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

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

Oral Reports

  1. Vasil'ev Denis Yu., Velmovsky P.V.
    Seasonal variability of surface temperature over the territory of Russia for 1930-2021  
  2. Balugin N.V., Fomin B.A., Yushkov V.A., Marichev V.N., Bochkovskii D.A.
    VERTICAL PROFILES OF AEROSOL LOADING OF THE STRATOSPHERE OBTAINED IN JOINT REMOTE LIDAR AND DIRECT AEROLOGICAL SONDE MEASUREMENTS  
  3. Terpugova S.A., Antonov A.V., Shmargunov V.P., Panchenko M.V.
    APPLICATION OF A DIFFUSION SPECTROMETER of AEROSOL TO STUDY THE CONDENSATION ACTIVITY OF NANOMETER PARTICLES
  4. Kravtsova N.S., Sadovnikov S.A., Yakovlev S.V., Gerasimova M.P., Tuzhilkin D.A., Vasilenko I.A., Nevzorov A.A., Sukhanov A.Ya.
    Lidar design and results of development of the lidar signal registration program
  5. Varlamova E.V., Solovyev V.S., Tomshin O.A.
    Features of snowmelt dynamics in Siberia under Arctic amplification
  6. Konovalov I.B., Golovushkin N.A.
    A model study of the impact of smokes from Siberian fires on precipitation intensity in the landscapes of Siberia and the eastern Arctic
  7. Nosov V.V., Lukin V.P., Nosov E.V., Torgaev A.V., Kovadlo P.G.
    ATMOSPHERIC TURBULENCE AT THE BAIKAL ASTROPHYSICAL OBSERVATORY
  8. V.N. Uzhegov, M.V. Panchenko, V.P. Shmargunov
    FEATURES OF THE SPECTRAL DEPENDENCE OF AEROSOL RADIATION ATTENUATION COEFFICIENTS IN NATURAL AND MODEL SMOKES    
  9. Chentsov A.V., Chesnokova T.Yu., Voronin B.A.
    Investigation of possibility to detect H219O radioactive isotopologue in laboratory conditions
  10. V.V. Nosov, V.P. Lukin, E.V. Nosov, A.V. Torgaev
    Determination of atmospheric turbulence regions with specified characteristics from meteorological measurements
  11. Nebosko E.Yu., Shpak K.A., Mikhailov E.F.
    DISPERSION CHARACTERISTICS OF ATMOSPHERIC AEROSOLS IN THE BOREAL FOREST ZONE OF CENTRAL SIBERIA ACCORDING TO MEASUREMENT DATA IN 2021-2022.  
  12. Schybanov E.B., Kalinskaya D.V.
    Estimation of the ground concentration of dust particles by variation of the sea reflectance