Results 161 to 170 of about 114,060 (217)
TEC disturbances caused by CME-triggered geomagnetic storm of September 6-9, 2017. [PDF]
Uga CI, Gautam SP, Seba EB.
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A Survey of Current Operations-Ready Thermospheric Density Models for Drag Modeling in LEO Operations. [PDF]
Mutschler S +10 more
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From Foreshock 30-Second Waves to Magnetospheric Pc3 Waves. [PDF]
Turc L +9 more
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Juno Observations of Jupiter's Magnetodisk Plasma: Implications for Equilibrium and Dynamics. [PDF]
Liu ZY +10 more
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Magnetospheric Control of Ionospheric TEC Perturbations via Whistler-Mode and ULF Waves. [PDF]
Shen Y +6 more
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Variability of foF2 in the equatorial ionosphere
Advances in Space Research, 2004Abstract We have used data from two equatorial stations in the African longitude sector to study the monthly variability of foF2. Diurnal, seasonal, and solar activity effects were investigated. The data established by this study are proposed as equatorial input values for the development of a variability model for the International Reference ...
Dieter Bilitza, J O Adeniyi
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Equatorial ionospheric absorption
Journal of Atmospheric and Terrestrial Physics, 1956Abstract A study has been made of the variation of absorption with frequency and sun's zenith distance χ at Ibadan at vertical incidence. Since the propagation at Ibadan is almost purely transverse, simple theories in terms of doviative and nondeviative absorption may be applied.
Wright, R W, Skinner, N J
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Nature, 1966
A NUMBER of authors1–3 have shown that near the magnetic equator ionospheric drifts occur, in both the E and F regions, which are mainly westwards by day and mainly eastwards by night. Results for F region drifts at Ibadan have been given by Skinner, Lyon and Wright1 for the International Geophysical Year (IGY) (1957–58). These show that for quiet days
R. W. MORRISS, A. J. LYON
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A NUMBER of authors1–3 have shown that near the magnetic equator ionospheric drifts occur, in both the E and F regions, which are mainly westwards by day and mainly eastwards by night. Results for F region drifts at Ibadan have been given by Skinner, Lyon and Wright1 for the International Geophysical Year (IGY) (1957–58). These show that for quiet days
R. W. MORRISS, A. J. LYON
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Electric field in the equatorial ionosphere
Planetary and Space Science, 1992Abstract A model of the ionosphere as a global conductor is used to examine synchronous variations of electric fields and currents at high and low latitudes. The special form of a boundary value problem and a multigrid numerical method permit investigation of auroral field penetration to the equator.
V.V. Denisenko, S.S. Zamay
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Contemporary Physics, 1973
Abstract At the magnetic equator the Earth's magnetic field is completely horizontal. This provides a constraint on the motion of the charged particles that comprise the ionosphere and produces dis...
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Abstract At the magnetic equator the Earth's magnetic field is completely horizontal. This provides a constraint on the motion of the charged particles that comprise the ionosphere and produces dis...
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