Our results show spray’s impact on our intensifying model TCs as progressing in three stages. These are: 1) When maximum azimuthal-mean 10-m windspeed is below 30–40 m s-1, spray evaporation cools boundary layer (BL) inflow, suppressing eyewall deep convection and causing spray to weaken intensification. 2) Intensification beyond this threshold produces surface warming due to spray under the eyewall, which should promote intensification. However, spray-induced changes to the BL and secondary circulation reduce the efficiency of moist static energy transport into eyewall deep convection, and spray continues to oppose intensification overall. Further intensification may strengthen spray surface warming under the eyewall enough to overwhelm the influence of the structural inefficiency, and a transition occurs towards spray promoting intensification. 3) In the presence of strong warming due to spray under the eyewall, the eyewall contracts and spray promotes intensification. The magnitude of spray’s impact on minimum sea level pressure is at all times within approximately +/- 5 mb.

