Eduardo Landulfo1, Lucila Maria Viola Pozzetti2, Antônio Renato Biral3, Ani Sobral Torres4, Caio Alencar de Matos5, Patricia Sawamura6, Alexandros Papayannis7

Centro de Lasers e Aplicações, Instituto de Pesquisas Energéticas e Nucleares,Av. Lineu Prestes, 2242 – São Paulo – SP – 05508-000 – Brazil
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7 National Technical University of Athens, Heroon Polytechniou 9 – 15780 – Zografou – Athens, This e-mail address is being protected from spambots. You need JavaScript enabled to view it

 

During the months of January through March 2004 Lidar measurements were carried with an aerosol backscattering LIDAR within the frame of the HIBISCUS-TROCCINOX-TROCCIBRAS campaign. The main goals of this joint campaign were to study the impact of aerosols and ozone precursors being transported to the stratosphere due convection vertical motion. The data here presented summarizes these measurements with a special emphasis to the planetary boundary layer altitude and its time evolution, cloud base height and some instances of calculated aerosol backscattering coefficient in the 532 nm.