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Vol 32, No 2 (2019)

Optical Waves Propagation

The Effect of Phase Aberrations on the Position and Length of the Filamentation Domain

Apeksimov D.V., Geints Y.E., Zemlyanov A.A., Iglakova A.N., Kabanov A.M., Kuchinskaya O.I., Matvienko G.G., Oshlakov V.K., Petrov A.V.

Abstract

The results of experimental and theoretical studies of femtosecond laser pulse filamentation with use of a bimorph deformable mirror are presented. The mirror allows controlling the position of the filamentation domain throughout a model path due to phase distortions of different parts of a laser beam, determining localization of filaments and high-intensity channels in a beam cross section, and forming long (>100 m) high-intensity (1011–1012 W/cm2) weakly diverging plasma-free channels.

Atmospheric and Oceanic Optics. 2019;32(2):109-116
pages 109-116 views

Extinction Matrix of Atmospheric Ice Crystals with Their Preferred Spatial Orientation for the Visible and IR Regions

Kustova N.V., Konoshonkin A.V., Timofeev D.N., Shishko V.A.

Abstract

The extinction matrix for an ensemble of hexagonal ice plates and columns is presented. The extinction matrix for droxtal and bullet crystals has been estimated. The calculations have been carried out for particles with characteristic dimensions from 10 to 100 μm and wavelengths from 0.3 to 10 μm assuming a gamma distribution of particle size with a width parameter μ < 4. It has been found that the extinction matrix of an ensemble of atmospheric ice crystals in the visible wavelength region is a unit matrix with a coefficient equal to the doubled area of the particle projection. The error of this representation does not exceed tenths of a percent and does not depend on the type of crystals and their spatial orientation. It has also been found that such a representation of the extinction matrix in the IR region is possible only for hexagonal columns, bullets, and similar crystals with a characteristic size greater than 20 μm for wavelengths less than 8 μm.

Atmospheric and Oceanic Optics. 2019;32(2):117-123
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Spectroscopy of Ambient Medium

LED-Based Fourier-Transform Spectroscopy: HD16O Absorption Spectrum in 0.6-μm Spectral Region

Sinitsa L.N., Serdyukov V.I., Polovtseva E.R., Bykov A.D.

Abstract

A high-resolution vibrational-rotational absorption spectrum of НD16О molecule has been studied in the visible region from 16 600 to 17 400 cm–1 using LED-based Fourier-transform spectroscopy. The spectrum was recorded using a IFS-125M Fourier-transform spectrometer with a resolution of 0.09 cm−1. A high-brightness 3HP LED was used as a source of radiation. For the measurements, we used a White-type multipass cell with an optical path length of 2880 cm. The spectral line parameters (line centers and intensities) were derived from the spectral analysis. The linelist contains more than 300 transitions to (005) and (104) vibrational states. The results obtained have been compared with the calculated and experimental data of other authors.

Atmospheric and Oceanic Optics. 2019;32(2):124-127
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Optics of Clusters, Aerosols, and Hydrosoles

Variability in Parameters of the Near-Surface Aerosol Microstructure in Summer According to Results of Inversion of Measurements of Spectral Extinction of Light on a Horizontal Path in Tomsk: Part I–Geometrical Cross Section of Fine and Coarse Particles

Veretennikov V.V., Men’shchikova S.S., Uzhegov V.N.

Abstract

Results on retrieving parameters of the near-surface aerosol microstructure from spectral measurements of the coefficient of aerosol extinction of light in summer are presented. The experimental data have been obtained using an atmospheric transmittance meter at 11 wavelengths in the range 0.45–3.91 μm on a horizontal path near Tomsk. The inverse problem was solved using a numerical algorithm based on the integral distribution method. In the first part of the work, the variability of the geometrical cross section of particles from the fine fraction, coarse fraction, and total ensemble is analyzed. The effect of the smoke pollution of the atmosphere on variations in microstructure parameters has been considered. It has been shown that the main contribution (73–77%) to the total cross section of near-surface aerosol is made by particles of the fine fraction. Coefficients of variation in the cross sections of particles on monthly intervals without regard to the influence of smokes are high within 53–61% for the fine fraction and 53–69% for the coarse fraction of aerosol. The correlations between the aerosol extinction coefficients at different wavelengths and retrieved parameters of the aerosol microstructure have been studied.

Atmospheric and Oceanic Optics. 2019;32(2):128-137
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Variability in Parameters of the Near-Surface Aerosol Microstructure in Summer according to Results of Inversion of Measurements of Spectral Extinction of Light on a Horizontal Path in Tomsk: Part II–Volume Concentration and Mean Radius of Particles

Veretennikov V.V., Men’shchikova S.S., Uzhegov V.N.

Abstract

The variability of the volume concentration and mean radius of particles of the fine and coarse fractions of surface aerosol in summer has been studied from the results of solution of the inverse problem for spectral measurements of the aerosol extinction coefficient. It has been shown that the main contribution (80%) to the total volume of near-surface aerosol is made by particles of the coarse fraction. The mean radius of fine particles varies from 0.08 to 0.25 μm. The variation range of the mean radius of coarse aerosol is 1.06–3 μm. The influence of atmosphere smokiness on variations in microstructure parameters is considered. The variability of retrieved microstructure parameters of near-surface aerosol is compared with similar results obtained from solar photometry data.

Atmospheric and Oceanic Optics. 2019;32(2):138-146
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Statistical Model of Cloud Optical Depths in Certain Zones of the Yamal Peninsula Region Using Satellite Data

Troshkin D.N., Pavlov V.E.

Abstract

The optical depths of summertime clouds are statistically analyzed in the region of Ob Bay in three bounded zones over “dry” areas and areas comprising large water basins. We used experimental data, obtained onboard the European satellite ENVISAT (MERIS instrument) in 2008–2011. The shape of the probability distribution functions of the optical depths in each of the zones is determined. These functions have 3–4 modes in logarithmic coordinates. The functions were fit using a set of normal logarithmic distributions with adjusted parameters, found to be well repetitive from one year to another. The water-poor western zone is characterized by three modes; and for eastern zones, with northward-flowing rivers full of relatively warm waters, the number of modes increases to four. Very likely, the additional mode at small optical depths is explained by water evaporation, followed by condensation of water vapor. It is hypothesized that a certain role in the latter case may be played by anthropogenic emissions, owing to which the number of condensation nuclei in the atmosphere is larger in the eastern than the western zone. We present the plots of the distribution functions and tables of fit parameters that define these functions. These data may be useful in calculation of radiation budget for small territories in the region of the Yamal Peninsula.

Atmospheric and Oceanic Optics. 2019;32(2):147-151
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Remote Sensing of Atmosphere, Hydrosphere, and Underlying Surface

Methane Vertical Profile Retrieval from the Thermal and Near-Infrared Atmospheric Spectra

Zadvornykh I.V., Gribanov K.G., Zakharov V.I., Imasu R.

Abstract

We present a method and algorithm for inverse problem solution in satellite sounding of the atmosphere for retrieval of vertical profiles of optically active gases by joint use of high-resolution thermal and near-infrared atmospheric spectra. To show the capabilities of the method, a computational experiment was performed on retrieving the vertical profile of the main methane isotopologue with simultaneous use of the simulated thermal and near-infrared spectra. The spectra simulated are similar to those measured by TANSO-FTS/GOSAT IR spectrometer. The signal-to-noise ratio in the simulated spectra was set to 350. The model experiments show higher accuracy of retrieval of the methane vertical profile and its total column in the case when both spectral bands (thermal and near-IR) are used in comparison with the case when each band is used separately.

Atmospheric and Oceanic Optics. 2019;32(2):152-157
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Specific Features of Transport and Transformation of Atmospheric Aerosol and Gas Admixtures in the Coastal Zone of Lake Baikal

Zayakhanov A.S., Zhamsueva G.S., Tsydypov V.V., Balzhanov T.S., Balin Y.S., Penner I.E., Kokhanenko G.P., Nasonov S.V.

Abstract

Diurnal dynamics of atmospheric gases and the meteorological characteristics of the atmosphere at different altitudes on the southeastern coast of Lake Baikal are experimentally studied. The measurements were performed at the Boyarsky stationary site (51.84° N, 106.06° E) in July–August 2015–2016. Simultaneously, lidar measurements were carried out to study the formation of the vertical structure of aerosol fields both under natural (background) conditions and in the presence of sources of smoke from forest fires.

Atmospheric and Oceanic Optics. 2019;32(2):158-164
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The Analysis of Capabilities of Neural Networks in CO2 Sounding with Spaceborne IPDA-Lidar with the Use of Different A Priori Data

Matvienko G.G., Sukhanov A.Y., Babchenko S.V.

Abstract

The possibility of retrieving, using a neural network, the columnar carbon dioxide concentration profile when sounding from a space orbit of 450 km and from a balloon at altitudes of 23 and 10 km are analyzed. The use of a priori data on temperature, pressure, and reflected and scattered signals is considered. The errors of retrieval of the columnar CO2 are 0.15% and 0.5% at altitudes lower than 2 km for lidar with a telescope diameter of 1 m and laser pulse energy of 50 μJ at a resolution of 60 km.

Atmospheric and Oceanic Optics. 2019;32(2):165-170
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Atmospheric Radiation, Optical Weather, and Climate

Change in the Synoptic Regime of Tomsk in the Late 20th–Early 21st Centuries

Sklyadneva T.K., Belan B.D., Rasskazchikova T.M., Arshinova V.G.

Abstract

Synoptic processes that occurred in the Tomsk region between 1993 and 2016 are analyzed. A significant decrease in the difference between the frequency of cyclones and anticyclones over the past decade is revealed. There are tendencies to a decrease in the frequency of Arctic air mass invasion, and to an increase, of subtropical and tropical air masses.

Atmospheric and Oceanic Optics. 2019;32(2):171-176
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Estimates of UV Indices During the Periods of Reduced Ozone Content over Siberia in Winter–Spring 2016

Chubarova N.E., Timofeev Y.M., Virolainen Y.A., Polyakov A.V.

Abstract

UV radiation is calculated for Russian regions where anomalies of the total ozone content were observed in the first quarter of 2016. Winter ozone depletion in northern regions of Siberia, even to the levels of the so-called ozone hole, is not critical. However, much weaker ozone reduction in the early spring can lead to dangerous levels of erythemal UV radiation, when skin protection from ultraviolet radiation is required.

Atmospheric and Oceanic Optics. 2019;32(2):177-179
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Optical Models and Databases

Monitoring of Atmospheric Parameters: 25 Years of the Tropospheric Ozone Research Station of the Institute of Atmospheric Optics, Siberian Branch, Russian Academy of Sciences

Davydov D.K., Belan B.D., Antokhin P.N., Antokhina O.Y., Antonovich V.V., Arshinova V.G., Arshinov M.Y., Akhlestin A.Y., Belan S.B., Dudorova N.V., Ivlev G.A., Kozlov A.V., Pestunov D.A., Rasskazchikova T.M., Savkin D.E., Simonenkov D.V., Sklyadneva T.K., Tolmachev G.N., Fazliev A.Z., Fofonov A.V.

Abstract

We describe the current state and technical characteristics of Tropospheric Ozone Research (TOR) station, created 25 years ago to monitor atmospheric composition, basic meteorological variables, and other parameters. The multiyear observations showed that the air quality on the territory of Akademgorodok in Tomsk has been substantially degraded since the creation and development of the Special Economic Zone on its territory.

Atmospheric and Oceanic Optics. 2019;32(2):180-192
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Comparison of Several Numerical Methods for Fog Prediction

Zarochentsev G.A., Rubinstein K.G., Bychkova V.I., Ignatov R.Y., Yusupov Y.I.

Abstract

Several methods for visibility calculation for fog forecasting are discussed, including a method suggested by the authors. We use the WRF-ARW model to obtain the necessary meteorological information. The forecasts are estimated using data with a high spatial resolution from European Synoptic stations. The analysis of the methods shows a generally satisfactory quality of forecasts for this phenomenon.

Atmospheric and Oceanic Optics. 2019;32(2):193-201
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Optical Instrumentation

Development of the Model of Turbulent Atmosphere at the Large Solar Vacuum Telescope Site as Applied to Image Adaptation

Kovadlo P.G., Lukin V.P., Shikhovtsev A.Y.

Abstract

The work is aimed at the improvement of the model of a turbulent atmosphere at the Large Solar Vacuum Telescope site using the analysis of the energy turbulence spectrum in a wide range of frequencies and deformations of the vertical profile of the structure parameter of the refractive index of air in the atmospheric boundary layer (up to 1 km), depending on the energy of the surface turbulence.

Atmospheric and Oceanic Optics. 2019;32(2):202-206
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Aeroptical Effects Caused by Supersonic Airflow around an Ogival Body

Sukharev A.A.

Abstract

An optical model of a shock wave generated due to supersonic airflow around a body of an ogival form is developed. Mean values of airflow parameters were calculated from the Navier–Stokes equations using the CFD Fluent 6.0 software package accounting for the gas compressibility. It is shown that the maximum values of the structure parameters are several orders of magnitude larger than the values typical for an unperturbed shock wave in the atmosphere. Results of numerical simulation of propagation of an optical beam which crosses the shock wave at the beginning of a path and then propagates through a homogeneous medium are presented. It is shown that an increase in the aircraft speed increases the transverse dimensions of the beam due to diffraction. The angular deviation of the beam from rectilinear propagation under the impact of the shock wave depends only on the altitude above the Earth’s surface where the shock wave is generated. The impact of the shock wave on the crossing beam weakens as the altitude increases.

Atmospheric and Oceanic Optics. 2019;32(2):207-212
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Software-Controlled High-Resolution Laser Photoacoustic Spectrometer: Techniques and Programs for Measuring and Processing Weak Absorption Spectra of Atmospheric Gases

Kapitanov V.A., Osipov K.Y.

Abstract

A software-controlled photoacoustic spectrometer designed on the basis of a TEC-520 diode laser (output power 30 mW, coarse tuning range 6060–6600 cm−1, bandwidth ∼5 × 10–5 cm−1, fine tuning range is 0–2.5 cm−1), WS-UIR laser wavelength meter (relative error Δλ/λ ∼ 10–8), and resonance photoacoustic detector with a threshold sensitivity of ∼3 × 10–10 W cm−1 Hz−1/2 is described, as well as techniques and software developed for measurements and spectra processing. The water vapor spectra are analyzed.

Atmospheric and Oceanic Optics. 2019;32(2):213-219
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Low-Temperature Cell for Studying Absorption Spectra of Greenhouse Gases

Serdyukov V.I., Sinitsa L.N., Lugovskoi A.A., Emelyanov N.M.

Abstract

A low temperature vacuum cell 220 cm in length with windows of quartz, ZnSe, and KBr has been designed for working with the high resolution Bruker IFS 125-M Fourier spectrometer. It provides a threshold sensitivity to absorption on the order of 10–7 cm–1, and allows recording absorption spectra of gases in the temperature range from 200 to 296 K in the region 1000–20 000 cm–1 with an accuracy of 0.9 K.

Atmospheric and Oceanic Optics. 2019;32(2):220-226
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Effectiveness of Combined Laser and Gas Chromatographic Remote Detection of Traces of Explosives

Baldin M.N., Bobrovnikov S.M., Vorozhtsov A.B., Gorlov E.V., Gruznov V.M., Zharkov V.I., Panchenko Y.N., Pryamov M.V., Sakovich G.V.

Abstract

The results of remote detection of objects containing explosives with a lidar detector of traces of explosives in combination with a portable express gas chromatograph are presented. It is shown that the lidar detector of traces of explosives confidently detects the simulators of TNT, hexogen, and PETN from a distance of 5 m when sounding the surface of a sample. Laser action on the sample surface causes desorption of vapors, which are reliably detected by the gas chromatograph. It is shown that the joint use of the laser sounding and gas chromatography techniques makes it possible to increase the reliability of detection of explosives. The prospects of using the gas chromatography in the development of laser sounding techniques are determined.

Atmospheric and Oceanic Optics. 2019;32(2):227-233
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