G. A. Ivlev
Russian Academy of Sciences
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Featured researches published by G. A. Ivlev.
Journal of Atmospheric and Oceanic Technology | 2012
P. N. Antokhin; Michael Yu. Arshinov; Boris D. Belan; D. K. Davydov; Eugenii V. Zhidovkin; G. A. Ivlev; Artiom V. Kozlov; Valerii S. Kozlov; Michael V. Panchenko; Ioganes E. Penner; Dimitrii A. Pestunov; D. V. Simonenkov; Gennadii N. Tolmachev; Alexander Fofonov; Vitalii S. Shamanaev; Vladimir P. Shmargunov
AbstractThe scientific instrumental complex of the Optik-E AN-30 aircraft laboratory developed at the Institute of Atmospheric Optics of the Siberian Branch of the Russian Academy of Sciences is described in detail. Specifications of the main units of the instrumental complex are presented. Special attention is given to the metrological support of measurements of the atmospheric parameters. Experimental capabilities of the aircraft laboratory are illustrated by the results obtained in recent flights over various regions of the Russian Federation.
Atmospheric and Oceanic Optics | 2011
P. N. Antokhin; V. G. Arshinova; M. Yu. Arshinov; Boris D. Belan; Sergey Borisovich Belan; D. K. Davydov; G. A. Ivlev; A. V. Kozlov; T. M. Rasskazchikova; A. V. Fofonov
Distribution of impurities over the region abutting the Ural Mountains is analyzed with the purpose of searching for traces of western European emissions over the territory of Siberia. It is shown that transborder transfer of impurities from Europe to Asia along direct trajectories (along a circle of latitude) from west to east is possible only in the free troposphere, in a layer higher than 2 km. Within the limits of the atmospheric boundary layer, the transfer of impurities from Europe to Siberia is probable only along trajectories rounding the Urals from north or south.
Atmospheric and Oceanic Optics | 2012
Boris D. Belan; G. A. Ivlev; Tatyana K. Sklyadneva
The monitoring results of the total (0.3–2.4 μm) and UV (0.28–0.32 μm) radiation in Tomsk in 2003–2010 are presented. In this period, stable radiation conditions were observed with an abnormally high income of total solar radiation in 2003. A tendency toward a drop of incoming UV-B radiation is noted; no significant effect of the total ozone content on variations in the UV-B radiation in warm periods is revealed.
Atmospheric and Oceanic Optics | 2014
V. M. Dorokhov; G. A. Ivlev; V. I. Privalov; A. M. Shalamyansky
Changes in the total ozone in the Earth’s atmosphere affect both the observed atmospheric changes and the climate of our planet. Ground-based measurements of the total ozone in the Russian Federation are carried out with the use of Dobson and Brewer spectrophotometers and SAOZ spectrometers; M-124 filter ozonometers are used in the Russian ozone network. In the near future, we will start the installation and trial operation of up-to-date automated UVOS spectrometers for observations of the total ozone and UV radiation. The work describes the main specifications of equipment used in ground-based measurements of the total ozone in Russia. The problems of modernization of the national network for the total ozone and UV solar radiation monitoring are considered.
Atmospheric and Oceanic Optics | 2018
O. Yu. Antokhina; P. N. Antokhin; V. G. Arshinova; M. Yu. Arshinov; Boris D. Belan; Sergey Borisovich Belan; D. K. Davydov; G. A. Ivlev; A. V. Kozlov; Philippe Nedelec; Jean-Daniel Paris; T. M. Rasskazchikova; Denis Savkin; D. V. Simonenkov; Tatyana K. Sklyadneva; Gennadii N. Tolmachev; A. V. Fofonov
Data on the vertical distribution of gaseous and aerosol composition of air, measured onboard the Tu-134 Optic airborne laboratory in October 2014 over the Kara Sea and coastal areas of the Russian Arctic, are presented. We revealed the specific features of the altitude distributions of CO2 and aerosol over the Kara Sea as compared to continental conditions. No significant deviations from continental distributions are found for CH4, CO, and O3.
20th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics | 2014
G. G. Matvienko; Boris D. Belan; M. V. Panchenko; O. A. Romanovskii; S. M. Sakerin; D. M. Kabanov; S. A. Turchinovich; Yu. S. Turchinovich; T. A. Eremina; V. S. Kozlov; Svetlana A. Terpugova; V. V. Pol’kin; Elena P. Yausheva; D. G. Chernov; T. B. Zuravleva; T. V. Bedareva; S. L. Odintsov; V. D. Burlakov; M. Yu. Arshinov; G. A. Ivlev; Denis Savkin; A. V. Fofonov; V. A. Gladkikh; A. P. Kamardin; D. B. Belan; M. V. Grishaev; V. V. Belov; S. V. Afonin; Yu. S. Balin; Grigorii P. Kokhanenko
The main aim of the work was complex experimental measurements of microphysical, chemical, and optical parameters of aerosol particles in the surface air layer and free atmosphere. From the measurement data, the entire set of aerosol optical parameters was retrieved, required for radiation calculations. Three measurement runs were carried out in 2013 within the experiment: in spring, when the aerosol generation maximum is observed, in summer (July), when the altitude of the atmospheric boundary layer is the highest, and in the late summer – early autumn, when the second nucleation period is recorded. The following instruments were used in the experiment: diffusion aerosol spectrometers (DAS), GRIMM photoelectric counters, angle-scattering nephelometers, aethalometer, SP-9/6 sun photometer, СЕ 318 Sun-Sky radiometer (AERONET), MS-53 pyrheliometer, MS-802 pyranometer, ASP aureole photometer, SSP scanning photometer, TU-134 Optik flying laboratory, Siberian lidar station, stationary multiwave lidar complex LOZA-M, spectrophotometric complex for measuring total ozone and NO2, multivariable instrument for measuring atmospheric parameters, METEO-2 USM, 2.4 AEHP-2.4m station for satellite data receive. Results of numerical calculations of solar down-fluxes on the Earth’s surface were compared with the values measured in clear air in the summer periods in 2010—2012 in a background region of Siberian boreal zone. It was shown that the relative differences between model and experimental values of direct and total radiation do not exceed 1% and 3%, respectively, with accounting for instrumental errors and measurement error of atmospheric parameters. Thus, independent data on optical, meteorological, and microphysical atmospheric parameters allow mutual intercalibration and supplement and, hence, provide for qualitatively new data, which can explain physical nature of processes that form the vertical structure of the aerosol filed.
Japan Geoscience Union | 2017
Sergey Borisovich Belan; Jean-Daniel Paris; Phillip Nedelek; P. N. Antokhin; Victoriya Arshinova; Mikhail Arshinov; Boris D. Belan; D. V. Davydov; G. A. Ivlev; Alexander Fofonov; A. V. Kozlov; T. M. Rasskazchikova; Denis Savkin; D. V. Simonenkov; Tatyana K. Sklyadneva; Gennadii N. Tolmachev
EPJ Web of Conferences | 2016
G. G. Matvienko; Boris D. Belan; M. V. Panchenko; O. A. Romanovskii; S. M. Sakerin; D. M. Kabanov; S. A. Turchinovich; Yu. S. Turchinovich; T. A. Eremina; V. S. Kozlov; Svetlana A. Terpugova; V. V. Pol’kin; Elena P. Yausheva; D. G. Chernov; T.B. Zuravleva; T.V. Bedareva; S.L. Odintsov; V. D. Burlakov; M. Yu. Arshinov; G. A. Ivlev; Denis Savkin; A. V. Fofonov; V.A. Gladkikh; A.P. Kamardin; Yu. S. Balin; Grigorii P. Kokhanenko; Ioganes E. Penner; S. V. Samoilova; P. N. Antokhin; V. G. Arshinova
The EGU General Assembly | 2015
Boris D. Belan; Mikhail Arshinov; Jean-Daniel Paris; Philippe Nédélec; Gérard Ancellet; Jacques Pelon; Antoine Berchet; Emmanuel Arzoumanian; Sergey Borisovich Belan; Johannes E. Penner; Yurii S. Balin; Grigorii P. Kokhanenko; D. K. Davydov; G. A. Ivlev; A. V. Kozlov; A. S. Kozlov; Dmitrii G. Chernov; Alexader V. Fofonov; D. V. Simonenkov; Gennadii N. Tolmachev
Archive | 2010
Boris D. Belan; G. A. Ivlev; A. V. Kozlov; T. M. Rasskazchikova; D. V. Simonenkov; Gennadii N. Tolmachev; Nadezhda Fokina; Aleksandr Fofonov