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Solar-Terrestrial Environment Laboratory Nagoya University | 論文
- Hard X-Ray Investigation of the Galactic Center Region with Suzaku(Chapter 5. The Galactic Center and Ridge Emissions, The Extreme Universe in the Suzaku Era)
- Iron and Nickel Line Diagnostics for the Galactic Center Diffuse Emission
- Discovery of a Possible X-Ray Counterpart to HESS J1804-216
- Balloon measurement of electric fields near the Harang discontinuity
- X-ray intensity, ozone density, and VLF wave intensity observed by scientific balloon experiments at Esrange
- Surface flow on the ablation area of the Lirung Galcier in Langtang Valley, Nepal Himalayas
- C Self-Focusing of Plasma Waves (Part III. Applications to the Collisionless Plasma in Fluid Model)
- Implications for Galaxy Evolution from Cosmic Evolution of the Supernova Rate Density
- Discovery of a Slow X-Ray Pulsator, AX J1740.1-2847, in the Galactic Center Region
- A New Eclipsing X-Ray Burster near the Galactic Center : A Quiescent State of the Old Transient A1742-289
- Preparation of Artficial Kosa Aerosol with Two Original Desert Sands
- Time Variability of the Geocoronal Solar-Wind Charge Exchange in the Direction of the Celestial Equator
- Detection of a Rare Supersoft Outburst Event during a Suzaku Observation of 1E 0102.2-7219
- NITRIC ACID TRANSPORT FROM THE STRATOSPHERE TO THE TROPOSPHERE AND ICE SHEET IN ANTARCTICA THROUGH POLAR STRATOSPHERE
- Micro-Turbulence in the Solar Wind at 5-76 Rs Observed with Interplanetary Scintillation
- Evolution of the Solar Wind Structure in the Acceleration Region during 1990-1993 (STEP Interval)
- Solar Wind Motion near the Sun Derived from Simultaneous Interplanetary Scintillation Observations at 2 GHz and 8 GHz
- Energetic particle precipitation in the Brazilian geomagnetic anomaly during the "Bastille Day storm" of July 2000
- Unusual ionospheric absorption characterizing energetic electron precipitation into the South Atlantic Magnetic Anomaly
- Magnetic Storm-Related Energetic Electrons Penetrating into the Magnetosphere, Deduced from Ground-Based Measurements of Resonant Waves