The heating of a water aerosol droplet until it disintegrates (by varp
orization or explosion) is investigated in the approximation of a unif
orm optical field in the interior of the droplet for three isobaric re
gimes: thermal conduction, combined conduction and convection, and con
vection. The main characteristics of the heating process are determine
d and described for droplets with initial radii of 1-5 mum, including:
the distributions of the temperature and velocity of the liquid insid
e the droplet, the variation of the droplet radius, the heating time t
o disintegration, and the explosion threshold. The time of homogeneous
nucleation of vapor bubbles in the metastable liquid is adopted as th
e criterion of explosion. The boundaries between the investigated heat
ing regimes are more accurately determined. It is shown that the explo
sion threshold is influenced by the time profile of the irradiating pu
lse.