Cosmic ray intensity distribution perpendicular to solar equatorial plane at 1 A.U. during 1978-83

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

Annual Variations, Distribution (Property), Solar Cosmic Rays, Solar Position, Earth (Planet), Geomagnetism, Solar Activity

Scientific paper

The distribution of cosmic ray intensity perpendicular to solar equatorial plane, was investigated by using its yearly variation with respect to the heliolatitudinal position of the Earth, for the two intervals 1978 to 1980 and 1981 to 1983. The monthly mean values of two high latitude stations along with the solar and geomagnetic indices are used to derive the cosmic ray intensity distribution free from the changes due to variation in solar activity. The correction is found to be significant only during the interval 1976 to 1980. The results indicate a significant linear increase in cosmic ray intensity from north to south of solar equator, contrary to that observed during 1973 to 1975. No symmetrical gradients are found during the period of study, in agreement with earlier results.

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

Cosmic ray intensity distribution perpendicular to solar equatorial plane at 1 A.U. during 1978-83 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 Cosmic ray intensity distribution perpendicular to solar equatorial plane at 1 A.U. during 1978-83, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Cosmic ray intensity distribution perpendicular to solar equatorial plane at 1 A.U. during 1978-83 will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-756508

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