PMIP (Paleoclimate Model Intercomparison Project) is designed to compa
re and improve the ability of General Circulation Models (GCMs) to sim
ulate a wide range of climatic conditions including known features of
past climatic states that are significantly different from present con
ditions. One of the first simulations of past climate conducted under
this project targets the 6000 yr BP period for the following reasons:
1) deglaciation was complete and the last remnants of the Laurentide I
ce Sheet had essentially disappeared by this time, 2) sea surface temp
eratures approached modern values, 3) the orbital insolation regime wa
s the only major boundary condition significantly different from prese
nt, and 4) a number of study sites can already be used to provide prel
iminary paleoenvironmental reconstructions for this period. Contributi
ons from the Canadian scientific community towards this experiment are
presented, following a brief overview of Canadian modern environmenta
l conditions which places the regional contributions into a broader pe
rspective.