THE ROLE OF THE OCEANS AND THE SUN IN LATE PLEISTOCENE AND HISTORIC GLACIAL AND CLIMATIC FLUCTUATIONS
Isotope data from Greenland ice cores and historic atmospheric and oceanic temperature records show a consistent pattern of fluctuating 25-30–year warm and cool periods over the past 500 years. During the past century, five of these climate fluctuations can be tied to glacial oscillations, oceanic temperature changes, atmospheric temperature changes, and solar variation.
The question is—what drives these oscillations? The older fluctuations can be linked to changes in 14C and 10Be isotope production rates in the upper atmosphere, suggesting variation in cosmogenic radiation. Historic climatic and oceanic temperature fluctuations are associated with solar variations. The excellent correlation of glacial, climatic, oceanic, and solar variation strongly suggests cause and effect relationships. Past patterns of these variations allow projection into the future.