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study of dynamical variation of particles and waves in the inner magnetosphere using ground-based network observations.
This can be verified from Fig. 7a c, in which the time variation of particles fraction is shown.
A significant variation of particles velocity along the detonation plume is observed.
We started a new project called the PWING project (study of dynamical variation of particles and waves in the inner magnetosphere using ground-based network observations) in April 2016.
In situ measurements by Arase and ground-based measurements by the PWING (study of dynamical variation of Particles and Waves in the INner magnetosphere using Ground-based network observations) project can also contribute to understand the mechanism of plasma particle precipitation by wave particle interaction (Shiokawa et al. 2017).
These comprehensive datasets will contribute to the investigation of dynamical variation of particles and waves in the inner magnetosphere, which is one of the most important research topics in recent space physics, and the outcome of our research will improve safe and secure use of geospace around the Earth.
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An activity-correlated variation of particle concentrations was found.
As it can be seen, the variation of particle fraction with time is negligible.
The variation of particle size is owing to the irradiation wavelength.
Variation of particle size or additional coatings allow custom-design of workload release curves.
An advanced variation of Particle Swarm Optimization algorithm is used to solve the optimization problem.
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