XXVI International Symposium "Atmospheric and Ocean Optics. Atmospheric Physics"
July 06-10, 2020, Moscow
Participant Organizations
Organization: V.E. Zuev Institute of Atmospheric Optics SB RAS, Tomsk, Russia
List of reports:
- Marichev V.N., Bochkosvky D.A.
STUDIES OF VARIABILITY OF THE CONTENT OF BACKGROUND AEROSOL IN THE STRATOSPHERE OVER TOMSK BY LIDAR MEASUREMENT DATA IN 2016-2019
- Marichev V.N., Bochkosvky D.A.
LIDAR RESEARCHES OF MANIFESTATIONS OF WINTER STRATOSPHERIC WARMING OVER TOMSK IN 2016-2020.
- Skorokhodov A.
COMPARISON OF CHARACTERISTICS FOR DIFFERENT CLOUD TYPES OVER THE TERRITORY OF WESTERN SIBERIA BASED ON MODIS AND VIIRS DATA IN THE DAYTIME AND NIGHTTIME
- Gladkikh V.A., Mamyshev V.P., Nevzorova I.V., Odintsov S.L.
Estimation of contributions from various-scale components of the wind vector and air temperature to turbulent heat fluxes in the atmospheric surface layer
- Gladkikh V.A., Mamyshev V.P., Nevzorova I.V., Odintsov S.L.
Statistics of components forming vertical turbulent heat fluxes in the atmospheric surface layer
- Konoshonkin A.V.
Simulation of diffuse solar radiation in a limb sensing scheme in the presence of crystal clouds
- Nasrtdinov I.M.
Algorithm for calculation of reflected solar radiation in the presence of broken clouds for a limb sensing scheme
- Simonova G.V., Turchinovich Yu.S., Makshtas A.P.
Studies of the carbon isotope composition of the atmospheric aerosol in the Spitsbergen and the Severnaya Zemlya archipelagos
- Belyakova I.A., Filinyuk O.V., Baikov A.N., Mamyshev V.P., Nikiforova O.Yu., Ponomarev Yu.N., Jafarova O.A.
Change in skin conductivity at weak low-frequency pulsed acoustic impact in children with pulmonary tuberculosis
- Lomakina N.Ya.
DISTRIBUTION FEATURES OF LOW STRATIFORM CLOUDS AND PRECIPITATION OVER THE SIBERIAN REGION
- Lomakina N.Ya.
MODERN TRENDS OF LONG-TERM CHANGE IN THE AMOUNT OF LOW STRATIFORM CLOUDS OVER THE SIBERIAN REGION
- Kustova N.V., Shishko V.A., Konoshonkin A.V, Timofeev D.N., Borovoi A.G.
The coherent and incoherent light scattering in the visinity of backscattering direction on the particles of cirrus clouds
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