https://ogma.newcastle.edu.au/vital/access/ /manager/Index ${session.getAttribute("locale")} 5 Ground magnetometer observation of a cross-phase reversal at a steep plasmapause https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:3254 Wed 11 Apr 2018 17:06:56 AEST ]]> Mass and electron densities in the inner magnetosphere during a prolonged disturbed interval https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:3259 Wed 11 Apr 2018 16:08:23 AEST ]]> EMIC waves observed by Cluster near the plasmapause https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:17370 E. Wave polarization appeared to be associated with plasma density, with left hand in the equatorial region, right hand at higher latitudes nearer the plasmapause, and a mixture between.Wave normal angles were typically <60°, and Poynting flux measurements show that wave energy was predominantly directed along the geomagnetic field toward high latitudes in both hemispheres. These results suggest that the plasma density and its gradient play a significant role in confining the wave source region and affecting the wave properties, which will help understand wave generation and propagation mechanisms in the magnetosphere plasma environment.]]> Wed 11 Apr 2018 11:32:27 AEST ]]> Monitoring the plasmapause using geomagnetic field line resonances https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:2003 Wed 11 Apr 2018 10:37:04 AEST ]]> Doppler clutter in HF radar systems produced by ULF waves https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:14033 Wed 11 Apr 2018 09:25:20 AEST ]]> Is the plasmapause a preferred source region of electromagnetic ion cyclotron waves in the magnetosphere? https://ogma.newcastle.edu.au/vital/access/ /manager/Repository/uon:1121 Sat 24 Mar 2018 08:32:00 AEDT ]]>