We evaluate the equilibrium response of the atmospheric climate to a w
ide range of systematic variations in carbon dioxide (100 to 1000 ppm)
and solar luminosity (+/-5% of today's value) using the NCAR CCM1. Th
e quantitative responses of each set of simulations are compared using
a formal sensitivity analysis. Although the forcings on the climate a
re different, both temporally and spatially, similarities appear in th
e climatic response. The results of this analysis have broader implica
tions for the use of simulations of past climates as a guide for possi
ble future climatic change.