2004
DOI: 10.1364/ao.43.001180
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Inversion of multiwavelength Raman lidar data for retrieval of bimodal aerosol size distribution

Abstract: We report on the feasibility of deriving microphysical parameters of bimodal particle size distributions from Mie-Raman lidar based on a triple Nd:YAG laser. Such an instrument provides backscatter coefficients at 355, 532, and 1064 nm and extinction coefficients at 355 and 532 nm. The inversion method employed is Tikhonov's inversion with regularization. Special attention has been paid to extend the particle size range for which this inversion scheme works to approximately 10 microm, which makes this algorith… Show more

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Cited by 159 publications
(176 citation statements)
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“…Another technique that is widely used is the Tikhonov-Phillips Regularization (TPR), which shifts the spectrum of the operator (see [3,6,7]), thus…”
Section: Regularizationmentioning
confidence: 99%
See 1 more Smart Citation
“…Another technique that is widely used is the Tikhonov-Phillips Regularization (TPR), which shifts the spectrum of the operator (see [3,6,7]), thus…”
Section: Regularizationmentioning
confidence: 99%
“…Also, there is lots of research into the questions on how special a priori information on the solution can be used to improve the results. In [7], for instance, a special algorithm for the retrieval of bi-modal distributions is proposed. Another example can be found in [8], which takes special care to incorporate a priori information on the solution in the form of a nonnegativity constraint.…”
Section: Introductionmentioning
confidence: 99%
“…Although having multiple advantages (high dynamic range, high spatial and temporal resolution), lidar data suffer by a limited physical content. Both the problems of retrieving optical profiles and microphysical properties from lidar data are ill-posed, needing advanced mathematical algorithms [1]- [3].…”
Section: Introductionmentioning
confidence: 99%
“…The source and type of aerosols in cloud-free regions close to the cloud boundaries are identified from the analysis of the air mass backtrajectories provided by NOAA Hysplit model [5], along with the values of multi-wavelength aerosol lidar ratios (S) and the Ångström exponents (å) [6], averaged over the altitude range between the cloud base and the cloud top. In the same region, the aerosol size distribution close to the clouds is also retrieved from multi-wavelength aerosol extensive optical properties, averaged over the altitude range between the base and the top of the cloudy region, using the algorithm developed by Veselovskii [7]. …”
Section: Methodsmentioning
confidence: 99%