the ~ 2400-year cycle in atmospheric radiocarbon concentration: bispectrum of 14c data over the last 8000 years
Clicks: 133
ID: 252119
2002
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This
article has not been analysed, so there is no overall score —
reader engagement is measured and shown alongside.
Reader Engagement
Popular Article
30.0
/100
133 views
25 readers
AI Quality Assessment
Not analyzed
Readership in this journal
PopularRanked #203 of 484 articles by views in journal of food measurement and characterization
Most read
Least read
Bar heights use a square-root scale. Only the 120 most-read articles are drawn; the journal has 484 in total.
Mint this article as an NFT
Not yet mintedCreate a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.
5
SUSD
one-off · no wallet required
Abstract
We have carried out power
spectrum, time-spectrum and bispectrum analyses of the long-term series of the
radiocarbon concentrations deduced from measurements of the radiocarbon content
in tree rings for the last 8000 years. Classical harmonic analysis of this time
series shows a number of periods: 2400, 940, 710, 570, 500, 420, 360, 230, 210
and 190 years. A principle feature of the time series is the long period of ~
2400 years, which is well known. The lines with periods of 710, 420 and 210
years are found to be the primary secular components of power spectrum. The
complicated structure of the observed power spectrum is the result of ~
2400-year modulation of primary secular components. The modulation induces the
appearance of two side lines for every primary one, namely lines with periods
of 940 and 570 years, of 500 and 360 years, and 230 and 190 years. The
bispectral analysis shows that the parameters of carbon exchange system varied
with the ~ 2400-year period during the last 8000 years. Variations of these
parameters appear to be a climate effect on the rate of transfer of 14C
between the atmosphere and the the ocean.
Key words. Meteorology and atmospheric dynamics (climatology; ocean-atmosphere interaction; paleoclimatology)
Key words. Meteorology and atmospheric dynamics (climatology; ocean-atmosphere interaction; paleoclimatology)
| Reference Key |
vasiliev2002annalesthe
Use this key to autocite in the manuscript while using
SciMatic Manuscript Manager or Thesis Manager
|
|---|---|
| Authors | ;S. S. Vasiliev;S. S. Vasiliev;S. S. Vasiliev;V. A. Dergachev |
| Journal | journal of food measurement and characterization |
| Year | 2002 |
| DOI |
10.5194/angeo-20-115-2002
|
| URL | |
| Keywords |
Citations
No citations found. To add a citation, contact the admin at info@scimatic.org
Comments
No comments yet. Be the first to comment on this article.