Towards Direct Simulation of Future Tropical Cyclone Statistics in a High-Resolution Global Atmospheric Model
Figure 13
The change in maximum potential intensity (MPI) of surface (10 meter) winds (knots/°C) calculated by Emanuel’s Carnot heat engine theory in the fvCAM2.2 () climate change experiment (SRES A1B). The results are averaged from July 1 to November 30 (JASON) to be comparable to Vecchi and Soden [41].
