Fig. 5: Spatial differences in temperature and precipitation driven by orbital forcing under varying atmospheric pCO2 levels at 300 Ma. | Nature Communications

Fig. 5: Spatial differences in temperature and precipitation driven by orbital forcing under varying atmospheric pCO2 levels at 300 Ma.

From: Tectonic–astronomical interactions in shaping late Paleozoic climate and organic carbon burial

Fig. 5

Maps illustrate the climatic response to different orbital configurations (Emax & Omax versus Emin & Omin) at 300 Ma, evaluated under atmospheric CO2 concentrations of 400 ppm and 800 ppm. a, b Annual mean surface temperature differences (°C) between Emax & Omax and Emin & Omin configurations. c, d Monthly mean precipitation differences (mm/month) under the same configurations.

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