Water relations were studied in Norway spruce [Picea abies (L.) Karst.] trees grown at ambient (AC, 350 μmol mol -1 ) and elevated (EC, 700 μmol mol -1 ) CO 2 concentrations under temperate water stress. The results suggested that both crown position and variability in atmospheric CO 2 concentration are responsible for different patterns of crown water relations. Mean hourly sap flux density (F SA ) showed higher values in upper crown position in comparison with the whole crown in both AC and EC treatments. Mean soil-to-leaf hydraulic conductance (G Tsa ) was 1.4 times higher for the upper crown than that calculated across the whole crown for the trees in AC. However, G Tsa did not vary significantly with crown position in EC trees, suggesting that elevated CO 2 may mitigate differences in hydraulic supply for different canopy layers. The trees in EC treatment exhibited significantly higher values of F SA measured on the whole crown level and slightly higher soil water content compared to AC treatment, suggesting more economical use of soil water and therefore an advantage under water-limited conditions.