Scalings are obtained for the development of unsteady natural convection, b
oth in rectangular and vertical circular containers, and are validated by c
omparison with results obtained using direct numerical simulation. It is fo
und that the numerical results agree well with the scalings. Three main sta
ges of flow evolution are identified and the differences at each of these s
tages between the rectangular and cylindrical geometries are quantified. It
is shown that in the flow regimes considered there is a difference in ther
mal boundary layer thickness; that the horizontal intrusion layer has a uni
form thickness for the rectangular flow, but increases towards the symmetry
axis for the cylindrical flow; and that the rate of stratification is much
faster for the cylindrical geometry. (C) 2001 Elsevier Science Inc. All ri
ghts reserved.