Fig. 5: Simulated meteorological parameters for the paleo-location of the Esplugafreda sedimentary record for various atmospheric CO2 concentrations.
From: Substantial continental temperature rise over the Paleocene-Eocene Thermal Maximum in the Pyrenees

a near-surface air temperature and (b) daily precipitation. Model data displayed are ensemble means of eight Earth system models of DeepMIP45. Reconstructed (soil carbonate-based) TJJA values for the LP and PETM are also shown for comparison.