2001
DOI: 10.1364/ao.40.004759
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Wavelength dependence of backscatter by use of aerosol microphysics and lidar data sets: application to 21-µm wavelength for space-based and airborne lidars

Abstract: An aerosol microphysics dataset was used to model backscatter in the 0.35-11-mum wavelength range, with the results validated by comparison with measured cw and pulsed lidar backscatter obtained during two NASA-sponsored airborne field experiments. Different atmospheric features were encountered, with aerosol backscatter ranging over 4 orders of magnitude. Modeled conversion functions were used to convert existing lidar backscatter datasets to 2.1 mum. Resulting statistical distribution shows the midtropospher… Show more

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Cited by 18 publications
(15 citation statements)
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“…The only reliable method of assessing the variability of the aerosol versus time and height in a given location is to collect datasets over an extended period. The frequency of precipitation, the back trajectory of the air mass, and the season are all factors that are known to influence the aerosol concentration (Spinhirne et al 1997;Srivastava et al 2001;Vaughan et al 2002). The observed SNR versus height for the complete vertically staring dataset was analyzed and Fig.…”
Section: B Snr Statisticsmentioning
confidence: 99%
“…The only reliable method of assessing the variability of the aerosol versus time and height in a given location is to collect datasets over an extended period. The frequency of precipitation, the back trajectory of the air mass, and the season are all factors that are known to influence the aerosol concentration (Spinhirne et al 1997;Srivastava et al 2001;Vaughan et al 2002). The observed SNR versus height for the complete vertically staring dataset was analyzed and Fig.…”
Section: B Snr Statisticsmentioning
confidence: 99%
“…The in situ instruments provided both microphysical measurements and thermal IR scattering characteristics at flight altitude. Extensive comparisons of the focused CW laser backscatter data and modeled aerosol backscatter using the particle counters have been reported [ Cutten et al , 1996; Srivastava et al , 1997; Cutten et al , 1998; Srivastava et al , 2001]. Several studies of aerosol in the free troposphere based on measurement data from these in situ instruments have been reported [ Clarke , 1993; Srivastava et al , 1995; Rothermel et al , 1996a; Cutten et al , 1996; Srivastava et al , 1997].…”
Section: Experiments Descriptionmentioning
confidence: 99%
“…In our simulation the combined effects of Mie and molecular backscattering are taken into account. Since the aerosol type and density in the atmosphere is hard to predict and model, we have assumed a moderate loading of aerosols [12] with uniform scattering throughout the measurement range. The Rayleigh backscatter parameters have been adopted from the U.S. Standard Atmospheric Model.…”
Section: Simulation Resultsmentioning
confidence: 99%