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www.ann-geophys.net/24/751/2006/ © European Geosciences Union 2006
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Simultaneous observations at different altitudes of ionospheric backscatter in t...
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Simultaneous observations at di€erent altitudes of ionospheric backscatter in th...
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Simultaneous observations at different altitudes of ionospheric backscatter in t...
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HF radar polar patch formation revisited: summer and winter variations in daysid...
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A comparison of optical and coherent HF radar backscatter observations of a post...
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A comparison of optical and coherent HF radar backscatter observations of a post...
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Joule heating hot spot at high latitudes in the afternoon sector
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A case study of HF radar spectra and 630.0 nm auroral emission in the pre-midnig...
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A case study of HF radar spectra and 630.0 nm auroral emission in the pre midnig...
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A comparison of velocity measurements from the CUTLASS Finland radar and the EIS...
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A comparison of velocity measurements from the CUTLASS Finland radar and the EIS...
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A comparison of F-region ion velocity observations from the EISCAT Svalbard and...
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Letter to the Editor: A comparison of F-region ion velocity observations from th...
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E.: Multi-instrument study of the dynamic cusp during dominant IMF By conditions...
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A comparison of velocity measurements from the CUTLASS Finland radar and the EIS...
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An inter-hemispheric, statistical study of nightside spectral width distribution...
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Investigation of the relationship between optical auroral forms and HF radar E r...
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Investigation of the relationship between optical auroral forms and HF radar E r...
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Geophysics. Cosmic physics
Physics
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QC1-999
QC801-809
Science
Physical Sciences
Science & Technology
Astronomy & Astrophysics
Geology
Geosciences
Meteorology & Atmospheric Sciences
Multidisciplinary
ionosphere
INTERPLANETARY MAGNETIC-FIELD
HIGH-LATITUDE CONVECTION
magnetospheric physics
CONVECTION
FLUX-TRANSFER EVENTS
IR content
SMALL-SCALE IRREGULARITIES
auroral ionosphere
F-REGION
magnetopause
plasma convection
BACKSCATTER
BOUNDARY-LAYER
CUTLASS FINLAND RADAR
DAYSIDE AURORAL ACTIVITY
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