Positive plasma anomalies appear during the main phase of geomagnetic storms at (sub)auroral latitudes, extending across the polar cap as tongue of ionisation (TOI). Physical mechanisms of TOI, including electrodynamic plasma transport and neutral wind forcing, are simulated with TIE-GCM during the superstorm of Nov. 2003. The simulations are compared with TEC observations and GNSS tomography. The electrodynamic transport (vertical ExB component in particular) is identified as the main mechanism controlling TOI anomaly during great storms (Dst < -300 nT). This makes the choice of high-latitude convection model critical for simulations
International audienceWe have utilised the near-global imaging capabilities of the Northern Hemisphe...
International audienceWe present two event studies illustrating the detailed relationships between p...
We present observations of the auroral expansions during two substorms, focusing on multistage inten...
During the main phase of geomagnetic storms, large positive ionospheric plasma density anomalies ari...
Various plasma anomalies appear at auroral latitudes, extending across the polar cap as a tongue of ...
Large-scale ionospheric plasma anomalies appear at high latitudes, extending across the polar cap as...
We focus on the ionospheric response of northern high-latitude region to the 6 April 2000 superstorm...
This study investigates the effects of November superstorms on the daytime-evening northern topside ...
A time-dependent, three-dimensional, multi-ion model of the global ionosphere-polar wind system was ...
We investigate large-scale plasma density increases occurring during the 22 October 1999 great storm...
This dissertation includes studies on the generation mechanisms and plasma characteristics of polar ...
Radio tomography and the EISCAT and Super-DARN radars have been used to identify long-lived, high-al...
This study focuses on the 31 March 2001 superstorm's evening and nighttime sectors. We specified for...
This study focuses on the 15 May 2005 geomagnetic superstorm and aims to investigate the global vari...
Geomagnetic storms on 7–8 September 2017 triggered severe ionospheric disturbances that had a seriou...
International audienceWe have utilised the near-global imaging capabilities of the Northern Hemisphe...
International audienceWe present two event studies illustrating the detailed relationships between p...
We present observations of the auroral expansions during two substorms, focusing on multistage inten...
During the main phase of geomagnetic storms, large positive ionospheric plasma density anomalies ari...
Various plasma anomalies appear at auroral latitudes, extending across the polar cap as a tongue of ...
Large-scale ionospheric plasma anomalies appear at high latitudes, extending across the polar cap as...
We focus on the ionospheric response of northern high-latitude region to the 6 April 2000 superstorm...
This study investigates the effects of November superstorms on the daytime-evening northern topside ...
A time-dependent, three-dimensional, multi-ion model of the global ionosphere-polar wind system was ...
We investigate large-scale plasma density increases occurring during the 22 October 1999 great storm...
This dissertation includes studies on the generation mechanisms and plasma characteristics of polar ...
Radio tomography and the EISCAT and Super-DARN radars have been used to identify long-lived, high-al...
This study focuses on the 31 March 2001 superstorm's evening and nighttime sectors. We specified for...
This study focuses on the 15 May 2005 geomagnetic superstorm and aims to investigate the global vari...
Geomagnetic storms on 7–8 September 2017 triggered severe ionospheric disturbances that had a seriou...
International audienceWe have utilised the near-global imaging capabilities of the Northern Hemisphe...
International audienceWe present two event studies illustrating the detailed relationships between p...
We present observations of the auroral expansions during two substorms, focusing on multistage inten...