Abstract
We propose that the mechanisms driving hyporheic exchange vary systematically with different channel morphologies and associated fluvial processes that occur in mountain basins, providing a framework for examining physical controls on hyporheic environments and their spatial variation across the landscape. Furthermore, the spatial distribution of hyporheic environments within mountain catchments represents a nested hierarchy of process controls. Large‐scale process drivers (geology, climate, fire, and land use) impose a suite of watershed conditions (topography, streamflow, sediment supply, and vegetation) on the fluvial system. Different combinations of imposed watershed conditions result in different reach‐scale channel morphologies (e.g. step‐pool, pool‐riffle, and braided) that, in turn, structure hyporheic processes (e.g. pressure divergence, spatial variation of hydraulic conductivity) and resultant hyporheic environments (scales and rates of hyporheic exchange). Consequently, a holistic view of natural and anthropogenic drivers over a range of spatial and temporal scales is needed for understanding hyporheic ecosystems.