On the equatorial trough of F2-layer ionization

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

3

Atmospheric Ionization, Equatorial Atmosphere, Equatorial Electrojet, F 2 Region, Troughs, Alouette Satellites, Annual Variations, Diurnal Variations, Ionospheric Ion Density, Longitude, Magnetic Equator, Neutral Atmospheres, Solar Terrestrial Interactions, Solstices

Scientific paper

Data on f(0)F2 from the satellites Alouette and ISS-b are used to study the diurnal, seasonal and longitudinal variations of the location of the equatorial trough. The trough is located at about 40-100 km to the north of the magnetic equator, which can be explained by the systematic deviation of the equatorial electrojet towards the northern hemisphere. The trough is situated to the north of the mean trough during daytime and at the June solstice, while it is to the south by night and at the December solstice. These features are consistent with the neutral wind system inherent in different local hours and different seasons. There is also a marked declination effect of the trough location which is related to the subtropical crests of f(0)F2, and may also be related to the zonal wind as a secondary effect.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

On the equatorial trough of F2-layer ionization does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with On the equatorial trough of F2-layer ionization, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and On the equatorial trough of F2-layer ionization will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1833458

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.