Simultaneous Satellite and Ground Based Observations of Polar Cap Phenomena

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Evidence for an extended reconnection line at the dayside magnetopause
Large Field Events in the Distant Magnetotail During Magnetic Storms
Anisotropy Reversals in the Distant Magnetotail and Their Association with Magnetospheric Substorms
On the Determination of a Moving MHD Structure : Minimization of the Residue of Integrated Faraday's Equation
Structure and Kinetic Properties of Plasmoids and Their Boundary Regions
A Quasi-stagnant Plasmoid Observed With Geotail on October 15, 1993
Leakage Ions from the LLBL to MSBL : Confirmation of Reconnection Events at the Dayside Magnetopause
On the Origin of the Upstream Diffuse Ions : Case Studies from GEOTAIL Observations
Investigation of electron density profile in the lower ionosphere by SRP-4 rocket experiment
Low Frequency plasma wave Analyzer (LFA) onboard the PLANET-B spacecraft
Plasma Wave Observations with GEOTAIL Spacecraft
Distribution of Singly-Charged Oxygen Observed in a High-Density Region Flowing Tailward in the Plasma Sheet by GEOTAIL at X_--60Re
The Low Energy Particle (LEP) Experiment onboard the GEOTAIL Satellite
Propagation Characteristics of Auroral Hiss Observed by Akebono Satellite
Geotail Observations of an Unusual Magnetotail under Very Northward IMF Conditions
Simultaneous Satellite and Ground Based Observations of Polar Cap Phenomena
Signature of Electric Field Associated with Localized Electron Precipitation in the Polar Cap Region -Akebono (EXOS-D) Results-
Non-thermal electrons at the Earth's bow shock : A 'gradual' event
Automatic Waveform Selection method for Electrostatic Solitary Waves
Plasma Entry from the Flanks of the Near-Earth Magnetotail : GEOTAIL Observations in the Dawnside LLBL and the Plasma Sheet
Evidence of Two Active Reconnection Sites in the Distant Magnetotail
Magnetotail Convection in Geomagnetically Active Times 2. Dawn-Dusk Motion in the Plasma Sheet
magnetotail Convection in Geomagnetically Active Times 1. Distance to the Neutral Lines
Visualization of Shock Wave and Detonation Wave

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