Electric potential patterns obtained by the SuperDARN radar network are used as input to the Coupled Thermosphere-Ionosphere-Plasmasphere model, in an attempt to improve the modelling of the spatial distribution of the ionospheric plasma at high latitudes. Two case studies are considered, one under conditions of stable IMF Bz negative and the other under stable IMF Bz positive. The modelled plasma distributions are compared with sets of well-established tomographic reconstructions, which have been interpreted previously in multi-instrument studies. For IMF Bz negative both the model and observations show a tongue-of-ionisation on the nightside, with good agreement between the electron density and location of the tongue. Under Bz p...
Information derived from tomographic images has demonstrated the extreme variability of the ionosphe...
A few of the difficulties in accurately modelling high-latitude electron densities with a large-sca...
Various ionospheric plasma anomalies appear at auroral latitudes, extending across the polar cap as ...
Electric potential patterns obtained by the SuperDARN radar network are used as input to the Coupled...
Electric potential patterns obtained by the SuperDARN radar network are used as input to the Coupled...
The dayside high-latitude trough is a persistent feature of the post-noon wintertime auroral ionosp...
Radiotomography provides observations of ionospheric electron density structure on horizontal scales...
During the main phase of geomagnetic storms, large positive ionospheric plasma density anomalies ari...
The activities of the International Ionospheric Tomography Community open up new possibilities of si...
A series of radio tomography reconstructions from the University of Wales Aberystwyth receiver chain...
Results are presented from a multi-instrument study of the spatial distribution of the summertime, ...
Radio tomography and the EISCAT and Super-DARN radars have been used to identify long-lived, high-al...
Positive plasma anomalies appear during the main phase of geomagnetic storms at (sub)auroral latitu...
Large-scale ionospheric plasma anomalies appear at high latitudes, extending across the polar cap as...
Abstract. The tomographic reconstruction technique generates a two-dimensional latitude versus heigh...
Information derived from tomographic images has demonstrated the extreme variability of the ionosphe...
A few of the difficulties in accurately modelling high-latitude electron densities with a large-sca...
Various ionospheric plasma anomalies appear at auroral latitudes, extending across the polar cap as ...
Electric potential patterns obtained by the SuperDARN radar network are used as input to the Coupled...
Electric potential patterns obtained by the SuperDARN radar network are used as input to the Coupled...
The dayside high-latitude trough is a persistent feature of the post-noon wintertime auroral ionosp...
Radiotomography provides observations of ionospheric electron density structure on horizontal scales...
During the main phase of geomagnetic storms, large positive ionospheric plasma density anomalies ari...
The activities of the International Ionospheric Tomography Community open up new possibilities of si...
A series of radio tomography reconstructions from the University of Wales Aberystwyth receiver chain...
Results are presented from a multi-instrument study of the spatial distribution of the summertime, ...
Radio tomography and the EISCAT and Super-DARN radars have been used to identify long-lived, high-al...
Positive plasma anomalies appear during the main phase of geomagnetic storms at (sub)auroral latitu...
Large-scale ionospheric plasma anomalies appear at high latitudes, extending across the polar cap as...
Abstract. The tomographic reconstruction technique generates a two-dimensional latitude versus heigh...
Information derived from tomographic images has demonstrated the extreme variability of the ionosphe...
A few of the difficulties in accurately modelling high-latitude electron densities with a large-sca...
Various ionospheric plasma anomalies appear at auroral latitudes, extending across the polar cap as ...