CN109507072A - A kind of fine particle turbulent flux measurement method - Google Patents

A kind of fine particle turbulent flux measurement method Download PDF

Info

Publication number
CN109507072A
CN109507072A CN201811376291.9A CN201811376291A CN109507072A CN 109507072 A CN109507072 A CN 109507072A CN 201811376291 A CN201811376291 A CN 201811376291A CN 109507072 A CN109507072 A CN 109507072A
Authority
CN
China
Prior art keywords
visibility
fine particle
pulsation
aerosol
light scattering
Prior art date
Legal status (The legal status is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the status listed.)
Granted
Application number
CN201811376291.9A
Other languages
Chinese (zh)
Other versions
CN109507072B (en
Inventor
任燕
张宏昇
鞠婷婷
康凌
蔡旭辉
宋宇
高迎鹏
王鹏飞
张仁健
武云飞
Current Assignee (The listed assignees may be inaccurate. Google has not performed a legal analysis and makes no representation or warranty as to the accuracy of the list.)
Peking University
Original Assignee
Peking University
Priority date (The priority date is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the date listed.)
Filing date
Publication date
Application filed by Peking University filed Critical Peking University
Priority to CN201811376291.9A priority Critical patent/CN109507072B/en
Publication of CN109507072A publication Critical patent/CN109507072A/en
Application granted granted Critical
Publication of CN109507072B publication Critical patent/CN109507072B/en
Active legal-status Critical Current
Anticipated expiration legal-status Critical

Links

Classifications

    • GPHYSICS
    • G01MEASURING; TESTING
    • G01NINVESTIGATING OR ANALYSING MATERIALS BY DETERMINING THEIR CHEMICAL OR PHYSICAL PROPERTIES
    • G01N15/00Investigating characteristics of particles; Investigating permeability, pore-volume, or surface-area of porous materials
    • G01N15/06Investigating concentration of particle suspensions
    • G01N15/075

Abstract

The invention discloses a kind of fine particle turbulent flux measurement methods.The sample frequency that the present invention passes through raising measurement of extinction coefficient instrument, obtain the light scattering extinction of the aerosol of high frequency, and under conditions of low visibility, according to there are approximate power exponent relationships between the mass concentration and visibility of fine particle, it is pulsed using the mass concentration that instantaneous visibility pulses to obtain fine particle, vertical speed pulsation is obtained in conjunction with ultrasonic wind-warm syndrome instrument measurement, obtains fine particle turbulent flux;The present invention is pulsed by the mass concentration of extinction coefficient pulsation inverse fine particle, finally finds out fine particle turbulent flux using eddy-correlation technique, is solved the problems, such as the mass concentration pulsation of fine particle and its acquisition of turbulent flux for the first time, is provided basis for Forecast Mode;And easy to operate, exploitativeness is strong, can be mating with existing water and heat observation system, can also be separately formed observation system, and observation data processing is mature.

Description

A kind of fine particle turbulent flux measurement method
Technical field
The invention belongs to air pollution meteorology fields, and in particular to a kind of measurement method of fine particle turbulent flux.
Background technique
In Atmospheric Survey, measurement of extinction coefficient instrument obtains extinction coefficient, measurement of extinction coefficient by measurement scattered light intensity Instrument is designed using the principle of forward scattering.Measurement of extinction coefficient instrument transmitter emits big in infrared-ray measurement sampling volume The scattered light intensity of gas effectively calculates extinction coefficient by scattered light intensity.It is limited by measurement accuracy, measurement of extinction coefficient instrument High frequency sampled data cannot be obtained, the sampling time is at the soonest only up to 1 minute.But such sample frequency is for obtaining The dither and progress turbulent flow analysis of extinction coefficient and the calculating of corresponding turbulent flux are far from being enough.
In the prior art, the basic skills obtained for turbulent flux has: eddy-correlation technique, Bowen specific energy balancing method And Aerodynamic Method.Wherein, eddy-correlation technique meets the original definition of turbulent flux, and principle is rigorous, simple direct.But it needs The turbulence pulsation sensor for wanting high-precision, response speed to be exceedingly fast.Since there is presently no the quality for directly obtaining fine particle is dense The instrument of high-frequency data is spent, so just fine particle turbulent flux can not be calculated using eddy-correlation technique.
Summary of the invention
In order to solve the problems, such as directly acquiring for fine particle turbulent flux, it is logical that the invention proposes a kind of fine particle turbulent flows The measurement method of amount.
The measurement method of fine particle turbulent flux of the invention, comprising the following steps:
1) the sample frequency f for improving measurement of extinction coefficient instrument, obtains the light scattering extinction b of the aerosol of high frequencyspi, i= 1,2,3 ... ..., N, N are number of samples, are natural number, bspiFor the light scattering extinction of the aerosol of sampled point i;
2) to the light scattering extinction b of the aerosol of high frequencyspReynolds decomposition is done, the light scattering extinction arteries and veins of aerosol is obtained It is dynamic:Mean value of the light scattering extinction of aerosol in a period of time;
3) since the absorption delustring and the absorption delustring of atmospheric molecule of aerosol are smaller, with the light scattering extinction of aerosol The extinction coefficient total as atmosphere obtains the visibility v of sampled point ii:
vi=3.912/bspi
Obtain visibility pulsation For visibility a period of time mean value;
4) spectrum analysis is done into the light scattering extinction pulsation of aerosol and visibility pulsation, is obtained using Fourier transformation Extinction coefficient composes Sb(n) and visibility composes Sv(n);
5) theoretical according to turbulent flow Kolmogorov husband, the light scattering extinction and visibility of aerosol are as scalar, spectrum Function Sb(n) and Sv(n) meet -2/3 power relationship in inertia secondary area between frequency n, and the spectral line place of upwarping is on spectrogram For noise signal, to obtain frequency n where noise signal;
6) according to Fourier transformation relationship, it will be less than the data reconstruction of frequency n, the scattering for the aerosol that obtains that treated disappears Backscatter extinction logarithmic ratio pulsation and visibility pulsation, the data obtained since then are exactly to remove the visibility pulsation V ' of the true high frequency of noise;
7) particulate matter continuous meter measures mean value of the mass concentration in a period of time of fine particleIn low visibility Under conditions of, there are approximate power exponent relationships between the mass concentration and visibility of fine particle:
Wherein,For mean value of the visibility in a period of time of true high frequency, a and b are an abnormal low visibility event Fitting coefficient obtains fitting coefficient a and b by nonlinear fitting according to above formula;
8) the mass concentration pulsation C ' of fine particle is obtained by visibility pulsation V ':
9) vertical speed pulsation w ' is obtained by ultrasound wind-warm syndrome instrument measurement;
10) eddy-correlation technique is utilized, by the mass concentration pulsation C ' and vertical speed pulsation w ' of fine particle, is obtained thin Particulate matter turbulent flux F:
Wherein, in step 1), the sample frequency f of the light scattering extinction of aerosol is 1~5HZ.Number of samples N with adopt Sample frequency f is related, in the range of 1200f~3600f.
In step 3), low visibility refers to visibility at 5 kilometers or less.
Step 2), 3) and 7) in, be for a period of time 20~60min.
Advantages of the present invention:
The present invention obtains the scattering delustring system of the aerosol of high frequency by the sample frequency of raising measurement of extinction coefficient instrument Number, and under conditions of low visibility, according to there are approximate power exponent passes between the mass concentration and visibility of fine particle System is pulsed to obtain the mass concentration pulsation C ' of fine particle using instantaneous visibility, be hung down in conjunction with ultrasonic wind-warm syndrome instrument measurement Straight velocity fluctuation w ', obtains fine particle turbulent flux F;The present invention improves the sample frequency of extinction coefficient, is calculated with reaching The requirement of turbulent flux is pulsed by the mass concentration of extinction coefficient pulsation inverse fine particle, is finally asked using eddy-correlation technique Fine particle turbulent flux out solves the problems, such as the mass concentration pulsation of fine particle and its acquisition of turbulent flux for the first time, is Forecast Mode provides basis;And easy to operate, exploitativeness is strong, can be mating with existing water and heat observation system, can also be single Observation system is solely constituted, observation data processing is mature.
Detailed description of the invention
Fig. 1 (a) and (b) are respectively that two embodiments of the measurement method of fine particle turbulent flux according to the present invention obtain The mass concentration correlativity schematic diagram of the visibility and fine particle arrived;
Fig. 2 is that obtain a abnormal low visibility event for the measurement method of fine particle turbulent flux according to the present invention is general Condition figure, wherein (a) is the mass concentration time series chart of fine particle, (b) is visibility time series chart, (c) for than wet Time series chart (d) is horizontal wind speed time series chart;
Fig. 3 is the fine particle that one embodiment of the measurement method of fine particle turbulent flux according to the present invention obtains Mass concentration, turbulent flux and vertical speed time series chart, wherein (a) be fine particle mass concentration time sequence Column figure, (b) is turbulent flux time series chart, (c) is the time series chart of vertical speed;
Fig. 4 is the fine grained that another embodiment of the measurement method of fine particle turbulent flux according to the present invention obtains The time series chart of the mass concentration of object, turbulent flux and vertical speed, wherein (a) be the mass concentration of fine particle when Between sequence chart, (b) be turbulent flux time series chart, (c) be vertical speed time series chart;
Fig. 5 is the matter for the fine particle that the embodiment of the measurement method of fine particle turbulent flux according to the present invention obtains The frequency spectrum of concentration is measured with the distribution map of stable current field;
Fig. 6 is the flow chart of the measurement method of fine particle turbulent flux of the invention.
Specific embodiment
With reference to the accompanying drawing, by specific embodiment, the present invention is further explained.
Studies have shown that atmospheric visibility is research shows that the decline of atmospheric visibility is mainly brought by Particulate Pollution, The light scattering extinction of particulate matter accounts for the 70%~80% of overall extinction coefficient.Furtherly, the decline of atmospheric visibility is main It is caused by the scattering delustring of particulate matter, and the mass concentration of fine particle is the Main Factors for determining visibility quality, There are certain nonlinear correlations for visibility and the low visibility level of fine particle, as shown in Figure 1, wherein (a) is 27 days 2 months Visibility and fine particle mass concentration C correlativity schematic diagram, (b) for March 3 visibility and fine particle matter Measure concentration correlativity schematic diagram.
By taking the low visibility weather event typical twice that 2 months 2018 on March 5th, 25 days 1 occurred as an example, this The overview of continuous abnormal low visibility event twice, as shown in Figure 2, wherein (a) is the mass concentration time series of fine particle Figure (b) is visibility time series chart, (c) than wet time series chart (d) to be horizontal wind speed time series chart.This two It is selected in secondary abnormal low visibility event 27 days 2 months and visibility in two days on the 3rd March is less than for 5km, meet the requirement of low visibility.
The measurement method of the fine particle turbulent flux of the present embodiment, as shown in Figure 6, comprising the following steps:
1) the sample frequency f for improving measurement of extinction coefficient instrument, obtains the light scattering extinction b of the aerosol of high frequencyspi, i= 1,2,3 ... ..., N, bspiFor the light scattering extinction of the aerosol of sampled point i, the sample integration time is 1s;
2) to the light scattering extinction b of the aerosol of high frequencyspReynolds decomposition is done, the light scattering extinction arteries and veins of aerosol is obtained It is dynamic:Mean value of the light scattering extinction of aerosol in 30min;
3) since the absorption delustring and the absorption delustring of atmospheric molecule of aerosol are smaller, with the scattering delustring system of aerosol The number extinction coefficient total as atmosphere, obtains sampled point i visibility vi
vi=3.912/bspi
Obtain visibility pulsationviFor the visibility of sampled point i,For visibility 30min mean value;
4) spectrum analysis is done into the light scattering extinction pulsation of aerosol and visibility pulsation, is obtained using Fourier transformation Extinction coefficient composes Sb(n) and visibility composes Sv(n);
5) according to turbulent flow Kolmogorov husband (K41) theory, the light scattering extinction of aerosol and visibility as scalar, Its spectral function Sb(n) and Sv(n) meet -2/3 power relationship in inertia secondary area between frequency n, and spectral line upwarps on spectrogram Place is noise signal, to obtain frequency n where noise signal;
6) data of frequency n be will be less than according to Fourier transformation relationship, the scattering of reconstruct obtains that treated aerosol disappears Backscatter extinction logarithmic ratio pulsation and visibility, the data obtained since then are exactly to remove the pulsation visibility V ' of the true high frequency of noise;
7) particulate matter continuous meter is measured as mean value of the mass concentration in a period of time of fine particleSee in low energy Under conditions of degree, there are approximate power exponent relationships between the mass concentration and visibility of fine particle:
Wherein,For mean value of the visibility in a period of time of true high frequency, fitting coefficient is obtained by nonlinear fitting A and b, as shown in Figure 1;
8) the mass concentration pulsation C of fine particle is obtained by visibility pulsation V ':
9) vertical speed pulsation w ' is obtained by ultrasound wind-warm syndrome instrument measurement, sample frequency is respectively 10HZ;
10) turbulent flow eddy-correlation technique is utilized, by the mass concentration pulsation C ' and vertical speed pulsation w ' of fine particle, is obtained To fine particle turbulent flux F:
It obtains shown in fine particle turbulent flux time series such as Fig. 3 (b) and 4 (b).
In Fig. 3, (a) is the time series chart of the mass concentration of fine particle, (b) is turbulent flux time series chart, (c) For the time series chart of vertical speed.In Fig. 4, (a) is the time series chart of the mass concentration of fine particle, (b) logical for turbulent flow The time series chart of amount is (c) time series chart of vertical speed.
Meanwhile the mass concentration frequency spectrum of fine particle has also been obtained with the variation of stable current field, as shown in figure 5, it becomes Change meets K41 theory, also demonstrates the reasonability that the present invention calculates fine particle turbulent flux using turbulent flow eddy-correlation technique.
It is finally noted that the purpose for publicizing and implementing example is to help to further understand the present invention, but this field Technical staff be understood that without departing from the spirit and scope of the invention and the appended claims, it is various replacement and repair It is all possible for changing.Therefore, the present invention should not be limited to embodiment disclosure of that, and the scope of protection of present invention is to weigh Subject to the range that sharp claim defines.

Claims (5)

1. a kind of measurement method of fine particle turbulent flux, which is characterized in that the measurement method the following steps are included:
1) the sample frequency f for improving measurement of extinction coefficient instrument, obtains the light scattering extinction b of the aerosol of high frequencyspi, i=1,2, 3 ... ..., N, N are number of samples, are natural number, bspiFor the light scattering extinction of the aerosol of sampled point i;
2) to the light scattering extinction b of the aerosol of high frequencyspReynolds decomposition is done, the light scattering extinction pulsation of aerosol is obtained: Mean value of the light scattering extinction of aerosol in a period of time;
3) since the absorption delustring and the absorption delustring of atmospheric molecule of aerosol are smaller, using the light scattering extinction of aerosol as The total extinction coefficient of atmosphere obtains the visibility v of sampled point ii:
vi=3.912/bspi
Obtain visibility pulsation For visibility a period of time mean value;
4) spectrum analysis is done into the light scattering extinction pulsation of aerosol and visibility pulsation, obtains delustring using Fourier transformation Coefficient spectrum Sb(n) and visibility composes Sv(n);
5) theoretical according to turbulent flow Kolmogorov husband, the light scattering extinction and visibility of aerosol are as scalar, spectral function Sb (n) and Sv(n) meet -2/3 power relationship in inertia secondary area between frequency n, and the spectral line place of upwarping is to make an uproar on spectrogram Acoustical signal, to obtain frequency n where noise signal;
6) according to Fourier transformation relationship, it will be less than the data reconstruction of frequency n, the scattering delustring system for the aerosol that obtains that treated Rapid pulse is dynamic and visibility pulsation, the data obtained since then are exactly to remove the visibility pulsation V ' of the true high frequency of noise;
7) particulate matter continuous meter measures mean value of the mass concentration in a period of time of fine particleIn the item of low visibility Under part, there are approximate power exponent relationships between the mass concentration and visibility of fine particle:
Wherein,For mean value of the visibility in a period of time of true high frequency, a and b are the fitting of an abnormal low visibility event Coefficient obtains fitting coefficient a and b by nonlinear fitting according to above formula;
8) the mass concentration pulsation C ' of fine particle is obtained by visibility pulsation V ':
9) vertical speed pulsation w ' is obtained by ultrasound wind-warm syndrome instrument measurement;
10) eddy-correlation technique is utilized, by the mass concentration pulsation C ' and vertical speed pulsation w ' of fine particle, obtains fine grained Object turbulent flux F:
2. measurement method as described in claim 1, which is characterized in that in step 1), the light scattering extinction of aerosol Sample frequency f is 1~5HZ.
3. measurement method as described in claim 1, which is characterized in that in step 1), the range of number of samples be 1200f~ 3600f。
4. measurement method as described in claim 1, which is characterized in that in step 3), low visibility refers to visibility 5 Kilometer or less.
5. measurement method as described in claim 1, which is characterized in that step 2), 3), 7) He 8) in, for a period of time for 20~ 60min。
CN201811376291.9A 2018-11-19 2018-11-19 Fine particle turbulent flux measurement method Active CN109507072B (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
CN201811376291.9A CN109507072B (en) 2018-11-19 2018-11-19 Fine particle turbulent flux measurement method

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
CN201811376291.9A CN109507072B (en) 2018-11-19 2018-11-19 Fine particle turbulent flux measurement method

Publications (2)

Publication Number Publication Date
CN109507072A true CN109507072A (en) 2019-03-22
CN109507072B CN109507072B (en) 2020-09-08

Family

ID=65749097

Family Applications (1)

Application Number Title Priority Date Filing Date
CN201811376291.9A Active CN109507072B (en) 2018-11-19 2018-11-19 Fine particle turbulent flux measurement method

Country Status (1)

Country Link
CN (1) CN109507072B (en)

Cited By (2)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN110057731A (en) * 2019-04-09 2019-07-26 哈尔滨工业大学 Based on laser beam Intensity Analysis oceanic turbulence and particle cognitive method and device
CN110296912A (en) * 2019-06-19 2019-10-01 北京理工大学 The detection system and method for dust cloud cluster dispersion ability Turbulent Kinetic based on ultrasound

Citations (9)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
SU1529908A1 (en) * 1988-02-19 1995-11-20 Всесоюзный Научно-Исследовательский Институт Молекулярной Биологии Method of determination of sizes and concentration of aerosol particles
CN1587987A (en) * 2004-08-13 2005-03-02 赵凤生 Method for obtaining near ground layer sand dust particle quantity deep time-space distribution
CN102539336A (en) * 2011-02-01 2012-07-04 环境保护部卫星环境应用中心 Method and system for estimating inhalable particles based on HJ-1 satellite
CN104833979A (en) * 2015-04-27 2015-08-12 北京航天控制仪器研究所 Laser ranging method and laser ranging data signal processing method
CN105067534A (en) * 2015-07-25 2015-11-18 中国科学院合肥物质科学研究院 Pollutant transport flux measurement and calculation method based on ground-based MAX-DOAS
CN105158210A (en) * 2015-08-31 2015-12-16 中国科学技术大学 Method and system for measuring atmospheric aerosol mass vertical conveying flux
CN106126903A (en) * 2016-06-21 2016-11-16 北京市环境保护监测中心 The computational methods of PM2.5 three-dimensional transport fluxes and device
DE102017001436A1 (en) * 2017-02-15 2018-08-16 Paragon Ag Particle measuring apparatus and method of operating the same
CN108469281A (en) * 2018-01-18 2018-08-31 天津大学 Two-phase Research on vortex signal processing based on EMD and Spectrum Correction

Patent Citations (9)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
SU1529908A1 (en) * 1988-02-19 1995-11-20 Всесоюзный Научно-Исследовательский Институт Молекулярной Биологии Method of determination of sizes and concentration of aerosol particles
CN1587987A (en) * 2004-08-13 2005-03-02 赵凤生 Method for obtaining near ground layer sand dust particle quantity deep time-space distribution
CN102539336A (en) * 2011-02-01 2012-07-04 环境保护部卫星环境应用中心 Method and system for estimating inhalable particles based on HJ-1 satellite
CN104833979A (en) * 2015-04-27 2015-08-12 北京航天控制仪器研究所 Laser ranging method and laser ranging data signal processing method
CN105067534A (en) * 2015-07-25 2015-11-18 中国科学院合肥物质科学研究院 Pollutant transport flux measurement and calculation method based on ground-based MAX-DOAS
CN105158210A (en) * 2015-08-31 2015-12-16 中国科学技术大学 Method and system for measuring atmospheric aerosol mass vertical conveying flux
CN106126903A (en) * 2016-06-21 2016-11-16 北京市环境保护监测中心 The computational methods of PM2.5 three-dimensional transport fluxes and device
DE102017001436A1 (en) * 2017-02-15 2018-08-16 Paragon Ag Particle measuring apparatus and method of operating the same
CN108469281A (en) * 2018-01-18 2018-08-31 天津大学 Two-phase Research on vortex signal processing based on EMD and Spectrum Correction

Non-Patent Citations (4)

* Cited by examiner, † Cited by third party
Title
REN, YAN, ET AL.: "Determining the fluctuation of PM2.5 mass concentration and its applicability to Monin-Obukhov similarity", 《SCIENCE OF THE TOTAL ENVIRONMENT》 *
安俊岭,等: "京津冀污染物跨界输送通量模拟", 《环境科学学报》 *
宋宇,等: "北京市能见度下降与颗粒物污染的关系", 《环境科学学报》 *
方雪,等: "一次连续沙尘过程中沙尘气溶胶的垂直传输特征", 《兰州大学学报:自然科学版》 *

Cited By (3)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN110057731A (en) * 2019-04-09 2019-07-26 哈尔滨工业大学 Based on laser beam Intensity Analysis oceanic turbulence and particle cognitive method and device
CN110296912A (en) * 2019-06-19 2019-10-01 北京理工大学 The detection system and method for dust cloud cluster dispersion ability Turbulent Kinetic based on ultrasound
CN110296912B (en) * 2019-06-19 2020-07-21 北京理工大学 System and method for detecting dust cloud cluster diffusion dynamic turbulent flow energy based on ultrasound

Also Published As

Publication number Publication date
CN109507072B (en) 2020-09-08

Similar Documents

Publication Publication Date Title
Agrawal et al. Laser diffraction particle sizing in STRESS
Finkelstein et al. Sampling error in eddy correlation flux measurements
Williams et al. Microscale temperature and velocity spectra in the atmospheric boundary layer
Kunkel et al. Study of the near-wall-turbulent region of the high-Reynolds-number boundary layer using an atmospheric flow
Cava et al. Analysis of short-term closure of the surface energy balance above short vegetation
CN103942439B (en) Inhalable particle concentration estimating method based on meteorological observation data
Brown et al. On the attenuation of sound by turbulence
Wolff et al. Aerodynamic gradient measurements of the NH 3-HNO 3-NH 4 NO 3 triad using a wet chemical instrument: an analysis of precision requirements and flux errors
CN106383207A (en) Computing method applied to atmospheric aerosol mass concentration horizontal route distribution
CN106443708A (en) Atmospheric particulate monitoring lidar data processing method
CN104792672A (en) Height distribution detection device and method for PM2.5 mass concentration
CN108959705B (en) Method for predicting subtropical forest biomass
CN107808054A (en) A kind of sediment resuspension model building method based on field inspection
CN109507072A (en) A kind of fine particle turbulent flux measurement method
Bosveld Derivation of fluxes from profiles over a moderately homogeneous forest
CN103234882A (en) Method for inverting mass concentration of atmospheric particulates based on flight time of particulates
Gallagher et al. Ozone deposition to coastal waters
Lyu et al. High-order statistics of temperature fluctuations in an unstable atmospheric surface layer over grassland
CN106706566B (en) A kind of calculation method of laser radar detection SEQUENCING VERTICAL visibility
CN106932607B (en) Method and device for simply and conveniently judging influence of wind measurement data on shielding of wind measurement tower body
Poggio et al. Scintillometer wind measurements over complex terrain
Mazzarella An inventory of specifications for wind measuring instruments
Garcıa-Garcıa et al. Fine-scale measurements of fog-droplet concentrations: A preliminary assessment
CN105158210B (en) A kind of measuring method and system of atmospheric aerosol quality vertical transport flux
Eichinger et al. The application of a scanning, water Raman-lidar as a probe of the atmospheric boundary layer

Legal Events

Date Code Title Description
PB01 Publication
PB01 Publication
SE01 Entry into force of request for substantive examination
SE01 Entry into force of request for substantive examination
GR01 Patent grant
GR01 Patent grant