Particle precipitation plays a key role in the coupling of the terrestrial magnetosphere and ionosphere by modifying the upper atmospheric conductivity and chemistry, driving field-aligned currents, and producing aurora. Yet quantitative observations of precipitating fluxes are limited, since ground-based instruments can only provide indirect measurements of precipitation, while particle telescopes aboard spacecraft merely enable point-like in situ observations with an inherently coarse time resolution above a given location. Further, orbit timescales generally prevent the analysis of whole events. On the other hand, global magnetospheric simulations can provide estimations of particle precipitation with a global view and higher time resolu...
Using the data from the Analyzer of Space Plasma and Energetic Atoms (ASPERA-3) experiment on board ...
International audienceDMSP F6 and F7 spacecraft observations of the average electron and ion energy,...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/95215/1/jgra18503.pd
Particle precipitation plays a key role in the coupling of the terrestrial magnetosphere and ionosph...
The precipitation of charged particles from the magnetosphere into the ionosphere is one of the cruc...
Particle precipitation is a central aspect of space weather, as it strongly couples the magnetospher...
Particle precipitation is a central aspect of space weather, as it strongly couples the magnetospher...
One of the most noticeable effects of solar–terrestrial physics is the aurora which regularly appear...
Data from the Far Ultraviolet Imager (FUV) on the Imager for Magnetopause-to-Aurora Global Explorati...
The brightness of proton aurora observed near solar maximum at summer and winter solstices with the ...
[1] On April 28 2001, simultaneous global images of electron and proton aurora were obtained by IMAG...
The Far Ultraviolet (FUV) imaging system on board the IMAGE satellite provides a global view of the ...
Observations with the FUV imagers on board the IMAGE satellite have been used to map the auroral ele...
In regions of thin strong current sheets, the first adiabatic invariant of protons can be violated l...
International audienceDMSP F7 spacecraft observations for the whole of 1986 were used to construct t...
Using the data from the Analyzer of Space Plasma and Energetic Atoms (ASPERA-3) experiment on board ...
International audienceDMSP F6 and F7 spacecraft observations of the average electron and ion energy,...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/95215/1/jgra18503.pd
Particle precipitation plays a key role in the coupling of the terrestrial magnetosphere and ionosph...
The precipitation of charged particles from the magnetosphere into the ionosphere is one of the cruc...
Particle precipitation is a central aspect of space weather, as it strongly couples the magnetospher...
Particle precipitation is a central aspect of space weather, as it strongly couples the magnetospher...
One of the most noticeable effects of solar–terrestrial physics is the aurora which regularly appear...
Data from the Far Ultraviolet Imager (FUV) on the Imager for Magnetopause-to-Aurora Global Explorati...
The brightness of proton aurora observed near solar maximum at summer and winter solstices with the ...
[1] On April 28 2001, simultaneous global images of electron and proton aurora were obtained by IMAG...
The Far Ultraviolet (FUV) imaging system on board the IMAGE satellite provides a global view of the ...
Observations with the FUV imagers on board the IMAGE satellite have been used to map the auroral ele...
In regions of thin strong current sheets, the first adiabatic invariant of protons can be violated l...
International audienceDMSP F7 spacecraft observations for the whole of 1986 were used to construct t...
Using the data from the Analyzer of Space Plasma and Energetic Atoms (ASPERA-3) experiment on board ...
International audienceDMSP F6 and F7 spacecraft observations of the average electron and ion energy,...
Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/95215/1/jgra18503.pd