It is shown how the electron distribution in the upper regions of the ionosphere may be determined from simultaneous measurements of the Doppler shifts of radio signals of two differen frequencies received from an artificial satellite. The method is illustrated in detail by computations made on the 20 and 40 Mc/s signals from Sputnik I
Applying a methodology developed and tested in previous studies, the contribution from t...
A computer simulation of the ionospheric experiment of the Apollo-Soyuz Test Project (ASTP) was perf...
Ground-based ionosphere sounding measurements alone are incapable of reliably modeling the topside e...
356-367Since the launch of Sputnik I in 1957, satellite radio beacons have been used to measure the ...
Existing radar aids for the research of the ionosphere and ionosondes allow only local diagnostics o...
Differential Doppler measurements of signals from NNSS Navigational Satellites can be used to give t...
134-138Electron density profiles from the Alouctte-II satellite are used to study the latitudinal di...
Ground-based incoherent scatter radar studies of the upper part of the F2 layer are capable of provi...
Ground-based incoherent scatter radar studies of the upper part of the F2 layer are capable of provi...
Ground-based incoherent scatter radar studies of the upper part of the F2 layer are capable of provi...
A new experimental technique is presented for the determination of the total electron content (TEC) ...
Radio-frequency signals originating on Earth and recorded in space allow retrieval of ionospheric pa...
The Ørsted Satellite has performed limb-sounding observations of the ionosphere. The observed Satell...
Simultaneous use of ionograms and observations of cosmic radio noise taken at New Delhi (at 22.4 mc/...
The method of plotting a spatial distribution pattern of the total electron content (TEC) in the reg...
Applying a methodology developed and tested in previous studies, the contribution from t...
A computer simulation of the ionospheric experiment of the Apollo-Soyuz Test Project (ASTP) was perf...
Ground-based ionosphere sounding measurements alone are incapable of reliably modeling the topside e...
356-367Since the launch of Sputnik I in 1957, satellite radio beacons have been used to measure the ...
Existing radar aids for the research of the ionosphere and ionosondes allow only local diagnostics o...
Differential Doppler measurements of signals from NNSS Navigational Satellites can be used to give t...
134-138Electron density profiles from the Alouctte-II satellite are used to study the latitudinal di...
Ground-based incoherent scatter radar studies of the upper part of the F2 layer are capable of provi...
Ground-based incoherent scatter radar studies of the upper part of the F2 layer are capable of provi...
Ground-based incoherent scatter radar studies of the upper part of the F2 layer are capable of provi...
A new experimental technique is presented for the determination of the total electron content (TEC) ...
Radio-frequency signals originating on Earth and recorded in space allow retrieval of ionospheric pa...
The Ørsted Satellite has performed limb-sounding observations of the ionosphere. The observed Satell...
Simultaneous use of ionograms and observations of cosmic radio noise taken at New Delhi (at 22.4 mc/...
The method of plotting a spatial distribution pattern of the total electron content (TEC) in the reg...
Applying a methodology developed and tested in previous studies, the contribution from t...
A computer simulation of the ionospheric experiment of the Apollo-Soyuz Test Project (ASTP) was perf...
Ground-based ionosphere sounding measurements alone are incapable of reliably modeling the topside e...