Cavitation has been suggested to be a possible source of long range interactions between mesoscopic hydrophobic surfaces. While evaporation is predicted by thermodynamics,little is known about its kinetics. Glauber dynamics Monte Carlo simulationsof a lattice gas close to liquid-gascoexistence and confined between partially drying surfacesare used to model the effect of water confinement on the dynamics of surface-inducedphase transition. Specifically, we examine how kinetics of induced evaporation change as the texture of hydrophobic surfacesis varied. Evaporationrates are considerably slowed with relatively small amount of hydrophilic coverage. However, the distribution of hydrophilic patches is found to be crucial, with the homogeneous one being much more effectivein slowingthe formation of vapor tubes which triggersthe evaporationprocess. We estimatethe fi-eeenergy barrierof vapor tube formation via transitionstate theory,usinga constrainedforwardbackward umbrella sampling technique applied to the metastable, confined liquid. Furthermore,to relate simulationrates to experimentalones, we perform simulationsusing the mass-conservingKawasakialgorithm. We predict evaporation time scales that range horn hundredsof picosecond in the case of mesoscopic surfacesN 104 nm2 to tens of nanosecondsfor smaller surfaces N 40 nm2, when the two surfacesare w 10 solvent layersapart. The present study demonstrates that cavitation is kinetically viable in real systems and should be considered in studies of processesat confined geometry. I.