The dynamical evolution of H II, regions and wind-driven bubbles in de
nse clouds is studied. In particular, we address two different issues:
(1) the conditions under which ultracompact H II) regions can reach p
ressure equilibrium with their surrounding medium (and thereby stall t
heir expansion) and (2) the appearance of a powerful dynamic instabili
ty in expanding H II regions. At pressure equilibrium, the ionized reg
ions become static, and as long as the ionization sources and the ambi
ent gas densities remain about constant, the resulting UCHII regions a
re stable and long-lived. The equilibrium sizes and densities, R(S,eq)
similar to 3 x 10(-2)F(48)(1/3)T(HII,4)(2/3)P(7)(-2/3) pc and n(i,eq)
similar to 4 10(4)P(7)T(HII,4)(-1) cm(-3) (where F-48 is the photoion
izing in units of 10(-7) dyne cm(-2), and T-HII,T-4 is the ion tempera
ture in units of 10(4) K), are similar to those actually observed in U
CHII regions. Similarly, ultracompact wind-driven bubbles can reach pr
essure equilibrium, and the resulting final sizes are similar to those
of UCHII's. The same is true for a combined ultracompact structure co
nsisting of an interior wind-driven cavity and an external HII region.
For nonmoving stars in a constant-density medium, the lifetimes for a
ll types of ultracompact objects only depend on the stellar lifetimes.
For cases with a density gradient, depending on the core size and slo
pe of the density distribution, some regions never reach the static eq
uilibrium condition. A powerful dynamic instability appears when cooli
ng is included in the neutral gas swept up by an HII region or a combi
ned wind-II n region structure. This instability was first studied by
Giuliani and is associated with the thin-shell instability described b
y Vishniac. The internal ionization front exacerbates the growth of th
e thin-shell instability, creating a rapid shell fragmentation, and ou
r numerical simulations confirm the linear analysis of Giuliani. The f
ragments tend to merge as the evolution proceeds, creating dense and m
ore massive clumps, and are slowly eroded by ionization fronts. Thus t
he resulting structures have a variety of shapes, sizes, densities, an
d lifetimes. Intriguing features such as ''elephant trunks'' and comet
ary-like globules can easily be explained as a result of this instabil
ity.