Incoherent scatter radar study of the impact of the meteoric influx on nocturnal E-region ionization

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

14

Planetology: Solar System Objects: Meteors, Ionosphere: Ionosphere/Atmosphere Interactions, Ionosphere: Ionization Mechanisms, Ionosphere: Midlatitude Ionosphere

Scientific paper

We use the Arecibo incoherent scatter radar data collected from 1987 to 1995 to study meteoric impact on the nocturnal E-region electron/ion content. The nighttime ionization is observed to increase after midnight, which we interpret to be due to increase in background meteoric input. The column incremental rate due to meteoric ionization between 0100 to 0600 LT is estimated to be 109/cm2/hr. Direct meteoric deposition is responsible for 60% of the total ionization in the morning hours in the altitude range of 97 to 114 km. Although there appears to be an increase in electron content during shower periods, there is not an one-to-one relation between meteor showers and E-region ionization enhancement.

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

Incoherent scatter radar study of the impact of the meteoric influx on nocturnal E-region 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 Incoherent scatter radar study of the impact of the meteoric influx on nocturnal E-region ionization, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Incoherent scatter radar study of the impact of the meteoric influx on nocturnal E-region ionization will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-991952

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