What Drives Glacial Cycles? Talk and Reception with Wally Broecker
- Newberry Professor, Lamont-Doherty Earth Observatory, Columbia University
- Distinguished Visitor, Arizona State University
Similarities between the timing of orbitally driven changes in seasonality and extent of ice sheets makes clear that there must be a causal link. The long-standing view is that glaciers respond to summer insolation. However, this link cannot explain the hemispheric synchronicity of glacial response. Dr. Broecker proposes that, instead, orbital cycles drive reorganizations of the ocean's thermohaline circulation. These, in turn, generate changes in the atmosphere's CO₂ content. Hence, CO₂, rather than summer insolation, is the dominant driver of glacial cycles.
RSVP not required
pre-talk reception, 3:00 p.m.
talk begins, 3:30 p.m.