Atmosphere Ocean Science Colloquium
Key Uncertainties in Climate Forcing and Feedbacks
Speaker: Andrew Gettelman, NCAR
Location: Warren Weaver Hall 1302
Date: Wednesday, March 2, 2016, 3:30 p.m.
Radiative Forcing of climate occurs when the energy budget of the earth system is altered. The resulting change to temperature and circulation induces climate feedbacks, which govern the response of the system to changes, and can buffer the climate system response (in the case of negative feedbacks), or can enhance it (positive feedbacks). This presentation will review the framework for understanding climate forcing and climate feedbacks, particularly with respect to responses to anthropogenic forcing. The largest uncertainty in climate forcing is the induced change in cloudiness due to aerosols. The largest feedback uncertainty is the cloud feedback. The fact that the forcing is dependent on clouds, which are also the largest feedback, makes dis-entangling forcing and feedbacks complex. Several ensembles of a single comprehensive Earth System Model are analyzed to explore the interaction of feedbacks and forcing, which may provide further constraints on forcing and feedback, and hence future evolution of climate.