G. Wagner et al., Some results relevant to the discussion of a possible link between cosmic rays and the Earth's climate, J GEO RES-A, 106(D4), 2001, pp. 3381-3387
Based on a 16-year observation period (1980-1995), it was claimed recently
that Earth's climate was linked to variations in the flux of cosmic rays pe
netrating into the atmosphere via their postulated effect on global cloud c
over. Data from three independent studies yield information relevant to the
ongoing discussion of the likelihood of the existence of such a link. (1)
Model calculations show that the relative change in the ion production rate
from a solar maximum to a solar minimum is of the same order as, or even g
reater than,the corresponding change in global cloud cover. (2) However, th
e smoothed combined flux of Be-10 and Cl-36 at Summit, Greenland, from 20-6
0 kyr B.P. (proportional to the geomagnetically modulated cosmic ray flux)
is unrelated to the corresponding delta O-18 and CH4 data (interpreted as s
upraregional climate proxies). (3) Furthermore, although a comparison of th
e incoming neutron flux with cloud cover in Switzerland over the last 5 dec
ades shows a significant correlation at times during the 1980s and 1990s, t
his does not occur during the rest of the period.