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journal:(Research)
An Acoustic Balloon-Borne Instrument to Measure Temperature Fine Structure Near the Tropopause
Anomalous E-region ion layers in twilight conditions. Experiment and model
A Novel, High Resolution Temperature Sensor for Balloon Applications
Appendix H - Problems with Incorporating a New D-Region Model into the IRI
Appendix I - Improving the 75 to 300 km Ion Composition Model of the IRI
Climatology of Ozone in the Troposphere and Lower Stratosphere Over the European Arctic
Comparison of the F2-Layer Half-Widths Given by the IRI with the Rocket Data
Comparison of the Midlatitude Model with Low-Latitude Ion Composition Data
Effective recombination coefficients in the D- and E-regions during auroral absorption events
Electron Temperature Dependence of PMSE Power: Experimental and Modelling Results
Energetic Electron Precipitation During Auroral Events Observed by Incoherent Scatter Radar
ESRAD/EISCAT polar mesosphere winter echoes during MAGIC and ROMA
Formation mechanisms for low-altitude sporadic-E layers - Results from the METAL campaign
Formation mechanisms for low-altitude sporadic-E layers - Results from the METAL campaign