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. 2016 Jul 13;113(32):8927–8932. doi: 10.1073/pnas.1601472113

Fig. 6.

Fig. 6.

Daily evolutions of (A) convective self-aggregation, (B) anvil cloud amount, (C) Dr, and (D) upper-tropospheric γ predicted by the IPSL GCM in a RCE simulation forced by an SST of 305 K. Shading denotes the timescale (ca. 30 d) for subsidence to turn over the troposphere.