Extended Data Fig. 5: Circulation and energetics governing the evolution of land-monsoon intensity.
From: Emergence of the modern global monsoon from the Pangaea megamonsoon set by palaeogeography
Same as Fig. 4a–c, except for boreal and austral summer-mean relative moist static energy (MSE). Left panels: boreal summer, and right panels: austral summer. From top to bottom, the panels correspond to 240 Ma, 80 Ma, and pre-industrial.
