HelioWebKibi International University, Japan
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I[Kibi International University, Japan]
PI["Parent Institutions (0)"]
CI["Child Institutions (0)"]
AW["Affiliated Works (15)"]
CA["Linked Collaborating Authors (0)"]
I== skos:broader ==>PI
CI== skos:broader ==>I
AW== affil ==>I
AW== author ==>CA
click PI "#parent-institutions"
click CI "#child-institutions"
click AW "#affiliated-works"
click CA "#collaborating-authors"
Parent Institutions [?]
Child Institutions [?]
Affiliated Works
sorted by decreasing year, and then by display-name
- Case Study of the Evolution of Global Ionospheric Convection during Substorms
- Stormtime Electric Fields at High-Equatorial Latitudes as Observed by the Magnetometers, Incoherent-Scatter Radar and Satellite
- Convection and overshielding electric fields in the global ionosphere as observed with magnetometers and SuperDARN during the geomagnetic storm on 14-15 December 2006
- The region-2 current driven model of the substorm
- Global ionospheric currents driven by the Region-2 field-aligned currents at the onset of substorms
- Polar-equatorial ionospheric electric field and currents driven by the Region-2 field-aligned currents during storm/substorms
- Equatorial counterelectrojets during geomagnetic storms and their possible dynamos in the magnetosphere
- Seasonal dependence of the substorm overshielding at the subauroral latitude
- Penetration of the Electric Field to Low Latitude During Stormtime PC5 Pulsations as Observed by the HF Doppler Measurements and Magnetometer Array
- Substorm electric fields at nightside low latitude
- Transmission of Stormtime Electric Field and Currents to the Mid-Equatorial Latitude Ionosphere in the Magnetosphere-Ionosphere-Ground Circuit
- ROCSAT and HF Doppler sounder observations of the DP2-type electric field during the global Pc5 magnetic pulsation event
- Transmission of the Magnetospheric Electric Fields to the Low Latitude Ionosphere during Storm and Substorms
- A Severe Erosion of the Plasmasphere Arising from the September 2017 Storm
- Identifying the Physical Mechanisms to Explain the Extreme Plasmaspheric Erosion for the September 2017 Storm