Physical heterogeneity is a major topic in river sciences because it is known to be a key factor for ecological integrity. In this paper, we investigated the hydraulic enviroment in an alpine gravel-bed stream with an unaltered hydrological regime. The study was based on the hypothesis that spatial and temporal variability are correlated to the morphological template of a stream. Numerical hydrodynamic modelling was conducted at five morphologically contrasting study sites for different discharges chosen from discharge duration curves. On the basis of the resulting hydraulic variables, namely flow velocity and water depth, and of a recently proposed hydromorphological index of diversity, the differences in spatial and temporal variability were analysed by descriptive statistics. Spatial diversity was higher at morphologically natural sites than at sites that were partially or fully regulated by resectioning and bank protection. Conversely, temporal variability in the hydraulic environment was higher at regulated sites where hydraulic variables were subject to fluctuations with each small discharge modification, which is not the case for more impaired sites. Unless higher discharges with bed reshaping activity occur, natural streams are characterized not only by high spatial variability but also by a sustained persistence of aquatic habitats. Therefore, river engineering projects aimed at enhancing habitat heterogeneity should not only focus on a higher spatial variability of the physical environment but also aim for greater persistence of aquatic habitats. Figure 2. Photos of study sites. Sites S1 and S5 are from the view of the upstream direction, whereas sites S2, S3 and S4 are from the view of the downstream direction. A block ramp of site S5 is visible on the uppermost third of the relative photo. 655 SPATIAL AND TEMPORAL HYDRAULIC VARIABILITY IN AN ALPINE GRAVEL-BED STREAM Figure 3. Regression between specific flow (m 3 s À1 , km 2 ) and watershed area for flood discharges calculated to complete flow duration curves. 657 SPATIAL AND TEMPORAL HYDRAULIC VARIABILITY IN AN ALPINE GRAVEL-BED STREAM