Microphysical particle parameters from extinction and backscatter lidar data by inversion with regularization:: theory

被引:290
作者
Müller, D [1 ]
Wandinger, U [1 ]
Ansmann, A [1 ]
机构
[1] Inst Tropospher Res, D-04318 Leipzig, Germany
关键词
D O I
10.1364/AO.38.002346
中图分类号
O43 [光学];
学科分类号
070207 ; 0803 ;
摘要
A method is proposed that permits one to retrieve physical parameters of tropospheric particle size distributions, e.g., effective radius, volume, surface-area, and number concentrations, as well as the mean complex refractive index on a routine basis from backscatter and extinction coefficients at multiple wavelengths. The optical data in terms of vertical profiles are derived from multiple-wavelength lidar measurements at 355, 400, 532, 710, 800, and 1064 nm for backscatter data and 355 and 532 nm for extinction data. The algorithm is based on the concept of inversion with regularization. Regularization is performed by generalized cross-validation. This method does not require knowledge of the shape of the particle size distribution and can handle measurement errors of the order of 20%. It is shown that at least two extinction data are necessary to retrieve the particle parameters to an acceptable accuracy. Simulations with monomodal and bimodal logarithmic-normal size distributions show that it is possible to derive effective radius, volume, and surface-area concentrations to an accuracy of +/-50%, the real part of the complex refractive index to +/-0.05, and the imaginary part to +/-50%. Number concentrations may have errors larger than +/-50%. (C) 1999 Optical Society of America.
引用
收藏
页码:2346 / 2357
页数:12
相关论文
共 104 条
[1]   RELATIONSHIP BETWEEN VARIABLE SELECTION AND DATA AUGMENTATION AND A METHOD FOR PREDICTION [J].
ALLEN, DM .
TECHNOMETRICS, 1974, 16 (01) :125-127
[2]   MAXIMUM-ENTROPY REGULARIZATION OF FREDHOLM INTEGRAL-EQUATIONS OF THE 1ST KIND [J].
AMATO, U ;
HUGHES, W .
INVERSE PROBLEMS, 1991, 7 (06) :793-808
[3]   OBJECTIVE ALGORITHMS FOR THE AEROSOL PROBLEM [J].
AMATO, U ;
CARFORA, MF ;
CUOMO, V ;
SERIO, C .
APPLIED OPTICS, 1995, 34 (24) :5442-5452
[4]  
[Anonymous], SOVIET MATH DOKLADY
[5]   INDEPENDENT MEASUREMENT OF EXTINCTION AND BACKSCATTER PROFILES IN CIRRUS CLOUDS BY USING A COMBINED RAMAN ELASTIC-BACKSCATTER LIDAR [J].
ANSMANN, A ;
WANDINGER, U ;
RIEBESELL, M ;
WEITKAMP, C ;
MICHAELIS, W .
APPLIED OPTICS, 1992, 31 (33) :7113-7131
[6]   UNIQUENESS IN INVERSION OF INACCURATE GROSS EARTH DATA [J].
BACKUS, G ;
GILBERT, F .
PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY OF LONDON SERIES A-MATHEMATICAL AND PHYSICAL SCIENCES, 1970, 266 (1173) :123-&
[7]  
BACKUS G, 1968, GEOPHYS J ROY ASTRON, V266, P169
[8]   DETERMINATION OF ATMOSPHERIC AEROSOL SIZE DISTRIBUTION-FUNCTIONS FROM SCREEN DIFFUSION BATTERY DATA - MATHEMATICAL ASPECTS [J].
BASHUROVA, VS ;
KOUTZENOGIL, KP ;
PUSEP, AY ;
SHOKHIREV, NV .
JOURNAL OF AEROSOL SCIENCE, 1991, 22 (03) :373-388
[9]   INVERSE PROBLEM AND THE PSEUDOEMPIRICAL ORTHOGONAL FUNCTION-METHOD OF SOLUTION .1. THEORY [J].
BEN-DAVID, A ;
HERMAN, BM ;
REAGAN, JA .
APPLIED OPTICS, 1988, 27 (07) :1235-1242
[10]   INVERSE PROBLEM AND THE PSEUDOEMPIRICAL ORTHOGONAL FUNCTION-METHOD OF SOLUTION .2. USE [J].
BEN-DAVID, A ;
HERMAN, BM ;
REAGAN, JA .
APPLIED OPTICS, 1988, 27 (07) :1243-1254