A model study of the role of high-latitude topography in the climatic response to orbital insolation anomalies.

Abstract

The response of a combined global zonal-averaged energy balance model and a continental ice-sheet model to insolation anomalies produced by orbital perturbations is examined. Although the role of ice sheet dynamics is included in the model, this paper focuses mostly on the response of the atmosphere-hydrosphere to the perturbations.-from Authors