Zobrazeno 1 - 10
of 18
pro vyhledávání: '"M. G. Skoblin"'
Publikováno v:
Annales Geophysicae, Vol 13, Pp 532-540 (1995)
Daytime F2-layer positive storm effects at middle and lower latitudes in the winter thermosphere are analyzed using AE-C, ESRO-4 neutral gas composition data, ground-based ionosonde observations and model calculations. Different longitudinal secto
Externí odkaz:
https://doaj.org/article/861d1e49c031439a8b4913e15ea2be26
Autor:
M. G. Skoblin, M. Förster
Publikováno v:
Annales Geophysicae, Vol 13, Pp 277-284 (1995)
Mass spectrometer satellite observations show that a narrow region with steep latitudinal gradients of neutral composition is formed in the subauroral winter thermosphere during magnetic storms. In order to analyze the relative importance of indiv
Externí odkaz:
https://doaj.org/article/817fe9a0fca1412dbd2d55b75b8e4a6b
Publikováno v:
Annales Geophysicae, Vol 12, Pp 226-231 (1994)
Theoretical model calculations along with ground-based observations from Huancayo ionosonde station and ESRO-4 gas analyzer data, were used to estimate the contribution of neutral gas composition changes and E×B vertical plasma drift to the obse
Externí odkaz:
https://doaj.org/article/181c32ebc80c4e18813d5f6a48762d3f
Publikováno v:
Annals of Geophysics, Vol 39, Iss 4 (1996)
Monthly median f0F2 and M(3000)F2 ionospheric model, MQMF2, based on the multiquadric (MQ) method of spatial interpolation and a new ionospheric index MF2 describes the monthly median f0F2 and M(3000)F2 over Europe for any UT moment, month and level
Externí odkaz:
https://doaj.org/article/bc58013daac5425fad0a5e6fbc4a916d
Autor:
M. G. Skoblin, M. Förster
Publikováno v:
Annales Geophysicae, Vol 13, Iss 3, Pp 277-284 (0000)
Mass spectrometer satellite observations show that a narrow region with steep latitudinal gradients of neutral composition is formed in the subauroral winter thermosphere during magnetic storms. In order to analyze the relative importance of individu
Externí odkaz:
https://doaj.org/article/ca9f1e5b21f6481683b93d3028204d97
Publikováno v:
Annales Geophysicae, Vol 13, Iss 5, Pp 532-540 (0000)
Daytime F2-layer positive storm effects at middle and lower latitudes in the winter thermosphere are analyzed using AE-C, ESRO-4 neutral gas composition data, ground-based ionosonde observations and model calculations. Different longitudinal sectors
Externí odkaz:
https://doaj.org/article/5bbaa9b3c2ee408e80a8fba7fc1bafea
Publikováno v:
Annales Geophysicae, Vol 12, Iss 2/3, Pp 226-231 (0000)
Theoretical model calculations along with ground-based observations from Huancayo ionosonde station and ESRO-4 gas analyzer data, were used to estimate the contribution of neutral gas composition changes and E×B vertical plasma drift to the observed
Externí odkaz:
https://doaj.org/article/3cad2870de4948cc9b3ae3409e6e521e
Autor:
M. G. Skoblin, A. B. Bukharina, S. M. Nikiforov, Roman S. Ablizen, A. V. Pento, Alexander Makarov, Mikhail Monastyrskiy
Publikováno v:
Technical Physics. 65:1905-1911
A pulsed source of ions with ionization of the substance under study at atmospheric pressure by the UV radiation of laser plasma is numerically simulated. The calculations are based on an original mathematical model that describes evolution of an ens
Autor:
M. G. Skoblin, V. I. Kozlovskii, I. V. Sulimenkov, Alexander R. Pikhtelev, V. V. Zelenov, Vasily V. Filatov, Vladimir S Brusov
Publikováno v:
Journal of Analytical Chemistry. 72:1331-1339
The experimental results of a mass spectral analysis of volatile organic compounds in a gaseous sample, obtained using an original design of an ion source based on the Penning ionization of a gas sample by excited metastable inert gas atoms, are pres
Autor:
Alexander Makarov, D E Greenfield, I. A. Kopaev, S. S. Alimpiev, M. G. Skoblin, Mikhail A. Monastyrskiy
Publikováno v:
Quantum Electronics. 45:1171-1178
General theoretical approaches to the modelling of Coulomb effects in short ion bunches, developed previously by the authors, are applied in this paper to the calculation of multireflection mass-spectrometer systems. A separate module of the MASIM 3D