Atmospheric circulation accounts responsible for rapid distribution of heat and moisture across the earth and hence determines our weather and regional climate, today and in the past. While the atmosphere itself does not hold an archive for paleoclimate reconstruction, it left abundant information in the ice, and in sediments in the ocean and on land. In detail, records of millenial scale variations from different regions, archives and proxies differ considerably, hence holding a wealth of detail information most of which is still to be extracted.
Preliminary List of Solicited Speakers
Co-Sponsorship
Past Global Changes (PAGES)
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