XХХ International Symposium "Atmospheric and Ocean Optics. Atmospheric Physics"

July 01-05, 2024, St.Petersburg, Russia

Submitted reports

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Bazhenov O.E., Kharchenko O.V.
Chlorine oxide: an indicator and predictor of ozone destruction in the winter-spring Arctic stratosphere using Aura MLS observations
Kishcha Pavel
Impact of severe dust intrusion on surface water temperature in Lake Kinneret in the Eastern Mediterranean
Koval A.V.
ARCTIC STRATOSPHERE CHANGES IN THE 21ST CENTURY IN THE EARTH SYSTEM MODEL SOCOLV4
Zemlyanov A.A., Kochetov D.I., Zemlyanov Al.A., Donchenko V.A., Kravchenko I.V., Ryambov R.V.
ANGULAR DISTRIBUTION OF TWO-PHOTON EXCITED FLUORESCENCE OF AN AEROSOL OF ETHANOL DYE SOLUTION
Pavlinskiy Alexey Valerievich, Uymanova Valeria Alexandrovna
AIR TEMPERATURE TRENDS AND REPEATABILITY OF ADVERSE WEATHER PHENOMENA IN THE COASTAL ARCTIC ZONE
M.M.Efimov, N.M. Gavrilov
Verification of the method of maximum rate of atmospheric parameters change for determining the characteristics of sudden stratospheric warmings
S.A. Riabova, Ya.O. Romanovskii, D.B. Yakovlev, S.P. Soloviev, A.V. Krasheninnikov, S.Yu. Rybnov, Yu.S. Rybnov
Influence of air temperature on the concentration of aerosol particles smaller than 2.5 microns according toCenter for Geophysical Monitoring in Moscow of IDG RAS for May 2023
Marinayte I.I., Khodzher T.V., Shikhovtsev M.Yu., Lutskin Ye.S., Potyomkin V.L.
THE RESULTS OF EXPEDITION MEASUREMENTS OF РМ₁₀,PAH AND MERCURY ABOVE LAKE BAIKAL SUFACE IN AUGUST, 2023
Kostsov V.S., Ionov D.V., Andryukova A.B., Ryabushko E.P.
Derivation of the “land-sea” contrast of the cloud liquid water path from measurements of the SEVIRI satellite instrument: problems and analysis of results
Vasiliev M.S., Petrova A.N.
CHANGES IN THE DURATION OF THE COLD PERIOD IN THE ARCTIC ZONE OF YAKUTIA FOR 1991-2022
Zhuravleva T.B., Nasrtdinov I.M.
ANGULAR DISTRIBUTION OF REFLECTED SOLAR RADIATION AT THE LEVEL OF THE UNDERLYING SURFACE: INFLUENCE OF ANISOTROPY
Shamanaeva L.G., Potekaev A.I., Cherepanov O.S., Simakhin V.A.
Diurnal behavior of vertical gradients of wind speed and direction from minisodar data

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