Physics
Scientific paper
Feb 2004
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004jastp..66..313c&link_type=abstract
Journal of Atmospheric and Solar-Terrestrial Physics, Volume 66, Issue 3-4, p. 313-322.
Physics
11
Cosmic Rays, Causality Problem, Magnetic Field, Speleothems, Orbital Forcing, Paleoclimate
Scientific paper
The possibility that galactic cosmic rays (GCR) influence the Earth's cloud cover and therefore have an important impact on the Earth's radiative climate forcing has become a leading candidate to explain the observed sun-climate connection. A correlation between GCR and low cloud cover has been ascertained in models and observations over the past few years. The deposition of cosmogenic radionuclides in ice cores and deep sea sediments can be used as a proxy for the past GCR-flux and provides an important tool to study the supposed GCR-climate connection on glacial-interglacial timescales. In this study, a record of geomagnetic paleointensity based on 10Be from deep sea sediments is used as proxy for GCR-flux over the past 200,000 years. It is compared with climate records from marine, terrestrial and ice core archives. Our results are consistent with the GCR-climate theory and suggest the existence of a GCR-climate connection over the past 200,000 years.
Christl Marcus
Holzkämper Steffen
Mangini Augusto
Spötl Christoph
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