Atmospheric and Oceanic Optics最新文献_第8页

Remote Determination of Turbulence Parameters of a Stratified Atmospheric Boundary Layer 层状大气边界层湍流参数的远程测定

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Atmospheric and Oceanic Optics Pub Date : 2025-04-29 DOI: 10.1134/S1024856024701227

V. A. Banakh, I. N. Smalikho, E. V. Gordeev, A. A. Sukharev, A. V. Falits

{"title":"Remote Determination of Turbulence Parameters of a Stratified Atmospheric Boundary Layer","authors":"V. A. Banakh, I. N. Smalikho, E. V. Gordeev, A. A. Sukharev, A. V. Falits","doi":"10.1134/S1024856024701227","DOIUrl":"10.1134/S1024856024701227","url":null,"abstract":"Results of experiments on determining turbulence parameters of a stratified atmospheric boundary layer by means of remote sensing are presented. The height–time distributions of the dissipation rate of kinetic energy of turbulence and those of the structural constant of turbulent fluctuations of temperature obtained using a coherent wind lidar and a temperature radiometer are compared with height variations in parameters characterizing atmospheric stratification. It is shown that the dissipation rate which determines the intensity of wind turbulence decreases in the boundary layer with height for all types of thermal stratification. The intensity of turbulent fluctuations of temperature depends to a greater extent on variations in thermodynamic stability in the atmosphere. If the thermal instability of the atmosphere at larger heights exceeds that in lower layers, then the structural constant of temperature fluctuations can not decrease but increase with height. In accordance with height variations in the structural constant of temperature, values of the structural constant of turbulent pulsations of the refractive index can also increase with height and differ from those predicted based on known models.","PeriodicalId":46751,"journal":{"name":"Atmospheric and Oceanic Optics","volume":"38 1","pages":"1 - 11"},"PeriodicalIF":0.9,"publicationDate":"2025-04-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143888597","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Comparison of MetOp Satellite and Mobile Lidar Ozone Profiles MetOp卫星与移动激光雷达臭氧廓线的比较

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Atmospheric and Oceanic Optics Pub Date : 2025-04-29 DOI: 10.1134/S1024856024701379

A. A. Nevzorov, A. V. Nevzorov, N. S. Kravtsova, O. V. Kharchenko, Ya. O. Romanovskii

{"title":"Comparison of MetOp Satellite and Mobile Lidar Ozone Profiles","authors":"A. A. Nevzorov, A. V. Nevzorov, N. S. Kravtsova, O. V. Kharchenko, Ya. O. Romanovskii","doi":"10.1134/S1024856024701379","DOIUrl":"10.1134/S1024856024701379","url":null,"abstract":"Atmospheric trace gases (ATGs) are optically active constituents of the atmosphere. ATGs have a great influence on atmospheric processes: transformation of solar radiation, weather formation, air pollution by industrial emissions, and propagation of optical waves. Ozone occupies a special place among ATGs. The ozone layer plays the role of natural protection of the planet from shortwave solar radiation. Therefore, monitoring of the ozonosphere by ground-based and satellite instruments allows us to obtain the most reliable data on the state of the atmosphere and, in particular, the ozone layer. The solution of this urgent problem is possible only with permanent improvement of the hardware base and perfection of methodological approaches to scientific research of the atmosphere. In this work, a number of measurements were carried out using a mobile ozone lidar at the sensing wavelengths of 299/341 nm in the altitude range 0.1–12 km at the Siberian lidar station (SLS). Vertical ozone profiles retrieved from lidar and meteorological satellite data of the European Space Agency (MetOp) obtained in 2023 were compared. The comparisons showed that the average relative difference between the profiles varies from −65.6% to 15.3% at altitudes from 0.1 km to 12 km. The comparison results confirm good prospects for using these ozone sensing wavelengths in the altitude range 0.1–5 km, previously uncovered by the SLS. The results will be used in modeling the vertical distribution of ozone concentration and in assessing the ecological state of the atmosphere in the Tomsk oblast.","PeriodicalId":46751,"journal":{"name":"Atmospheric and Oceanic Optics","volume":"38 1","pages":"112 - 117"},"PeriodicalIF":0.9,"publicationDate":"2025-04-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143888796","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Optical Properties of Atmospheric Ice Crystals of Arbitrary Shape with Different Number of Facets for Problems of Laser Sensing 激光传感问题中任意形状不同面数大气冰晶的光学特性

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Atmospheric and Oceanic Optics Pub Date : 2025-04-29 DOI: 10.1134/S1024856024701343

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

引用次数: 0

Synergetic Ground-Based MW + IR Method for Ozone Profiling 协同地面微波+红外臭氧分析方法

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Atmospheric and Oceanic Optics Pub Date : 2025-04-29 DOI: 10.1134/S1024856024701276

Yu. I. Bordovskaya, Yu. M. Timofeev, Ya. A. Virolainen, A. V. Poberovskii

引用次数: 0

Dynamics of the Stratospheric Polar Vortex in 2022/2023 by Vortex Delineation Methods Using Geopotential and Potential Vorticity 2022/2023年平流层极涡动力学的位势和位涡圈定方法

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Atmospheric and Oceanic Optics Pub Date : 2025-04-29 DOI: 10.1134/S1024856024701306

V. V. Zuev, E. A. Sidorovski, A. V. Pavlinsky

{"title":"Dynamics of the Stratospheric Polar Vortex in 2022/2023 by Vortex Delineation Methods Using Geopotential and Potential Vorticity","authors":"V. V. Zuev, E. A. Sidorovski, A. V. Pavlinsky","doi":"10.1134/S1024856024701306","DOIUrl":"10.1134/S1024856024701306","url":null,"abstract":"Two methods for stratospheric polar vortex delineation are compared by the main vortex characteristics they provide: vortex area, average wind speed at the edge, mean temperature inside the vortex. One of the methods is based on the geopotential, and another one is based on the potential vorticity (PV). Both methods use ERA5 reanalysis data on isobaric and isentropic surfaces. The geopotential method yields 1.3‑time higher vortex area for the Arctic and 1.14-time higher for Antarctica than the PV method. The estimates of the average wind speed at the vortex edge are very close: the wind speed by PV method is 5% higher than by the geopotential method for the Arctic and 3% higher in Antarctic. Mean temperature inside the vortex by PV method is 1% lower in both the Arctic and Antarctica. The maximal differences in the estimates of the vortex area are 25.52 million km2 in the Arctic (on November 23, 2022, on the 600-K isentropic surface) and 23.78 million km2 in Antarctica (on December 14, 2022, on the 475-K surface). These differences increase with the altitude: from 4.23 million km2 on the 475-K surface to 10.24 million km2 on the 600-K surface in the Arctic, and from 4.91 million km2 on the 475-K surface to 6.17 million km2 on the 600-K surface in Antarctica. The significant difference in the vortex area confirms a need in careful selection of the delineation method when studying polar vortices.","PeriodicalId":46751,"journal":{"name":"Atmospheric and Oceanic Optics","volume":"38 1","pages":"65 - 68"},"PeriodicalIF":0.9,"publicationDate":"2025-04-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143888605","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Turbulent Lidar Measurement Technique and Comparison with Ground-Based Observations 湍流激光雷达测量技术及其与地面观测的比较

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Atmospheric and Oceanic Optics Pub Date : 2025-04-29 DOI: 10.1134/S1024856024701367

I. A. Razenkov

{"title":"Turbulent Lidar Measurement Technique and Comparison with Ground-Based Observations","authors":"I. A. Razenkov","doi":"10.1134/S1024856024701367","DOIUrl":"10.1134/S1024856024701367","url":null,"abstract":"The history of the creation of a turbulent lidar at V.E. Zuev Institute of Atmospheric Optics, Siberian Branch, Russian Academy of Sciences, began 11 years ago, when a bulky laboratory setup enabled experimentally detecting the backscatter enhancement (BSE) effect in a turbulent atmosphere for the first time. Subsequently, a number of design solutions were suggested to improve the lidar, which made it possible to reduce its size and increase its reliability. The main design features of the turbulent lidar, which is a new type of laser locator, are the coincidence of the optical axes of the transmitter and receiver, the presence of an additional receiving channel, and operation in the photon counting mode with the accumulation of echo signals. In this work, the lidar sounding technique is described; an algorithm for retrieving the profile of the structural characteristic of turbulent fluctuations of the refractive index of air from the ratio of lidar echoes is developed; the experimental technique is verified and the lidar data are compared with the readings of a solar radiometer and a scintillometer. Further development of the turbulent lidar sounding technique is to enable ground-based remote monitoring of the turbulence intensity in the atmospheric boundary layer, e.g., along glide paths at airports, distant early detection of clear air turbulence from an aircraft, etc.","PeriodicalId":46751,"journal":{"name":"Atmospheric and Oceanic Optics","volume":"38 1","pages":"103 - 111"},"PeriodicalIF":0.9,"publicationDate":"2025-04-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143888660","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Daily Dynamics of the Electric Field in the Turbulent Surface Air Layer under the Action of Local Factors 局地因素作用下湍流地面空气层电场的日动力学

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Atmospheric and Oceanic Optics Pub Date : 2025-04-29 DOI: 10.1134/S102485602470132X

D. V. Timoshenko, G. V. Kupovykh, T. V. Kudrinskaya

{"title":"Daily Dynamics of the Electric Field in the Turbulent Surface Air Layer under the Action of Local Factors","authors":"D. V. Timoshenko, G. V. Kupovykh, T. V. Kudrinskaya","doi":"10.1134/S102485602470132X","DOIUrl":"10.1134/S102485602470132X","url":null,"abstract":"This work studies the effect of the daily dynamics of turbulent processes on the daily dynamics of the electric field in the surface air layer. During simulation, the coefficient of turbulent diffusion within the electrode layer is specified as a stationary function of altitude in view of hydrodynamic concepts. A mathematical model of the dynamics of the electric field intensity in the surface air layer in the case of a turbulent electrode effect is presented. The main equation of the model is the equation of the total current in the surface layer, which has been derived in the approximation of strong turbulent mixing and describes the electrodynamics of the surface layer under the combined action of local and global current generators. The work examines the non-stationary nature of turbulent exchange in order to confirm the previously ascertained effects in the daily dynamics of the electric field strength in the surface air layer under stationary turbulence. To describe the daily dynamics of turbulent processes, gradient measurements in high-altitude conditions of the Elbrus region were used. Processing of the measurement data enables deriving the time dependence of the turbulent diffusion coefficient from the solution of the total current equation. Taking into account this dependence, the expression for the daily dynamics of the field strength was refined. Time shifts of the daily extremes, a change in their amplitude, and the appearance of additional extremes depending on the electric field strength have been established. All these effects are comparable to the global unitary variation and increase with the electric field strength. The results can be useful for solving a number of applied geophysical problems, in particular, monitoring the electric field of the atmosphere and analyzing atmospheric-electrical measurement data.","PeriodicalId":46751,"journal":{"name":"Atmospheric and Oceanic Optics","volume":"38 1","pages":"77 - 82"},"PeriodicalIF":0.9,"publicationDate":"2025-04-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143888596","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Features of the Vertical Distribution of Air Temperature over Tomsk during Sudden Stratospheric Warming in Winter 2023 According to Data from the Siberian Lidar Station 基于西伯利亚激光雷达站数据的2023年冬季平流层突然变暖期间托木斯克上空气温垂直分布特征

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Atmospheric and Oceanic Optics Pub Date : 2025-04-29 DOI: 10.1134/S102485602470129X

O. Yu. Antokhina, S. M. Bobrovnikov, V. I. Zharkov, O. S. Zorkaltseva, D. A. Trifonov

{"title":"Features of the Vertical Distribution of Air Temperature over Tomsk during Sudden Stratospheric Warming in Winter 2023 According to Data from the Siberian Lidar Station","authors":"O. Yu. Antokhina, S. M. Bobrovnikov, V. I. Zharkov, O. S. Zorkaltseva, D. A. Trifonov","doi":"10.1134/S102485602470129X","DOIUrl":"10.1134/S102485602470129X","url":null,"abstract":"Atmospheric temperature anomalies associated with sudden stratospheric warming events (SSWs) observed over the territory of Siberia require detailed study. In Siberia, there are few instruments that can provide the necessary information on the vertical distribution of atmospheric temperature. Unique lidar of the Siberian Lidar Station (SLS) of V.E. Zuev Institute of Atmospheric Optics SB RAS, Tomsk, Russia (56.48° N, 85.05° E), developed for regular lidar measurements of atmospheric parameters, is one of few ground-based devices in Siberia which provide necessary data on the vertical stratification of atmospheric temperature during the SSW effect. To determine the characteristics of atmospheric temperature anomalies during the SSW period in winter 2023 over Tomsk, data on atmospheric temperature in individual nights obtained by the SLS lidar, the WACCM model, the standard mid-latitude winter model, and the ERA5 reanalysis were compared. For the first time, the possibility of using vertical atmospheric temperature profiles obtained by the Raman scattering method to study the SSW effect is show. Use of lidar air temperature profiles to analyze changes in the vertical structure of the atmosphere during SSWs is demonstrated.","PeriodicalId":46751,"journal":{"name":"Atmospheric and Oceanic Optics","volume":"38 1","pages":"59 - 64"},"PeriodicalIF":0.9,"publicationDate":"2025-04-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143888604","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Estimation of Atmospheric Optical Parameters with Simultaneous Measurement of Vibrational-Rotational and Purely Rotational Raman Spectra 同时测量振动-旋转和纯旋转拉曼光谱估算大气光学参数

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Atmospheric and Oceanic Optics Pub Date : 2025-04-29 DOI: 10.1134/S1024856024701252

S. V. Samoilova, Yu. S. Balin, I. E. Penner

{"title":"Estimation of Atmospheric Optical Parameters with Simultaneous Measurement of Vibrational-Rotational and Purely Rotational Raman Spectra","authors":"S. V. Samoilova, Yu. S. Balin, I. E. Penner","doi":"10.1134/S1024856024701252","DOIUrl":"10.1134/S1024856024701252","url":null,"abstract":"The paper considers the methodological features of determining the optical extinction and backscattering coefficients by simultaneous lidar measurements at the following wavelengths: 532 nm (elastic scattering, ES), 607 nm (vibrational-rotational Raman scattering, RS), and 530 nm (purely rotational RS). The ES signal identifies the range of allowable values (RAV) of the coefficients based on the a priori introduction of a physically substantiated lidar ratio. The RS signal at λ = 607 nm, corresponding to a single line of the N2 spectrum, provides a plausible estimate of the ratios in the boundary layer and part of the middle troposphere. The RS signal at vλ = 530 nm—a set of N2 and O2 spectrum lines—is characterized by smaller errors and provides a quantitative estimate of the coefficients in all main tropospheric layers. At a wavelength of 530 nm, the differential backscattering cross section depends on height due to temperature changes, which leads to a redistribution of N2 and O2 line intensities. Estimation of parameters from the RS signals is considered plausible when the sought-after coefficients are quantitatively comparable and located within their RAVs. Testing of the algorithms is carried out using ground-based sensing data on the shore of Lake Baikal in August 2023.","PeriodicalId":46751,"journal":{"name":"Atmospheric and Oceanic Optics","volume":"38 1","pages":"27 - 36"},"PeriodicalIF":0.9,"publicationDate":"2025-04-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143888556","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

Estimates of the Frequency of Synoptic Variations in Aerosol Characteristics in the Arctic Atmosphere and the Contribution of Various Pollutants to Anomalously High Aerosol Concentrations 北极大气中气溶胶特征天气变化频率的估计和各种污染物对异常高气溶胶浓度的贡献

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Atmospheric and Oceanic Optics Pub Date : 2025-04-29 DOI: 10.1134/S1024856024701318

I. A. Kruglinsky, D. M. Kabanov, S. M. Sakerin

{"title":"Estimates of the Frequency of Synoptic Variations in Aerosol Characteristics in the Arctic Atmosphere and the Contribution of Various Pollutants to Anomalously High Aerosol Concentrations","authors":"I. A. Kruglinsky, D. M. Kabanov, S. M. Sakerin","doi":"10.1134/S1024856024701318","DOIUrl":"10.1134/S1024856024701318","url":null,"abstract":"The periodicity of synoptic-scale variations in aerosol characteristics in the atmosphere of Eurasian sector of the Arctic Ocean is analyzed on the basic of long-term measurements. Statistically significant maxima of amplitude functions in the range from 3.5 to 18 days were manifested in periodograms of the concentrations of submicron aerosol and black carbon (Vf and еВС). Cases of anomalously high еВС and Vf (5% of data), associated with long-range transports of continental pollutants, were considered in more detail. It is shown that the average duration of “anomalies” in еВС and Vf is few days, and the maximal duration attains 112 hours. The time intervals between “anomalies” are, on the average, 6–16 days, and the maximal intervals are from 28 to 69 days. Despite the short duration and rare occurrence of anomalous situations, they increase the average concentrations of aerosol and black carbon by 28–77%. Calculations showed that the major (79%) contributors to air pollution over the Kara and Barents Seas are made by the outflows of anthropogenic pollutants; and in the eastern sector of the Arctic Ocean, the contribution of smokes from wildfires is maximal. The effect of the products of associated gas combustion at gas-oil plants was manifested most strongly (up to 51%) in the atmosphere of Cape Baranov.","PeriodicalId":46751,"journal":{"name":"Atmospheric and Oceanic Optics","volume":"38 1","pages":"69 - 76"},"PeriodicalIF":0.9,"publicationDate":"2025-04-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143888553","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0