Paleoclimatology: The Science
This course focuses on the science behind our understanding of how our planet's climate has changed over time, in particular from 100 million years ago to the present. The most significant processes, astronomical, geological, oceanographic, and atmospheric, are examined with an emphasis on the broad scales of time and space over which they operate, and drive climatic change. Proxy data records are defined in the context of how they record climatic data, and how we "read" them to learn the climatic history they store.