Abstract
In this paper, we shall discuss the possibility of CO2 removal indirectly through the lower/middle stratosphere via reactions with cosmic rays. We postulate this possibility based on a comparative analysis of the content of the cosmic ray-generated isotope 10Be in ice core samples from Greenland and Antarctica and of CO2 (a) in the air inclusions of an ice core from the Vostok station in Antarctica. The correlation coefficients between the 10Be and CO2 (a) concentrations calculated from the available experimental data for various times over the last climatic cycle suggest a significant negative correlation between the variation of the most important greenhouse gas, CO2 (a), and the indicator of cosmic-ray intensity, 10Be. -from Journal translation
| Original language | English |
|---|---|
| Pages (from-to) | 18-22 |
| Number of pages | 5 |
| Journal | Transactions Doklady - Russian Academy of Sciences: Earth Science Sections |
| Volume | 336 |
| Issue number | 4 |
| Publication status | Published - 1995 |
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ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Environmental Science(all)
Cite this
Cosmic ray-induced reactions as a factor in the removal of CO2 from the atmosphere. / Semiletov, I. P.; Kharlamov, Y. M.; Myagkikh, A. I.; Nikitin, A. Y.; Pipko, I. I.
In: Transactions Doklady - Russian Academy of Sciences: Earth Science Sections, Vol. 336, No. 4, 1995, p. 18-22.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Cosmic ray-induced reactions as a factor in the removal of CO2 from the atmosphere
AU - Semiletov, I. P.
AU - Kharlamov, Y. M.
AU - Myagkikh, A. I.
AU - Nikitin, A. Y.
AU - Pipko, I. I.
PY - 1995
Y1 - 1995
N2 - In this paper, we shall discuss the possibility of CO2 removal indirectly through the lower/middle stratosphere via reactions with cosmic rays. We postulate this possibility based on a comparative analysis of the content of the cosmic ray-generated isotope 10Be in ice core samples from Greenland and Antarctica and of CO2 (a) in the air inclusions of an ice core from the Vostok station in Antarctica. The correlation coefficients between the 10Be and CO2 (a) concentrations calculated from the available experimental data for various times over the last climatic cycle suggest a significant negative correlation between the variation of the most important greenhouse gas, CO2 (a), and the indicator of cosmic-ray intensity, 10Be. -from Journal translation
AB - In this paper, we shall discuss the possibility of CO2 removal indirectly through the lower/middle stratosphere via reactions with cosmic rays. We postulate this possibility based on a comparative analysis of the content of the cosmic ray-generated isotope 10Be in ice core samples from Greenland and Antarctica and of CO2 (a) in the air inclusions of an ice core from the Vostok station in Antarctica. The correlation coefficients between the 10Be and CO2 (a) concentrations calculated from the available experimental data for various times over the last climatic cycle suggest a significant negative correlation between the variation of the most important greenhouse gas, CO2 (a), and the indicator of cosmic-ray intensity, 10Be. -from Journal translation
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UR - http://www.scopus.com/inward/citedby.url?scp=0029473650&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:0029473650
VL - 336
SP - 18
EP - 22
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 4
ER -