Multiwavelenght 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 composition [Adriani et al. 1999]. MAS is an aerosol backscattersond able to measure backscatter ratio (BR) and depolarization (D) ratio of the airmass in close proximity to its platform, with 2 seconds of temporal resolution. In the cases reported afterward, given the aircraft cruising speed, that translate into 400 metres of horizontal resolution. BR is a sort of optical mixing ratio of the particles in the atmosphere while D gives information about asphericity of the scatterers, hence their thermo dynamical state. In the last year we have deployed this instrument in the ENVISAT validation campaigns. A description of the instruments, a survey of results obtained so far and indications for future use will be given.

the detection of clouds and aerosols with the backscattersonde MAS during the m55 geophysica campaign for envisat validation

F Cairo;M Snels;F Cardillo;M Moriconi
2003

Abstract

Multiwavelenght 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 composition [Adriani et al. 1999]. MAS is an aerosol backscattersond able to measure backscatter ratio (BR) and depolarization (D) ratio of the airmass in close proximity to its platform, with 2 seconds of temporal resolution. In the cases reported afterward, given the aircraft cruising speed, that translate into 400 metres of horizontal resolution. BR is a sort of optical mixing ratio of the particles in the atmosphere while D gives information about asphericity of the scatterers, hence their thermo dynamical state. In the last year we have deployed this instrument in the ENVISAT validation campaigns. A description of the instruments, a survey of results obtained so far and indications for future use will be given.
2003
Istituto di Scienze dell'Atmosfera e del Clima - ISAC
92-9092-840-9
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/86389
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