The 15 m.y. geomagnetic reversal periodicity - A quantitative test

Computer Science

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

7

Dynamo Theory, Geodynamics, Paleomagnetism, Periodic Variations, Polarity, Cenozoic Era, Cretaceous Period, Fourier Analysis, Geomagnetism

Scientific paper

The three most commonly used geomagnetic polarity time scales that cover the past 100 m.y. are analyzed. In the three cases, different spectral analyses show a 13-16-m.y. periodicity in the rate of reversal occurrence. To test whether this periodicity is real or simply arises from a random generator, these polarity time scales are compared with a large number of synthetic sequences produced by a random process, characterized by a linear time variation of its mean activity. Geomagnetic and generated sequences were regularly sampled by using sliding windows, and then the Fourier spectra of the obtained frequency signals were compared. This test shows that the detected periodicity is presumably not a simple statistical fluctuation of an aperiodic generator, and consequently that a long-term periodicity in the geodynamo must be seriously considered.

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 15 m.y. geomagnetic reversal periodicity - A quantitative test 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 15 m.y. geomagnetic reversal periodicity - A quantitative test, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and The 15 m.y. geomagnetic reversal periodicity - A quantitative test will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1537906

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