Variability of D-region electron densities at Tromso
Abstract
The 2.75 MHz partial-reflection radar at Ramfjordmoen near Tromso has been used for a study of D-region electron densities by the differential-absorption method on a number of days during 1978-79. Received signals are generally stratified in several layers, typically over 60-80 km. Strong stable echoes are seen down to 55 km during periods of enhanced riometer absorption. Inferred electron densities vary between about 100-1000 per cu cm at about 60-80 km and show well-defined features which persist for about 10-20 min. During periods of high absorption, enhanced electron densities about 600 cm per cu cm are observed below 65 km. During a polar cap absorption event, the inferred electron densities at 60-70 km show a very stable profile. Possible sources of D-region ionization at high latitudes are briefly discussed.
- Publication:
-
Journal of Atmospheric and Terrestrial Physics
- Pub Date:
- April 1982
- DOI:
- 10.1016/0021-9169(82)90076-9
- Bibcode:
- 1982JATP...44..313R
- Keywords:
-
- D Region;
- Electron Density Profiles;
- Ionospheric Electron Density;
- Polar Cap Absorption;
- Radar Reflectors;
- Atmospheric Ionization;
- Atmospheric Stratification;
- High Frequencies;
- Ionospheric Propagation;
- Norway;
- Polar Regions;
- Radar Echoes;
- Riometers;
- Solar Protons;
- Geophysics