Current theories of pattern formation predict the existence of 'phase grain
boundaries' across which the orientation of the wave number of convective
rolls changes abruptly. However, the usual assumption of slow variation is
violated by these solutions. By restricting attention to near the critical
Rayleigh number Ra-c for linear onset of convection, a rational weakly nonl
inear theory may be envisaged. This might have either smoothly varying solu
tions, or discontinuous 'outer solutions' matched by an inner transition re
gion. We find smooth steady solutions, with just two participating modes; b
ut we show that there exists no weakly nonlinear solution of near-discontin
uous type. To elucidate the evolution of an initially discontinuous state,
we solve an associated linear time-dependent problem. Our results show that
, sufficiently close to Ra-c, steady transitions between differing roll ori
entations must take place gradually, rather than abruptly; and that predict
ions of abrupt transitions from model equations, which are not rigorously v
alidated, may mislead. (C) 2000 The Japan Society of Fluid Mechanics and El
sevier Science B.V. All rights reserved.