The ionospheric electron density peak (NmF2) is analyzed for the recent minima of solar activity for two mid-latitude stations, Rome (41.8°N, 12.5°E, geomagnetic latitude 41.7°N, Italy) and Gibilmanna (37.9°N, 14.0°E, geomagnetic latitude 37.6°N, Italy), and for the low-latitude station of Tucumán (26.9°S, 294.6°E, geomagnetic latitude 17.2°S, Argentina), located in the south ridge of the equatorial ionization anomaly. An inter-minima comparison reveals that from an ionospheric point of view the last minimum of solar activity (minimum 23/24) was peculiar, with values of NmF2 lower than those recorded during the previous minima for all the stations and all the hours of the day. A more pronounced decrease is observed at Tucumán than at Rome a...
Total electron content (TEC) over Tucumán (26.9°S, 294.6°W) measured with Faraday technique during t...
During the last decade the amount of ionosphere measurements, from ground and space born sources, ha...
The aim of this work is the analysis of the mid-latitude ionospheric trough (MIT) using the Global I...
The ionospheric electron density peak (NmF2) is analyzed for the recent minima of solar activity for...
In this paper we analyze the behaviour of the critical frequency of the F2 region of the ionosphere ...
Bottom side electron density profiles for two stations at the southern crest of the Equatorial Ioniz...
In this paper we analyze the behaviour of the critical frequency of the F2 region of the ionosphere(...
This study investigates the impacts of solar activity on the performance of the latest release of In...
18th EISCAT symposiumSession E3: Ionoshere/thermosphere/mesosphereMay 27 (Sat), Poster Sessio
Analysis of the seasonal, hemispheric and latitudinal variation of the ionospheric F2 peak during th...
The ionospheric peak electron density NmF2, simulated with the Coupled Thermosphere Ionosphere Plasm...
© 2016, Pleiades Publishing, Ltd.Based on an analysis of data from the European ionospheric stations...
Improved ionospheric modeling requires a better understanding of the relationship between ionospheri...
In this paper, we analyze daytime observations of the critical frequencies of the F2 (<i>fo</i>F2) ...
The thermosphere–ionosphere–mesosphere-electrodynamics coupled model TIME-GCM, coupled to NCEP lower...
Total electron content (TEC) over Tucumán (26.9°S, 294.6°W) measured with Faraday technique during t...
During the last decade the amount of ionosphere measurements, from ground and space born sources, ha...
The aim of this work is the analysis of the mid-latitude ionospheric trough (MIT) using the Global I...
The ionospheric electron density peak (NmF2) is analyzed for the recent minima of solar activity for...
In this paper we analyze the behaviour of the critical frequency of the F2 region of the ionosphere ...
Bottom side electron density profiles for two stations at the southern crest of the Equatorial Ioniz...
In this paper we analyze the behaviour of the critical frequency of the F2 region of the ionosphere(...
This study investigates the impacts of solar activity on the performance of the latest release of In...
18th EISCAT symposiumSession E3: Ionoshere/thermosphere/mesosphereMay 27 (Sat), Poster Sessio
Analysis of the seasonal, hemispheric and latitudinal variation of the ionospheric F2 peak during th...
The ionospheric peak electron density NmF2, simulated with the Coupled Thermosphere Ionosphere Plasm...
© 2016, Pleiades Publishing, Ltd.Based on an analysis of data from the European ionospheric stations...
Improved ionospheric modeling requires a better understanding of the relationship between ionospheri...
In this paper, we analyze daytime observations of the critical frequencies of the F2 (<i>fo</i>F2) ...
The thermosphere–ionosphere–mesosphere-electrodynamics coupled model TIME-GCM, coupled to NCEP lower...
Total electron content (TEC) over Tucumán (26.9°S, 294.6°W) measured with Faraday technique during t...
During the last decade the amount of ionosphere measurements, from ground and space born sources, ha...
The aim of this work is the analysis of the mid-latitude ionospheric trough (MIT) using the Global I...