The electron density in the lower ionosphere

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

2

Scientific paper

The amplitudes of the partial reflections obtained from heights between 60 and 120 km, on frequencies of 720 and 1420 kc/s, wore measured over a period of 2 years. The results indicate a mean electron density in the D-region 1·8 times greater than the values reported by other workers. This difference is caused by an increase of four times in the D-region ionization over the last sunspot cycle. The anomalous absorption in winter is caused by an increase of about 80 per cent in the ionization at heights below 90 km. An increase of the order of 500 electrons/cm3, at heights down to 60 km, is responsible for radio fade-outs. Some total reflections were obtained from a height of 90 km at noon, indicating a density of 20,000 electrons/cm3 and a gradient of 10,000 electrons/cm3 per km at this height. Total reflections from this 90 km layer were also obtained near sunset, and showed a very rapid increase in height immediately after ground sunset. Reflections obtained from clouds of ionization at night indicate gradients of up to 10,000 electrons/cm3 per km at heights of 80-115 km.

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

The electron density in the lower ionosphere 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 The electron density in the lower ionosphere, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and The electron density in the lower ionosphere will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1159627

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