Optical measurements of atmospheric particles from airborne platforms: in situ and remote sensing instruments for balloons and aircrafts

Multiwavelength laser backscattersondes (MAS) have been widely used from a variety of airborne platforms for in situ measurements of optical properties of clouds and atmospheric particulate as well as their phase and com- position. Recently, a new miniaturized LIDAR (MULID) has been developed using state-of-art technology for balloon borne profiling of the same quantities. A description of the two instruments, a survey of preliminary re- sults obtained during test flights and indications for future use are given.

[1]  C. Buontempo,et al.  The detection of clouds and aerosols with the backscattersonde MAS during the M55 Geophysica campaign for ENVISAT validation , 2003 .

[2]  J. Lamarque,et al.  STRATOSPHERE-TROPOSPHERE EXCHANGE | Local Processes , 2003 .

[3]  S. Balestri,et al.  APE-POLECAT - rationale, road map and summary of measurements , 1999 .

[4]  A. Adriani,et al.  Multiwavelength Aerosol Scatterometer for Airborne Experiments to Study the Optical Properties of Stratospheric Aerosol , 1999 .

[5]  Terry Deshler,et al.  Midlatitude lidar backscatter conversions based on balloonborne aerosol measurements , 1995 .

[6]  E. Danielsen In situ evidence of rapid, vertical, irreversible transport of lower tropospheric air into the lower tropical stratosphere by convective cloud turrets and by larger-scale upwelling in tropical cyclones , 1993 .

[7]  B. Johnson,et al.  Polar stratospheric clouds over McMurdo, Antarctica, during the 1991 spring: Lidar and particle counter measurements , 1992 .

[8]  M. Molina Heterogeneous chemistry on polar stratospheric clouds , 1991 .

[9]  S. Oltmans,et al.  Observations of backscatter, particle concentration and frost point in north polar vortex stratospheric clouds , 1990 .

[10]  S. Oltmans,et al.  Balloon borne observations of PSCs, Frost Point, ozone and nitric acid in the north polar vortex , 1989 .

[11]  P. Crutzen,et al.  Nitric acid cloud formation in the cold Antarctic stratosphere: a major cause for the springtime ‘ozone hole’ , 1986, Nature.

[12]  J. D. Spinhirne,et al.  The Structure and Phase of Cloud Tops as Observed by Polarization Lidar , 1983 .

[13]  J. Spinhirne,et al.  Cloud top remote sensing by airborne lidar. , 1982, Applied optics.