Friday, 8 June 2001: 10:30 AM
Current theories for climate variability arising from coupled ocean-
atmosphere interactions and their relevance for understanding the observed
record of climate variability will be presented.
Conceptual models of the large-scale dynamics of the coupled ocean/
atmosphere system include paradigms for ENSO,
midlatitude variability involving the
wind-driven ocean gyre circulations, oceanic linkages between the Tropics and
midlatitudes, and high latitude variability associated
with fluctuations in the thermohaline circulation.
The stochastic climate model "null hypothesis" for climate variability
resulting from ocean-atmosphere interactions will also be discussed.
In each case, the observational evidence
in support of and in contradiction to the theory will be reviewed.
- Indicates paper has been withdrawn from meeting
- Indicates an Award Winner