Possible gleissberg periodicity in large fluence solar proton events

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

Scientific paper

Using solar proton events (SPE) identified in ice cores, and from satellite and other data, it is shown that the frequency of occurrence of large SPEs has varied by a factor >10 in the interval 1561-1994. There is a well defined "Gleissberg" ( 80-85 year) periodicity in the data, with six well defined minima, two in close association with the Maunder and Dalton minima in sunspot numbers. The present "satellite" era is a recurrence of this series of minima. It is shown that the rate of occurrence of SPE during Schwabe cycle 1698-1711, at the end of the Maunder Minimum, was one of the highest in the period 1561-1994. This and auroral data indicate that the sun recommenced the acceleration of cosmic rays 15 years prior to the onset of significant geomagnetic activity. It is proposed that major changes in the solar corona at the end of the Maunder Minimum, and during the Gleissberg cycle, modulated the efficiency of the cosmic ray acceleration processes near the sun.

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

Possible gleissberg periodicity in large fluence solar proton events 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 Possible gleissberg periodicity in large fluence solar proton events, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Possible gleissberg periodicity in large fluence solar proton events will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-798524

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