum, low complex refractive indices similar to1.45- 0.005i, and single-scattering albedos >0.95 were found.