Simulation of air and ground temperatures in PMIP3/CMIP5 last millennium simulations: implications for climate reconstructions from borehole temperature profiles

For climatemodels to simulate the continental energy storage of the Earth’s energy budget theymust capture the processes that partition energy across the land-atmosphere boundary.We evaluate herein the thermal consequences of these processes as simulated bymodels in the third phase of the paleoclimatemodelling intercomparison project and the fifth phase of the coupledmodel intercomparison project (PMIP3/CMIP5).We examine air and ground temperature tracking at decadal and centennial time-scales within PMIP3 last-millennium simulations concatenated to historical simulations from theCMIP5 archive.We find a strong coupling between air and ground temperatures during the summer from850 to 2005CE.During thewinter, the insulating effect of snow and latent heat exchanges produce a decoupling between the two temperatures in the northern high latitudes. Additionally, we use the simulated ground surface temperatures as an upper boundary condition to drive a one-dimensional conductivemodel in order to derive synthetic temperaturedepth profiles for each PMIP3/CMIP5 simulation. Inversion of these subsurface profiles yields temperature trends that retain the low-frequency variations in surface air temperatures over the last millennium for all the PMIP3/CMIP5 simulations regardless of the presence of seasonal decoupling in the simulations. These results demonstrate the robustness of surface temperature reconstructions from terrestrial borehole data and their interpretation as indicators of past surface air temperature trends and continental energy storage.