CN114488198A - Multi-wavelength laser radar aerosol micro-physical characteristic inversion method based on multi-element full-array random forest - Google Patents
Multi-wavelength laser radar aerosol micro-physical characteristic inversion method based on multi-element full-array random forest Download PDFInfo
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Abstract
本发明公开了一种基于多元全排列随机森林的多波长激光雷达气溶胶微物理特性方法,包括:构建气溶胶光学‑微物理特性查找表;归一化输入光学特性和查找表获得
和Gnorm;计算与Gnorm对应个体的偏差并缩减查找表;对归一化光学特性全排列获得搜索序列,依次计算与Gnorm对应的归一化光学特性的相对误差,按误差大小缩减查找表可行解,将保留的查找表可行解平均获得备选微物理特性;基于随机森林理论,生成NRF个搜索序列并获得NRF个备选解,平均备选解获得反演的微物理特性和光学特性;并进一步计算其余的微物理特性。本发明结合KNN‑最近邻和随机森林原理,基于多波长激光雷达实现细模态气溶胶复折射率精确反演并将其应用于更少激光雷达通道。The invention discloses a multi-wavelength laser radar aerosol micro-physical characteristic method based on multivariate full-array random forest, comprising: constructing a look-up table of aerosol optical-micro-physical characteristics; normalizing input optical characteristics and obtaining the look-up table
and G norm ; compute The deviation of the individual corresponding to G norm is reduced and the look-up table is reduced; the search sequence is obtained by arranging the normalized optical properties, and then calculate The relative error of the normalized optical characteristics corresponding to G norm , the feasible solutions of the look-up table are reduced according to the size of the error, and the remaining feasible solutions of the look-up table are averaged to obtain alternative microphysical properties; based on the random forest theory, N RF search sequences are generated and Obtain N RF candidate solutions, average the candidate solutions to obtain the inverted microphysical properties and optical properties; and further calculate the remaining microphysical properties. The invention combines the KNN-nearest neighbor and random forest principles, realizes the precise inversion of the complex refractive index of the fine-mode aerosol based on the multi-wavelength laser radar, and applies it to fewer laser radar channels.Description
Technical Field
The invention belongs to the technical field of atmospheric aerosol remote sensing laser radars, and particularly relates to a multi-wavelength laser radar aerosol micro-physical characteristic inversion method based on a multi-element full-array random forest.
Background
Haze not only harms human health, promotes diseases such as respiratory diseases and cardiovascular diseases to be highly developed, but also causes regional and global climate change, so that weather such as extreme high temperature and strong rainfall is frequent, and the normal production and life of human are also seriously influenced. Aerosol particles suspended in the atmosphere are not only the main culprit of causing atmospheric pollution (haze) but also key factors of causing extreme weather phenomena. Atmospheric aerosols can be simply classified into different types of urban pollution, smog, sea salt, mineral dust, and the like. The first two aerosols with small spherical particles are usually dominated by the fine mode fraction, often referred to as fine mode aerosols, in terms of Particle Size Distribution (PSD). The fine mode is an important aspect of atmospheric research and is one of important sources of uncertainty of climate prediction, and is closely related to human activities.
In order to better quantify the impact of fine mode aerosols on earth energy budget, air quality and human health, their fundamental micro-physical properties, such as Complex Refractive Index (CRI), PSD, bulk properties (effective radius, number concentration, surface area concentration, volume concentration) and Single Scattering Albedo (SSA), need to be probed and studied.
YAG laser-based advanced multi-wavelength lidar, such as Raman lidar and High Spectral Resolution Lidar (HSRL), have been shown to describe the micro-physical properties of the fine-mode aerosol, which provides a unique opportunity for studying the fundamental properties of the fine-mode aerosol in distance resolution. The backscattering coefficients (β) at 355nm, 532nm and 1064nm and the extinction coefficients (α) at 355nm and 532nm, commonly referred to as 3 β +2 α structures, measured by a three-wavelength lidar, can be used to invert the aerosol micro-physical properties. However, limited to limited input parameters, inversion of aerosol microphysical properties from 3 β +2 α lidar data requires solving ill-posed inversion problems.
At present, regularization, linear evaluation method, permutation search average method and other methods have been developed to solve the inverse problem of inversion of micro physical properties. The regularization algorithm represents the PSD by a set of triangular basis functions, but it is very time consuming and insensitive to the inversion of the complex refractive index; the linear evaluation method utilizes the linear combination of the optical characteristics of the aerosol to represent the PSD, and can invert the bulk characteristics of the aerosol under certain precision; the permutation search averaging method extracts alternative solutions in the lookup table through different permutation orders to obtain complex refractive index and bulk characteristics, and the process is time-consuming and serious.
The above methods are difficult to obtain high-precision aerosol complex refractive index and single scattering albedo, and often rely on the optical characteristic input of 3 β +2 α to obtain satisfactory micro-physical characteristic inversion results (especially regularization algorithm), which is difficult to implement in most of the current laser radar systems. Particularly in airborne and space-borne lidar system applications.
Disclosure of Invention
Aiming at the defects of inversion of aerosol micro-physical characteristics of the multi-wavelength laser radar, the invention provides a multi-wavelength laser radar aerosol micro-physical characteristic inversion method based on a multi-element full-array random forest, which is based on an improved unsupervised random forest algorithm (RF) and a K-nearest neighbor (KNN) algorithm, aims to solve the problems of high-precision inversion of a CRI of a fine-mode aerosol and inversion of micro-physical characteristics of the aerosol with few laser radar channels (such as a 3 beta +1 alpha structure and a 2 beta +1 alpha structure), and provides reliable input guarantee for SSA inversion of the laser radar.
A multi-wavelength laser radar aerosol micro-physical characteristic inversion method based on a multi-element full-array random forest comprises the following steps:
(1) based on aerosol microReal part of complex refractive index m in physical propertiesrComplex imaginary part m of refractive indexiMode radius rmedConstructing a lookup table G according to the geometric variance sigma; the size of the lookup table G is the aerosol micro-physical property (m)r,mi,rmedσ) number of groups NLUTEach group comprising aerosol micro-physical properties (m)r,mi,rmedσ) and corresponding three-wavelength backscattering coefficient βλAnd extinction coefficient alphaλ;
(2) Input multi-wavelength aerosol optical properties ginputFor the optical characteristics ginputAnd a look-up table G for obtaining normalized optical propertiesAnd normalized look-up table Gnorm(ii) a Wherein the optical characteristics are normalizedIs Nnorm;
(3) Based on K-nearest neighbor theory, calculating normalized lookup table GnormOf the sets of normalized optical properties and the input normalized optical propertiesA deviation D of (A); sorting the obtained deviations D from small to large, and selecting the deviation D with the smallest errorGroup elements as initial look-up tables, ω0To reduce the coefficient, record the new lookup table as G(0);
(4) To pairPerforming a full permutation operation to obtain a product having NnormA search sequence of individual elements; sequentially calculating according to the sequence of each element of the search sequenceAnd searchingThe error d of the aerosol normalization optical characteristic individual corresponding to the table;
based on a K-nearest neighbor theory, utilizing a branch shearing coefficient omega to reduce a feasible solution range in a lookup table, wherein omega belongs to (0, 1); in the search sequence, the feasible solutions of the lookup table obtained after the last element is searched are averaged to obtain the alternative solution (m) of the micro-physical characteristicsr,mi,rmed,σ)retAnd inverted optical properties gret;
(5) Based on random forest theory, randomly generating NRFSearch sequence to obtain NRFIndividual micro-physical property alternative solutionAnd corresponding non-normalized optical propertiesθ=1,2,...NRF(ii) a Averaging the alternative solutions to obtain final inverted micro-physical property resultsAnd non-normalized optical properties
(6) Based on the obtainedAndcalculating to obtain other micro-physical characteristics including effective radiusNumber concentrationSurface area concentrationVolume concentrationAnd mode radius under number concentration distributionThe final obtained micro physical characteristic set is
In the step (1), the three-wavelength backscattering coefficient betaλAnd extinction coefficient alphaλIn (b), λ is a wavelength corresponding to wavelengths of 355nm, 532nm and 1064 nm. The specific process of constructing the lookup table G is as follows:
the correlation between the micro-physical and optical properties of the aerosol is expressed by the Fredholm integral equation:
wherein g is the optical characteristics of backscattering coefficient or extinction coefficient, lambda is the wavelength, Kg(r, λ, m; p) is a volume kernel function, the value of which depends on the complex refractive index m ═ m of the aerosol particlesr+miAnd a particle size range r, p being the shape factor; r ismaxAnd rminRespectively the upper and lower limits of the particle size distribution; v (r) is the volume concentration particle size distribution, expressed as a log normal distribution for fine mode aerosols, as follows:
wherein, VtAs total volume concentration, rmedIs the mode radius, σ is the geometric variance;
the lookup table is built for volume concentration normalization (V)t=1μm3cm-3) Thus by a set of determined fine mode aerosol micro physical characteristic parameters (m)r,mi,rmedσ) the optical properties of the aerosol at the corresponding wavelength λ can be obtained; by using NLUTConstructing a lookup table G by aerosol micro-physical characteristics of group global traversal, wherein the size of G is the group number N of the micro-physical characteristicsLUTRepresenting, each set comprising input aerosol micro-physical properties (m)r,mi,rmedσ) and corresponding three-wavelength backscattering coefficient βλAnd extinction coefficient alphaλ。
In the step (2), the optical characteristics ginputAnd lookup table G, normalized backscattering coefficient and extinction coefficient are expressed as:
wherein,andis the second order norm of the backscattering coefficient and extinction coefficient of different wavelengths; meanwhile, the ratio of extinction coefficient to backscattering of the aerosol is also independent of aerosol number concentration, which is expressed as:
for the 3 β +2 α structure, normalized optical properties were obtained as:
For the 3 β +1 α structure (β:355,532,1064nm, α:532nm), normalized optical properties were obtained as:
For the 2 β +1 α structure (β:355,532nm, α:532nm), normalized optical properties were obtained as:
Respectively to optical characteristics ginputAnd look-up table G performs the above process to obtain normalized optical propertiesAnd look-up table GnormAnd the normalized optical characteristics of both are arranged in the same order.
In the step (3), the deviation D is obtained by calculating the Mahalanobis distance, and the calculation formula is as follows:
In step (4), a compound having N is obtainednormSearch sequence of elements, NnormThe elements are randomly generated and may be repeated.
Sequentially calculating according to the sequence of each element of the search sequenceThe error d of the aerosol normalized optical characteristic individual corresponding to the lookup table is calculated by the following formula:
wherein, # denotes the number of searches,an ith normalized optical property for a kth group element in the look-up table after the # th normalized optical property is reduced; reduced # normalized optical Properties lookup Table G(#)Number of feasible solutions of
In the step (6), the formula for obtaining other micro physical characteristics by calculation is as follows:
in the formula,in terms of the volume concentration, the concentration of the active ingredient,is the mode radius in a number concentration distribution,in terms of a number of concentrations,in terms of the surface area concentration,is the effective radius.
Compared with the existing aerosol micro-physical characteristic inversion algorithm, the method provided by the invention can realize the high-efficiency and accurate inversion of the complex refractive index of the fine-mode aerosol and provide high-precision input for the inversion of the SSA. Meanwhile, the inversion result of the aerosol micro-physical property under fewer laser radar channels (such as 3 beta +1 alpha, 2 beta +1 alpha structures) can be optimized, so that the method has important significance for reducing the hardware cost and expanding the application range of the multi-wavelength laser radar for inverting the aerosol micro-physical property, and provides powerful support for more comprehensively understanding the aerosol property and the effect thereof in climate change.
Drawings
FIG. 1 is a schematic flow diagram of the present invention;
FIG. 2 is a diagram of inversion micro-physics results based on noiseless data in an embodiment of the present invention;
FIG. 3 is a diagram of inversion microphysical property results based on Gaussian noise data in an embodiment of the invention
Detailed Description
The invention will be described in further detail below with reference to the drawings and examples, which are intended to facilitate the understanding of the invention without limiting it in any way.
As shown in fig. 1, a multi-wavelength lidar aerosol micro-physical property inversion method based on a multivariate full-array random forest comprises the following steps:
step S1: complex refractive index real part m based on micro physical propertyrComplex imaginary part of refractive index miMode radius rmedGeometric variance σ, etc. of micro-physical characteristicsAnd constructing a lookup table G.
The correlation between the micro-physical and optical properties of the aerosol can be expressed by the Fredholm integral equation:
wherein g is the optical characteristics such as backscattering coefficient or extinction coefficient, λ is the wavelength, and the common wave bands are 355,532 and 1064 nm. Kg(r, λ, m; p) is a volume kernel function, the value of which depends on the complex refractive index m ═ m of the aerosol particlesr+miAnd the particle size range r, p is the shape factor, the invention takes spherical particles as an example, and can be obtained by Mie scattering theory. r ismaxAnd rminThe upper and lower limits of the particle size distribution, and v (r) the volume concentration Particle Size Distribution (PSD). The particle size distribution of the fine mode aerosol is usually expressed by a lognormal distribution, and the formula is as follows:
wherein, VtAs total volume concentration, rmedIs the mode radius, σ is the geometric variance. The invention establishes volume concentration normalization (V)t=1μm3cm-3) Thus by a set of determined fine mode aerosol micro physical characteristic parameters (m)r,mi,rmedσ) the optical properties of the aerosol at the corresponding wavelength λ are obtained. By using NLUTAnd constructing a lookup table G by the aerosol micro-physical characteristics of the global traversal. Number of groups N of micro physical characteristics for GLUTRepresenting, each set comprising input aerosol micro-physical properties (m)r,mi,rmed,σ,Vt) And corresponding three-wavelength backscattering coefficient betaλAnd extinction coefficient alphaλWhere λ is 355,532,1064 nm.
In this embodiment, the lookup table parameters are: m isr=1.34:0.02:1.66,mi=0:0.001:0.05, rmed=100:10:300nm, ln σ 0.38:0.02:0.5, so NLUT127449. In rice scattering theory, p is 1 and the particle size range r is 0:0.001:50 μm, i.e. rmax=50μm,rmin=0。
Step S2: input multi-wavelength aerosol optical properties ginputFor the optical characteristics ginputAnd a look-up table G to obtain normalized optical propertiesAnd look-up table GnormIn which the optical properties are normalizedIs Nnorm。
Taking the 3 β +2 α structure as an example (β:355,532,1064nm, α:355,532nm), the normalized backscattering coefficient and extinction coefficient are expressed as:
wherein,andis the second order norm of the backscattering coefficient and extinction coefficient at different wavelengths. Meanwhile, the ratio of extinction coefficient to backscattering of the aerosol is also independent of aerosol number concentration, which is expressed as:
for the 3 β +2 α structure, the normalized optical properties are:
For the 3 beta +1 alpha (beta: 355,532,1064nm, alpha: 532nm) structure, the corresponding optical characteristics in the lookup table are selected, and the normalized optical characteristics with the normalized optical characteristics ofNormalized number of optical characteristics Nnorm=6。
For a 2 β +1 α (β:355,532nm, α:532nm) structure, the normalized optical properties areNormalized number of optical characteristics Nnorm=4。
Respectively to optical characteristics ginputAnd look-up table G performs the above process to obtain normalized optical propertiesAnd look-up table GnormAnd the normalized optical characteristics of both are arranged in the same order.
In this embodiment, to verify the universality of the method of the present invention, the optical characteristics generated by the simulation of a plurality of groups of micro physical characteristics are used as input, and the simulation parameters are as follows: m isr=1.35,1.45,1.55,1.65, mi=0.001,0.005,0.01,0.015,0.02,0.025,0.05,rmed100,140,180,240,300nm, ln σ 0.4, and V0.1, yielding 192 sets of multi-wavelength (λ 355,532,1064nm) optical properties. In the present embodiment, there are two sets of test data, one set of test data is noise-free, and the other set of test data is randomly added with gaussian noise, where the noise level is 20%, and in the present embodiment, it represents that the noise level reaches 20% at a position with three times of standard deviation of gaussian distribution. The two groups of observation data are respectively input into a 3 beta +2 alpha structure, a 3 beta +1 alpha structure (beta: 355,532,1064nm, alpha: 532nm) and a 2 beta +1 alpha structure (beta: 355,532nm, alpha: 532nm) for method test.
Step S3: based on K-nearest neighbor theory, calculatingNormalized optical propertiesAnd GnormAnd the deviation D of each group of normalized optical characteristics is obtained by calculating the Mahalanobis distance, and the calculation formula is as follows:
wherein,for look-up table GnormThe kth group element. And S is a corresponding covariance matrix. Sorting the obtained deviations D from small to large, and selecting the error with the minimumGroup elements as initial look-up tables, ω0To reduce the coefficient, record the new lookup table as G(0)(ii) a In this embodiment, ω0=0.1。
Step S4: to pairPerforming a full permutation operation to obtain a product having NnormSearch sequence of elements, NnormThe elements are randomly generated and may be repeated. Sequentially calculating the correspondence according to the sequence of each element in the search sequenceThe error d of the aerosol normalized optical characteristic individual corresponding to the lookup table is calculated by the following formula:
wherein, # denotes the number of searches,for # normalized lightThe ith normalized optical property of the kth group element in the look-up table after the reduction of the optical property. Based on the K-nearest neighbor theory, the feasible solution range in the lookup table is reduced by utilizing a branch-cut coefficient omega, and omega belongs to (0, 1). Thus, the # normalized optical property reduced look-up table G(#)Number of feasible solutions ofAveraging the reduced lookup table obtained after searching the last element of the search sequence to obtain the alternative solution (m) of the micro-physical characteristicsr,mi,rmed,σ)retAnd inverted optical properties gret. In this embodiment, ω is 0.3.
Step S5: based on random forest theory, randomly generating NRFSearch sequence to obtain NRFIndividual micro-physical property alternative solutionAnd corresponding non-normalized optical propertiesθ=1,2,...NRF. Averaging the alternative solutions to obtain final inverted micro-physical property resultsAnd non-normalized optical propertiesIn this example, NRF=500。
Step S6: based on the obtainedAndcalculating to obtain the effective radiusNumber concentrationSurface area concentrationVolume concentrationAnd other micro-physical characteristics. The specific calculation process is as follows:
wherein,is the mode radius in the number concentration distribution. The final set of available microphysical properties is therefore
As shown in fig. 2, (a) - (d) respectively represent absolute error of real part of complex refractive index, absolute error of imaginary part of complex refractive index, relative error of volume concentration inversion, and relative error of effective radius inversion when three optical characteristic structures of 3 β +2 α,3 β +1 α, and 2 β +1 α are input. As the number of input optical characteristics decreases, the inversion errors of the real part of the complex refractive index, the imaginary part, the volume concentration, and the effective radius gradually increase. Under a 3 beta +2 alpha structure, the average value of the absolute errors of the real part of the complex refractive index obtained by the method is 0.016 (<0.05), the average value of the absolute errors of the imaginary part is 0.0019, and the corresponding relative errors are 0.36(<0.5), so that the errors are obviously reduced compared with the error of the conventional algorithm, and the method can obtain a more accurate complex refractive index inversion result. Meanwhile, under three input optical characteristic structures, the maximum values of inversion relative errors of the volume concentration and the effective radius are respectively 26% and 18%, which shows that the method can be applied to fewer optical characteristic channels and has important significance for reducing hardware cost and expanding application range of the multi-wavelength laser radar for inverting the micro physical characteristics of the aerosol.
As shown in fig. 3, (a) - (d) respectively represent absolute error of real part of complex refractive index, absolute error of imaginary part of complex refractive index, relative error of volume concentration inversion, and relative error of effective radius inversion when three optical characteristic structures of 3 β +2 α,3 β +1 α, and 2 β +1 α are input. Under the condition of introducing 20% of Gaussian noise, under a 3 beta +2 alpha structure, the absolute error of the real part of the complex refractive index obtained by the invention can still be less than 0.05, and the relative errors of the volume concentration and the effective radius are respectively 16% and 8%. The method is applied to other input optical characteristic structures, and shows better anti-noise capability on inversion of several micro-physical characteristics, particularly on volume concentration and effective radius, and the maximum relative errors of the method are respectively less than 34% and 29%, so that the method has the potential of inverting the micro-physical characteristics of the aerosol under fewer laser radar channels and has better anti-noise capability.
The embodiments described above are intended to illustrate the technical solutions and advantages of the present invention, and it should be understood that the above-mentioned embodiments are only specific embodiments of the present invention, and are not intended to limit the present invention, and any modifications, additions and equivalents made within the scope of the principles of the present invention should be included in the scope of the present invention.
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Cited By (1)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| CN118584504A (en) * | 2024-05-27 | 2024-09-03 | 武汉大学 | A multi-wavelength lidar aerosol microphysical characteristics inversion method and system |
Citations (6)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| DE102008003037B3 (en) * | 2008-01-02 | 2009-09-24 | Leibniz-Institut für Troposphärenforschung e. V. | Method for determining physical characteristics of atmospheric particles, involves preparing vertical profile of optical characteristic of particles and determining vertical profile of physical characteristic of particle by inversion method |
| CN109086801A (en) * | 2018-07-06 | 2018-12-25 | 湖北工业大学 | A kind of image classification method based on improvement LBP feature extraction |
| CN109884664A (en) * | 2019-01-14 | 2019-06-14 | 武汉大学 | A method and system for optical microwave synergistic inversion of urban above-ground biomass |
| CN110161532A (en) * | 2019-05-30 | 2019-08-23 | 浙江大学 | A method of based on multi-wavelength laser radar inverting microfluidic aerosol physical characteristic |
| CN110488252A (en) * | 2019-08-08 | 2019-11-22 | 浙江大学 | Overlap factor calibration device and calibration method for a ground-based aerosol lidar system |
| CA3146697A1 (en) * | 2019-08-06 | 2021-02-11 | Amgen Inc. | Systems and methods for determining protein concentrations of unknown protein samples based on automated multi-wavelength calibration |
-
2021
- 2021-12-28 CN CN202111623849.0A patent/CN114488198A/en active Pending
Patent Citations (6)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| DE102008003037B3 (en) * | 2008-01-02 | 2009-09-24 | Leibniz-Institut für Troposphärenforschung e. V. | Method for determining physical characteristics of atmospheric particles, involves preparing vertical profile of optical characteristic of particles and determining vertical profile of physical characteristic of particle by inversion method |
| CN109086801A (en) * | 2018-07-06 | 2018-12-25 | 湖北工业大学 | A kind of image classification method based on improvement LBP feature extraction |
| CN109884664A (en) * | 2019-01-14 | 2019-06-14 | 武汉大学 | A method and system for optical microwave synergistic inversion of urban above-ground biomass |
| CN110161532A (en) * | 2019-05-30 | 2019-08-23 | 浙江大学 | A method of based on multi-wavelength laser radar inverting microfluidic aerosol physical characteristic |
| CA3146697A1 (en) * | 2019-08-06 | 2021-02-11 | Amgen Inc. | Systems and methods for determining protein concentrations of unknown protein samples based on automated multi-wavelength calibration |
| CN110488252A (en) * | 2019-08-08 | 2019-11-22 | 浙江大学 | Overlap factor calibration device and calibration method for a ground-based aerosol lidar system |
Non-Patent Citations (2)
| Title |
|---|
| 李晓涛: "大气气溶胶粒径分布的多波长激光雷达反演", 《光学学报》, vol. 44, no. 06, 8 April 2024 (2024-04-08), pages 165 - 172 * |
| 赵双;陈曙晖;: "基于机器学习的流量识别技术综述与展望", 计算机工程与科学, no. 10, 15 October 2018 (2018-10-15), pages 34 - 44 * |
Cited By (1)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| CN118584504A (en) * | 2024-05-27 | 2024-09-03 | 武汉大学 | A multi-wavelength lidar aerosol microphysical characteristics inversion method and system |
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