Fig. 6: Data–model agreement scores for lower Cambrian lithology data and FOAM GCM simulations, incorporating palaeogeographic uncertainty of 200 km. | Nature Communications

Fig. 6: Data–model agreement scores for lower Cambrian lithology data and FOAM GCM simulations, incorporating palaeogeographic uncertainty of 200 km.

From: Quantitative comparison of geological data and model simulations constrains early Cambrian geography and climate

Fig. 6

The scores compare Köppen–Geiger climate classes assigned to climatically sensitive rock types with the climate classes produced under each GCM simulation, following the agreement scoring equation of ref. 49 (see ‘Methods’). Simulations were run with present-day orbital parameters.

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