Simulations of Permian climate and comparisons with climate-sensitive sediments

We use a climate model to simulate two intervals of Permian climate: the Sa kmarian (ca. 280 Ma), at the end of the major Permo-Carboniferous glaciatio n, and the Wordian (ca. 265 Ma). We explore the climate sensitivity to vari ous levels of atmospheric CO2 concentration and to changes in geography and topography between the two periods. The model simulates large seasonality and high aridity in the continental interiors of both hemispheres for both periods. The northern summer monsoon weakens and the southern monsoon stren gthens between the Sakmarian and the Wordian, owing to changes in geography and topography. The northern middle and high latitudes cool in winter, bet ween the Sakmarian and Wordian, associated with northward shift of the cont inents. This high-latitude cooling strengthens the winter westerlies and sh ifts the maximum storm-track precipitation south. In the Southern Hemispher e, the winter westerlies weaken from the Sakmarian to the Wordian. Starting the simulations with no permanent ice fields (i.e., by assuming that the l ate Sakmarian postdates deglaciation) and imposing increased levels of atmo spheric CO2 four times the present level, we find no tendency for reinitiat ion of major glaciation. Some permanent snow fields do develop in high sout hern latitudes, but these are primarily at high elevation. However, the com bination of low CO2 levels (such as present-day levels) and a cold summer o rbital configuration produces expanded areas of permanent snow. The results are based on statistics derived from the final 5 yr of 20-yr simulations. Paleoenvironmental indicators such as coal, evaporite, phosphate, and eolia n sand deposits agree qualitatively with the simulated climate. The extreme cold simulated in high latitudes is inconsistent with estimates of high-la titude conditions. Either the interpretation of observations is incorrect, the model is incorrect, or both; a possible model deficiency that leads to cold conditions in high latitudes is the relatively weak ocean-heat transpo rt simulated by the heat diffusion parameterization of the upper ocean mode l.