The non-collisional interaction between conducting obstacles and magne-tized plasma winds can be found in different scenarios, from the interaction occurring between regions inside galaxy clusters to the interaction between the solar wind and Mars, Venus, active comets or even the interaction between Ti-tan and the Saturnian’s magnetospheric flow. These objects generate, through several current systems, perturbations in the streaming magnetic field leading to its draping around the obstacle’s effective conducting surface. Recent ob-servational results suggest that several properties associated with the magnetic field draping, such as the location of the polarity reversal layer of the induced magnetotail, are affected by variations in the co...
A fully three-dimensional, nonlinear, time-dependent, multi-layered spherical kinematic dynamo model...
International audienceOrientations of the observed magnetic field in Earth's dayside magnetosheath a...
The solar wind interaction with the non-magnetic Venerean ionospheric obstacle is unique. Ionospheri...
The noncollisional interaction between conducting obstacles and magnetized plasma winds can be found...
International audienceMost planetary bodies are moving in the solar wind, in a stellar wind, or in a...
This study addresses the issue of the electromagnetic interactions between a stellar wind and planet...
Magnetic field draping occurs when the magnetic field lines frozen in a plasma flow wrap around a bo...
In this paper, we examined plasma structures (filaments), observed in the dayside magnetosphere but ...
Plasma, a gas of charged particles exhibiting collective behaviour, can be found everywhere in our v...
When the interplanetary magnetic field (IMF) encounters the Earth's magnetosphere, it is compressed ...
A planet's magnetosheath extends from downstream of its bow shock up to the magnetopause, where the ...
An asymmetrical pileup of the interplanetary magnetic field leads to an additional draping of the fi...
A fully three-dimensional, nonlinear, time-dependent, multi-layered spherical kinematic dynamo model...
International audienceAn asymmetrical pileup of the interplanetary magnetic field (IMF) leads to an ...
Titan and Venus are both unmagnetized bodies enveloped by induced magnetospheres created within the ...
A fully three-dimensional, nonlinear, time-dependent, multi-layered spherical kinematic dynamo model...
International audienceOrientations of the observed magnetic field in Earth's dayside magnetosheath a...
The solar wind interaction with the non-magnetic Venerean ionospheric obstacle is unique. Ionospheri...
The noncollisional interaction between conducting obstacles and magnetized plasma winds can be found...
International audienceMost planetary bodies are moving in the solar wind, in a stellar wind, or in a...
This study addresses the issue of the electromagnetic interactions between a stellar wind and planet...
Magnetic field draping occurs when the magnetic field lines frozen in a plasma flow wrap around a bo...
In this paper, we examined plasma structures (filaments), observed in the dayside magnetosphere but ...
Plasma, a gas of charged particles exhibiting collective behaviour, can be found everywhere in our v...
When the interplanetary magnetic field (IMF) encounters the Earth's magnetosphere, it is compressed ...
A planet's magnetosheath extends from downstream of its bow shock up to the magnetopause, where the ...
An asymmetrical pileup of the interplanetary magnetic field leads to an additional draping of the fi...
A fully three-dimensional, nonlinear, time-dependent, multi-layered spherical kinematic dynamo model...
International audienceAn asymmetrical pileup of the interplanetary magnetic field (IMF) leads to an ...
Titan and Venus are both unmagnetized bodies enveloped by induced magnetospheres created within the ...
A fully three-dimensional, nonlinear, time-dependent, multi-layered spherical kinematic dynamo model...
International audienceOrientations of the observed magnetic field in Earth's dayside magnetosheath a...
The solar wind interaction with the non-magnetic Venerean ionospheric obstacle is unique. Ionospheri...