Zobrazeno 1 - 10
of 35
pro vyhledávání: '"V. N. SHUBIN"'
Publikováno v:
Geomagnetism and Aeronomy. 62:S74-S86
Autor:
Ya. A. Sakharov, I. V. Mingalev, B. V. Kozelov, A. M. Merzly, Z. V. Suvorova, S. M. Chernyakov, V. N. Shubin, A. B. Talalaev, V. V. Tikhonov, M. V. Tikhonov, A. T. Yanakov, A. S. Kalishin
Publikováno v:
Bulletin of the Russian Academy of Sciences: Physics. 86:310-315
Publikováno v:
Geomagnetism and Aeronomy. 61:713-720
Autor:
A. M. Merzly, V. V. Tikhonov, V. N. Shubin, V. S. Mingalev, Z. V. Suvorova, A. B. Talalaev, Igor Mingalev
Publikováno v:
Geomagnetism and Aeronomy. 61:565-577
The predicted conditions of shortwave (SW) radio communication between a transmitter located at the midlatitudes and receivers located near the Norwegian and Barents seas are compared. The IRI-2016 and Global Dynamic Model of Ionosphere (GDMI) models
Publikováno v:
Geomagnetism and Aeronomy. 61:359-364
The properties of the annual asymmetry in the electron density of the F2-layer maximum NmF2 at noon are analyzed based on the global empirical model of the F2-layer critical frequency median (SDMF2 model). As a characteristic of this asymmetry, we us
Autor:
V. N. Shubin, I. V. Krasheninnikov
Publikováno v:
Geomagnetism and Aeronomy. 60:216-223
This paper considers the possibility of the deep trough formation in the integral amplitude–frequency dependence of the wave field at the classical limiting paths of a single-hop ionospheric radio waves propagation under conditions of low solar act
Autor:
V. N. Shubin, M. G. Deminov
Publikováno v:
Geomagnetism and Aeronomy. 59:429-440
A global dynamic model of the F2 layer of the ionosphere GDMF2 is designed to calculate foF2 in both quiet and geomagnetically disturbed conditions. The term “dynamic model” implies that the change in foF2 at middle, subauroral, and auroral latit
Autor:
V. N. Shubin, M. G. Deminov
Publikováno v:
Geomagnetism and Aeronomy. 58:348-355
The empirical model of the location of the main ionospheric trough (MIT) is developed based on an analysis of data from CHAMP satellite measured at the altitudes of ~350–450 km during 2000–2007; the model is presented in the form of the analytica
Publikováno v:
Geomagnetism and Aeronomy. 56:750-756
Based on an analysis of data from the European ionospheric stations at subauroral latitudes, it has been found that the main ionospheric trough (MIT) is not characteristic for the monthly median of the F2-layer critical frequency (foF2), at least for
Publikováno v:
Geomagnetism and Aeronomy. 55:609-622
A global model SMF2 (Satellite Model of F2 layer) of the F2-layer height was created. For its creation, data from the topside sounding on board the Interkosmos-19 satellite, as well as the data of radio occultation measurements in the CHAMP, GRACE, a