Long-term trends of foF2 independent of geomagnetic activity

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

9

Scientific paper

A detailed analysis of the foF2 data at a series of ionospheric stations is performed to reveal long-term trends independent of the long-term changes in geomagnetic activity during the recent decades (nongeomagnetic trends). The method developed by the author and published earlier is used. It is found that the results for 21 out of 23 stations considered agree well and give a relative nongeomagnetic trend of -0.0012 per year (or an absolute nongeomagnetic trend of about -0.012 MHz per year) for the period between 1958 and the mid-nineties. The trends derived show no dependence on geomagnetic latitude or local time, a fact confirming their independence of geomagnetic activity. The consideration of the earlier period (1948-1985) for a few stations for which the corresponding data are available provides significantly lower foF2 trends, the difference between the later and earlier periods being a factor of 1.6. This is a strong argument in favor of an anthropogenic nature of the trends derived.

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

Long-term trends of foF2 independent of geomagnetic activity 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 Long-term trends of foF2 independent of geomagnetic activity, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Long-term trends of foF2 independent of geomagnetic activity will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1370919

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