e o herent scatter radar and DPS-4 ionosonde. The height profiles of the TID propagation characteristics are obtained by means of cross-and their ionospheric manifestation, travelling ionospheric et al., 1998) and MU radar (Oliver et al., 1988). Herewith only Ma et al. (1998) have investigated the complete wave propagation vector of TIDs as function of height. In this (Reinisch et al., 1997) data are presented. The both tools DPS-4 ionograms have been manually scaled with the interactive ionogram scaling technology described by Rei-nisch et al. (2004). The electron density profiles were con-structed from the ionogram traces using the Reinisch and Huang (1983) method with the extrapolation above a pea
When applying the ray tracing in ionospheric propagation, the electron density modelling is the main...
A campaign was conducted in late September 1991 to obtain experimental measurements for use in ionos...
The reconstruction of the vertical electron-density profile is a fundamental problem in ionospheric ...
The spatiotemporal structure of TID characteristics is studied on the base of the electron density p...
The paper is devoted to the comparison of the electron density obtained by the incoherent scatter ra...
Characteristic signatures are often observed in HF radar range-time-intensity plots when travelling...
The ionospheric vertical sounding is a basic technique for studying the Earth’s ionosphere. Taking i...
This paper first discusses some early results (most hitherto unpublished) on off-vertical reflection...
Travelling Ionospheric Disturbances (T.I.D.s) are perturbations of the plasma in the ionosphere caus...
In spite of being interrupted several times in its long history of operation since 1950, the routine...
International audienceMost recent methods in ionospheric tomography are based on the inversion of th...
The various manifestations of TID in ionograms received with minute periodicity by Kazan (55°N, 48°E...
The reconstruction of the vertical electron-density profile is a fundamental problem in ionospheric...
203-206A method is presented for ray tracing from electron density information provided by a vertica...
topside ionograms in the 1960s and 1970s with a multinational network of ground stations that provid...
When applying the ray tracing in ionospheric propagation, the electron density modelling is the main...
A campaign was conducted in late September 1991 to obtain experimental measurements for use in ionos...
The reconstruction of the vertical electron-density profile is a fundamental problem in ionospheric ...
The spatiotemporal structure of TID characteristics is studied on the base of the electron density p...
The paper is devoted to the comparison of the electron density obtained by the incoherent scatter ra...
Characteristic signatures are often observed in HF radar range-time-intensity plots when travelling...
The ionospheric vertical sounding is a basic technique for studying the Earth’s ionosphere. Taking i...
This paper first discusses some early results (most hitherto unpublished) on off-vertical reflection...
Travelling Ionospheric Disturbances (T.I.D.s) are perturbations of the plasma in the ionosphere caus...
In spite of being interrupted several times in its long history of operation since 1950, the routine...
International audienceMost recent methods in ionospheric tomography are based on the inversion of th...
The various manifestations of TID in ionograms received with minute periodicity by Kazan (55°N, 48°E...
The reconstruction of the vertical electron-density profile is a fundamental problem in ionospheric...
203-206A method is presented for ray tracing from electron density information provided by a vertica...
topside ionograms in the 1960s and 1970s with a multinational network of ground stations that provid...
When applying the ray tracing in ionospheric propagation, the electron density modelling is the main...
A campaign was conducted in late September 1991 to obtain experimental measurements for use in ionos...
The reconstruction of the vertical electron-density profile is a fundamental problem in ionospheric ...