Zobrazeno 1 - 10
of 64
pro vyhledávání: '"Aleksey V. Nevzorov"'
Publikováno v:
International Journal of Optics, Vol 2012 (2012)
The lidar measurements (Tomsk: 56.5∘N; 85.0∘E) of the optical characteristics of the stratospheric aerosol layer (SAL) in the volcanic activity period 2006–2011 are summarized and analyzed. The background SAL state with minimum aerosol content,
Externí odkaz:
https://doaj.org/article/159e360ea94d471d8b88dbc773044aa9
Publikováno v:
28th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics.
Autor:
Aleksey V. Nevzorov, Andrey P. Makeev, Aleksey A. Nevzorov, Aleksandr I. Nadeev, Nikolay G. Zaitsev
Publikováno v:
28th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics.
Autor:
Oleg E. Bazhenov, Aleksey V. Nevzorov, Sergey V. Smirnov, Andrey V. Elnikov, Vadim A. Loginov
Publikováno v:
28th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics.
Autor:
Oleg E. Bazhenov, Aleksey V. Nevzorov
Publikováno v:
28th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics.
Publikováno v:
28th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics.
Publikováno v:
28th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics.
Publikováno v:
Atmospheric and Oceanic Optics. 34:411-416
We present the decadally averaged time series of the total ozone content and integrated aerosol backscattering coefficient over Tomsk in the period of 2000–2016, obtained using the М-124 ozonometer and lidar method, respectively. The relationship
Publikováno v:
Optical Memory and Neural Networks. 30:146-156
Lidar observations of aerosol and ozone, carried out at Siberian Lidar Station (SLS) of Institute of Atmospheric Optics, Siberian Branch, Russian Academy of Sciences in Tomsk (56°29′ N; 85°3′ E), showed the presence of stratospheric aerosol lay
Publikováno v:
Atmospheric and Oceanic Optics. 33:622-628
Lidar observations at Siberian Lidar Station (SLS) of the Institute of Atmospheric Optics, Siberian Branch, Russian Academy of Sciences, in Tomsk (56.5° N; 85.0° E) showed the presence of stratospheric aerosol layers, descent of air masses, and def