Weak upstream overdensities or underdensities lead to the corrugation of R-
type ionization fronts. The propagation velocity of the R-type front varies
as a result of the different line-of-sight emission measures, and is also
decreased because of the obliqueness of the front. The transition to D type
occurs earlier in some parts of the front, and the resulting non-linear in
stability of the front leads to the formation of dense clumps and tails wit
hin the H II region.
In this paper, we discuss criteria for the development of this instability.
In developing numerical models of this process, we have encountered numeri
cal artefacts that have to be treated with care in high-resolution hydrodyn
amical simulations of H II regions. We discuss the application of our resul
ts to the structure and development of H II regions.