CONFERENCES AND SYMPOSIA
V.E. ZUEV INSTITUTE OF ATMOSPHERIC OPTICS
XХIХ International Symposium "Atmospheric and Ocean Optics. Atmospheric Physics"
June 26-30, 2023, Moscow
Submitted reports
- Vinogradova A.A., Antonova V.M., Talovskaya A.V., Gubanova D.P.
Elemental composition of near-surface aerosol in Moscow under different winter conditions in 2020 and 2021 - Bobrovnikov S.M., Gorlov E.V., Zharkov V.I., Murashko S.N.
β-BAND SYSTEM OF THE FLUORESCENCE SPECTRUM OF PHOSPHORUS OXIDE - Karakhanyan A.A., Molodykh S.I.
Possibility to apply ionospheric electric potential in the problem of solar-troposphere relations
- Salnikov K.S., Shishko V.A., Konoshonkin A.V., Timofeev D.N., Kustova N.V., Borovoy A.G., Timofeev D.N., Kustova N.V., Borovoy A.G.
APPLICATION OF THE DISCRETE DIPOLE METHOD AND THE APPROXIMATION OF PHYSICAL OPTICS TO THE PROBLEM OF LIGHT SCATTERING BY ATMOSPHERIC ICE CRYSTALS OF CIRROUS CLOUDS FOR REMOTE SENSING PROBLEMS - Bazhenov O.E., Kharchenko O.V., Nevzorov A.V., Elnikov A.V., Loginov V.A.
Variations in total ozone content on territory of russia - Reyno V.V., Gerasimova L.O., Agafontsef M.V.
STUDY OF THERMAL INERTIA OF SAMPLES - Sutorikhin I.A., Kirillov V.V., Litvinenko S.A., Frolenkov I.M., , Churilova T.Ya., Efimova T.V., Moiseeva N. A.
HYDRO-OPTICS OF SECTIONS OF THE TELETSKOYE LAKE WATER AREA WITH DIFFERENT LEVELS OF NATURAL AND ANTHROPOGENIC IMPACT - Rodimova O.B.
ABSORPTION COEFFICIENT OF THE AR-BROADENED CO2 IN THE 4.3 μm BAND WING - Kryuchkov A.V., Filatov V.V., Gerasimova M.P., Sadovnikov S.A.
FIBER OPTIC ATMOSPHERIC METHANE METER - Petrova T.M., Solodov A.M., Solodov A.A., Deichuli V.M.
PARAMETERS OF THE HD16O ABSORPTION LINES IN THE SPECTRAL REGION OF 5100–5400 CM–1 BROADENED BY CARBON DIOXIDE PRESSURE - Nagovitsyna E.S., Dzholumbetov S.K., Poddubny V.A., Karasev A.A.
Usage of satellite measurements to assessment the fields of atmospheric aerosol by the method of fluid-location of the atmosphere - Lavygin I., Berngardt O.
Study of the spectral composition of waves in the lower ionospheric layers according to the data of the SuperDARN and SEKIRA radar using the ARIMA model