The sorption of moisture by spruce and meranti coated with both waterborne and solventborne coatings was studied during controlled conditions. Experimental variables included: coating ®lm thickness, temperature and gradients in relative humidity (33±98, 65±98 or 33±75%), or exposure to liquid water. Changes in moisture content of the wood and the tangential or the radial dimensions were recorded as a function of time. Apparent moisture diffusion coef®cients were calculated from the initial slope of the fractional weight increase following Fick's second law for unsteady state conditions. The apparent moisture diffusion coef®cients were clearly in¯uenced by both coating and wood species. The fastest moisture adsorption was observed for uncoated spruce which could be explained by the rapid capillary uptake of water. Moisture diffusion in coated samples of spruce or with coated or uncoated meranti was much lower. With the exception of liquid water, moisture diffusion during desorption was faster than during adsorption. The measured moisture diffusion coef®cients should be considered as apparent because they were dependent on the initial and ®nal moisture content. Moisture diffusion was found to be strongly dependent on temperature with activation energies between 55±76 kJ mol )1 . The rate of dimensional change was described by a two-parameter asymptotic regression model that included one constant for the rate of dimensional change and an asymptotic constant given by the dimensions at equilibrium wood moisture content as an asymptote. The differences in rate constant were inuenced by the same factors as those for moisture diffusion. The correlation between rate constant and moisture diffusion coef®cient was good except for very high moisture diffusion coef®cients that were controlled by capillary water uptake.