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Vol 29, No 6 (2016)

Optics of Stochastically-Heterogeneous Media

The mode conversion of structurally stable vector beams propagating through free space optical channels

Arsenyan T.I., Babanin E.A., Vokhnik O.M., Zotov A.M., Mardanov A.F., Suhareva N.A.

Abstract

The reconstruction of the spatial intensity distribution of structurally stable axially symmetrical beams in free space optical data transmitting channels has been studied experimentally. The structure transformation invariants of а beam as а space code bearer are discussed. The correlation and dispersion parameters of a random process of optical density modulation are estimated; a possibility of their multiple differences in different directions perpendicular to the beam axis is shown.

Atmospheric and Oceanic Optics. 2016;29(6):483-491
pages 483-491 views

Optics of Clusters, Aerosols, and Hydrosoles

Optical-microphysical and physical-chemical characteristics of Siberian biomass burning: Experiments in Aerosol Chamber

Popovicheva O.B., Kozlov V.S., Rakhimov R.F., Shmargunov V.P., Kireeva E.D., Persiantseva N.M., Timofeev M.A., Engling G., Eleftheriadis K., Diapouli E., Panchenko M.V., Zimmermann R., Schnelle-Kreis J.

Abstract

A series of experiments aimed at studying the effect of combustion regimes of typical Siberian biomasses on the optical, microphysical, and physical-chemical properties of smoke aerosols was performed in the Large Aerosol Chambe, Institute of Atmospheric Optics, Siberian Branch, Russian Academy of Sciences. A comprehensive data analysis showed that temperature regime of Siberian pine and coniferous tree burning has a key effect on the formation and time dynamics of all smoke characteristics. The polarization spectronephelometer measurements of light scattering are used to determine the size distributions and absorption indices of particles. Particles in the smoldering phase are weakly absorbing, but the mixed phase contains a strongly absorbing fine component produced in open flame phases. We studied microstructure characteristics of aerosols by the analysis of morphology and elemental composition. Groups of soot and organic particles were determined as micromarkers of emissions in open flaming and smoldering phases, respectively. The organic and elemental carbon contents, origin and concentration of chemical compounds in the water-soluble ion fraction exhibit a strong dependence on the combustion phase. Sugar anhydride (levoglucosan) was determined in the smoldering phase as a stable molecular marker of Siberian pine burning. A number of specific markers of coniferous wood burning were identified among the chemical compounds. Smoke aging is accompanied by condensation of organic and inorganic compounds, transformation of aerosol surface chemistry, and the formation of the group of potassium-rich particles, all demonstrating the complexity and variability of the chemical composition and microstructure of atmospheric aerosol pollution during Siberian forest fires.

Atmospheric and Oceanic Optics. 2016;29(6):492-500
pages 492-500 views

Quasiperiodic saltation in the windsand flux over desertified areas

Gorchakov G.I., Karpov A.V., Kuznetsov G.A., Buntov D.V.

Abstract

Saltation in a windsand flux over a desertified area is studied on the basis of high-speed video recording data using spectral and wavelet analysis. Features of quasiperiodic variations in the saltating sand concentration are studied. It is ascertained that narrow bands in the spectrum (“spectral lines”) of the power density of the saltating sand concentration fluctuations in the range from 100 to 200 Hz are consistent with trains (wave packets) of up to 8–9 periods in duration. It is suggested to use the duration of the trains observed as a measure of the coherence of wind speed pulsations in the surface air layer. It is shown that the trains in the quasiperiodic variability of the saltating sand concentration can be explained by the interaction of wind gusts with wave irregularities on the underlying surface of a fine ripple type. The wave packet formation of 4–5 periods in duration can be explained using the jet-pulse saltation model.

Atmospheric and Oceanic Optics. 2016;29(6):501-506
pages 501-506 views

Material and elemental composition of surface aerosols on the north-western coast of the Kandalaksha Bay of the White Sea

Starodymova D.P., Shevchenko V.P., Sivonen V.P., Sivonen V.V.

Abstract

Continuous sampling of aerosols is carried out on the north-western (NW) coast of the Kandalaksha Bay of the White Sea. Aerosol matter from 30 filters collected in summer and autumn, 2013, and spring, 2014, was studied by scanning electron microscopy. The elemental composition of aerosol matter was determined by the inductively-coupled plasma mass-spectrometry (ICP-MS). The major portion of aerosol particles collected in summer is of biogenic origin. Heavy metal concentrations in aerosols are at the Arctic background level. The distribution of trace element concentrations is characterized by simultaneous peaks of different elements. The backward trajectory analysis shows an increase in Ni and Cu concentrations corresponding to the arrival of air masses from the western part of the Kola Peninsula. That suggests the influence of smelters.

Atmospheric and Oceanic Optics. 2016;29(6):507-511
pages 507-511 views

Simulation of nanoparticle thermal diffusion in dense gases and fluids by the molecular dynamics method

Rudyak V.Y., Krasnolutskii S.L.

Abstract

This paper is devoted to the study of the thermal diffusion of nanoparticles in dense gases and fluids by the method of molecular dynamics with Rudyak–Krasnolutskii nanoparticle–molecule and Rudyak–Krasnolutskii–Ivanov nanoparticle–nanoparticle potentials. The thermal diffusion and binary diffusion coefficients were calculated with the help of the fluctuation-dissipation theorem. Nanofluids simulated consisted of argon as а carrier medium and aluminum nanoparticles. Dependences of the nanoparticle thermal diffusion and Soret coefficients on the particle diameter and volume concentration were derived. The thermal diffusion coefficient showed a significant dependence on the particle size for small nanoparticles (1–4 nm diameter).

Atmospheric and Oceanic Optics. 2016;29(6):512-515
pages 512-515 views

Remote Sensing of Atmosphere, Hydrosphere, and Underlying Surface

Multifrequency lidar sensing of atmospheric aerosol under conditions of information uncertainty

Lysenko S.A., Kugeiko M.M., Khomich V.V.

Abstract

A method is proposed for solving the inverse problem in multifrequency lidar sensing of the atmospheric aerosol. The method allows retrieving the spatial distribution of volume concentrations of aerosol components, the aerosol particle size distribution integral over the sensing path, and the complex refractive index of the particles, without any additional data for the lidar calibration and supplement of the inverse problem definition. The method is based on the assumption that the average sizes, their variances, and the complex refractive indices for the particles of each aerosol component do not change along the sensing path, and the number of the lidar spectral channels is greater than the number of aerosol components. In this case, the system of equations for the spectral-spatial readings of the lidar signal becomes overdetermined, and its numerical solution allows deriving not only the microphysical parameters of the aerosol, but also the lidar calibration constants at operational wavelengths. Examples of processing the elastic and Raman scattering lidar signals in a model aerodispersive medium at the wavelengths λ0 = 0.355, 0.532, and 1.064 μm and λR = 0.387 and 0.607 μm, respectively, are presented. It is shown that microphysical parameters of the fine aerosol component (with particle sizes less than 1–2 μm) can be retrieved from the signals with an error less than 10%, and the error in retrieving the microphysical parameters of coarse particles depends strongly on their contribution to the total medium transmission. The aerosol extinction and backscattering coefficients calculated on the basis of the aerosol microphysical parameters retrieved differ from their actual values by a few percent.

Atmospheric and Oceanic Optics. 2016;29(6):516-525
pages 516-525 views

Studying the accuracy of the algorithm for retrieving the surface albedo with high spatial resolution from a fragment of a satellite image

Nikolaeva O.V.

Abstract

An efficient algorithm for retrieving the albedo of a spatially inhomogeneous Lambertian surface from values of reflectance of solar radiation reflected from the “atmosphere–underlying surface” system is presented. The algorithm relies on the reflectance representation in the problem with an arbitrary surface albedo in terms of reflectances in problems for the same atmosphere with model underlying surfaces. Results of solving the model problems are presented. They demonstrate the possibility to use the algorithm in processing data of high spatial resolution (up to 15 m).

Atmospheric and Oceanic Optics. 2016;29(6):526-532
pages 526-532 views

Three algorithms of statistical modeling in problems of optical communication on scattered radiation and bistatic sensing

Belov V.V., Tarasenkov M.V.

Abstract

Three algorithms of the Monte Carlo method for the calculation of the pulse reaction in channels of laser sensing and communication are considered: the local estimation algorithm, double local estimation algorithm, and proposed modified double local estimation algorithm. Results of testing the algorithms and their comparison are shown. For the case of a homogeneous medium, the performances of the algorithms are compared. The comparison shows conditions for which the proposed algorithm has the advantage over the double local estimation algorithm. The contribution of double, triple, and higher multiplicity scattering is estimated. The high contribution of multiple scattering justifies the applicability of the Monte Carlo method for solving such problems.

Atmospheric and Oceanic Optics. 2016;29(6):533-540
pages 533-540 views

Atmospheric Radiation, Optical Weather, and Climate

Analysis of Siberian river runoffs in the 21st century

Kuzin V.I., Lapteva N.A.

Abstract

We discuss the results from the analysis of the hydrological input data for a model of Siberian river runoff for the 21st century. The INM, CRNM, GFDL, MIROC5, and HadGEM model calculations according to the RCP 8.5 scenario of the IPCC CMIP5 Project were used for the analysis. The calculations show a positive centennial trend for all the models. These data were used for the calculations of Siberian river discharge to the Arctic Ocean. The river runoff calculations in accordance with the data also indicate a positive trend, though with a different runoff magnitude.

Atmospheric and Oceanic Optics. 2016;29(6):541-544
pages 541-544 views

Anomalous wildfires in 2010 and 2012 on the territory of Russia and supply of black carbon to the Arctic

Vinogradova A.A., Smirnov N.S., Korotkov V.N.

Abstract

Model estimates of black carbon (BC) concentrations in air were performed for different regions of the Russian Arctic under the conditions of maximal wildfires during summers of 2010 and 2012 on the territory of Russia. Data available from the Federal Forestry Agency of the Russian Federation (Rosleskhoz) on burning areas subject to fires (for different months of 2000–2013) were processed taking into account the quality of combustible material and different fire types. The developing atmospheric BC concentrations in the northern regions were calculated using the back trajectory statistics method for the Kola Peninsula, southeastern Arkhangelsk region, and Nenets, Gydan, and Ust-Lena Nature Reserves. It is shown that the specific circulation conditions in the atmosphere, accompanying extremely strong fires, may hamper transport of atmospheric pollutants to Arctic regions during the fire period. The BC concentrations are, on average, minor in northwestern European Russia (Kola Peninsula) and in the region of Ust-Lena Nature Reserve; and the largest pollution of air in northeastern Europe (region of Nenets Nature Reserve) is due to BC emissions from fires. On the contrary, anthropogenic BC predominates in northwestern Siberia (region of Gydan Nature Reserve). Strong Siberian and Yakutia fires may increase summertime air pollution by black carbon in north Asian Russia by an order of magnitude. The results presented here can be used for the qualitative estimation and comparative analysis of climatic and ecological conditions in different regions of the Russian Arctic.

Atmospheric and Oceanic Optics. 2016;29(6):545-550
pages 545-550 views

Causes and factors of positive surface ozone anomalies in the Moscow region and on the southeastern coast of the Crimea

Zvyagintsev A.M., Kuznetsova I.N., Shalygina I.Y., Lapchenko V.A., Brusova N.E., Arkhangelskaya A.A., Tereb N.V., Lezina E.A.

Abstract

Ozone sources and factors responsible for anomalous surface ozone concentrations are discussed. Foreign observations and measurements of surface ozone in Moscow, nearby suburbs, and on the territory far removed from the megalopolis, as well as on the coast of the Black Sea, are used as an example to illustrate the interrelations between elevated surface ozone concentrations, air temperature, and transport speed in the planetary boundary layer, and to show the dependence on advection of ozone and its precursors. Studies of factors responsible for ozone episodes and causes of decreased ozone concentrations under meteorological conditions favorable for photochemical ozone production are the basis for interpretation and correction of model ozone predictions.

Atmospheric and Oceanic Optics. 2016;29(6):551-560
pages 551-560 views

Calculation of the turbulent friction velocity in a mathematical model of an urban heat island in a stably stratified environment

Kurbatskaya L.I., Kurbatskii A.F.

Abstract

We examine the parameterizations of the turbulent friction velocity u* for the mathematical model of an urban heat island of a low-aspect-ratio in a calm stably stratified environment with a thermophysically inhomogeneous underlying surface (unstable stratification over a localized surface heat source and stable stratification out of it). The results of u* calculation by Louis and Paulson noniterative algorithms for the quasi-steady circulation over an urban heat island are presented.

Atmospheric and Oceanic Optics. 2016;29(6):561-564
pages 561-564 views

Numerical analysis of atmospheric circulation and pollution transfer in the environs of Norilsk industrial region

Lezhenin A.A., Raputa V.F., Yaroslavtseva T.V.

Abstract

Using a numerical mesoscale model of the atmospheric boundary layer, the dynamics of air streams in the Norilsk valley is studied for typical weather conditions. It is shown that the orographic features of the region form a wind field, horizontally inhomogeneous and highly variable in altitude. The fields of local and regional dust and heavy metal precipitations are numerically reconstructed on the basis of expedition data on snow cover pollution in the environs of the Norilsk copper plant.

Atmospheric and Oceanic Optics. 2016;29(6):565-569
pages 565-569 views

Numerical model of bioaerosol transformation in the atmosphere

Penenko A.V., Sorokovoy A.A., Sorokovaya K.E.

Abstract

A nonstationary mathematical model of bioaerosol dynamics is considered. It is based on nonlinear integral-differential equations that describe coagulation, condensation, and evaporation processes versus particle sizes. A definitely positive numerical scheme for solution of the problem of aerosol transformation in the atmosphere is presented. The model is numerically compared with the models that describe individual processes in the composition of the former. The relative contribution of each process in the overall dynamics of aerosol populations is studied in numerical experiments.

Atmospheric and Oceanic Optics. 2016;29(6):570-574
pages 570-574 views

Optical Sources and Receivers for Environmental Studies

High-power gas-discharge excimer ArF, KrCl, KrF, and XeCl lasers on buffer-gas free gas mixtures

Razhev A.M., Kargapoltsev E.S., Churkin D.S.

Abstract

Results of experimental studies of the gas mixture (laser active medium) effect on the lasing energy and overall efficiency of excimer discharge ArF (193 nm), KrCl (222 nm) KrF (248 nm), and XeCl (308 nm) lasers operating in buffer-free gas mixtures are presented. The optimal (in terms of maximum radiation energy) ratios of the gas components of the excimer laser active media are found, at which efficient operation is achieved with a sufficiently high power of the laser radiation. It is confirmed experimentally that for the rare gas halide discharge pumped excimer lasers the presence of a buffer gas in the active medium is not required for efficient laser operation. For example, in two-component excimer laser gas mixtures, containing working rare and halogen-containing gases, laser pulse energy of up to 170 mJ and high pulsed power of laser radiation of up to 24 MW have been attained for the first time for pulsed gas-discharge excimer lasers operating on electronic transitions at excimer ArF*, KrCl*, KrF*, and XeCl* molecules pumped by a transverse electric volume discharge of a low-pressure buffer-free gas mixture. A overall efficiency maximum of up to 0.8% was experimentally attained for binary gas mixture of KrF and XeCl lasers.

Atmospheric and Oceanic Optics. 2016;29(6):575-579
pages 575-579 views

Visibility range of LED signaling lights of a runway

Kaloshin G.A., Matvienko G.G., Shishkin S.A., Anisimov V.I., Butuzov V.V., Zhukov V.V.

Abstract

Results of calculations for the luminous intensity from light emitting diode (LED) lights necessary for reliable visual detection of runway (RW) lights in real operational conditions are presented. The following groups of RW LED lights are considered: approach threshold lights, lights of the last 600 m of the runway, and runway end lights. Threshold levels of detection have been chosen. The effectiveness of RW LED lights is analyzed in different weather conditions during the night, at twilight, and in the daytime, and questions of a stepped adjustment of LED light radiation intensities in accordance with ICAO standards are considered.

Atmospheric and Oceanic Optics. 2016;29(6):580-585
pages 580-585 views