Zobrazeno 1 - 7
of 7
pro vyhledávání: '"E. I. Astafyeva"'
Publikováno v:
Annales Geophysicae, Vol 26, Pp 335-344 (2008)
We developed a method and programs for estimation of the global electron content (GEC) from GPS measurements, using the ionosphere models IRI-2001 and NeQuick. During the 23rd cycle of solar activity, the value of GEC varied from 0.8 to 3.2×1032
Externí odkaz:
https://doaj.org/article/6a4f266a240f42a9afac2f2d62130da3
Publikováno v:
Cosmic Research. 49:227-239
The evolution of seismo-ionospheric disturbances accompanied strong destructive earthquakes in the region of Kuril and Japan Islands on October 4, 1994, September 25, 2003, and November 15, 2006 is studied in the paper. For determination of the dynam
Publikováno v:
Geomagnetism and Aeronomy. 48:187-200
Global electron content (GEC) as a new ionospheric parameter was first proposed by Afraimovich et al. [2006]. GEC is equal to the total number of electrons in the near-Earth space. GEC better than local parameters reflects the global response to a ch
Publikováno v:
Annales Geophysicae, Vol 26, Pp 335-344 (2008)
Annales Geophysicae, Vol 26, Iss 2, Pp 335-344 (2008)
ResearcherID
Annales Geophysicae, Vol 26, Iss 2, Pp 335-344 (2008)
ResearcherID
We developed a method and programs for estimation of the global electron content (GEC) from GPS measurements, using the ionosphere models IRI-2001 and NeQuick. During the 23rd cycle of solar activity, the value of GEC varied from 0.8 to 3.2×1032 ele
Publikováno v:
Advances in Space Research. 41:1459-1462
By using data from GPS receivers we detected huge-amplitude solitary large-scale traveling acoustic-gravity waves (LS AGW) which manifested themselves as perturbations of total electron content (TEC) of duration of about 40 min. Originated in the aur
Publikováno v:
Advances in Space Research. 39:1313-1317
We proposed a method for calculation of global or regional maps of velocities of total electron content isolines (TECIL) displacements. Applying of our method to the global ionosphere maps allows us to obtain additional information about the ionosphe
Publikováno v:
Doklady Earth Sciences. 409:921-924