Published by the American Geophysical Union as part of the Water Resources Monograph
Series, Volume 19. What are the forms and processes characteristic of mountain rivers and …

Movement is considered an essential process in sha** the distributions of species.
Nevertheless, most species distribution models (SDMs) still focus solely on environment …

River channels commonly exhibit downstream variations in channel width, which can lead to
the development of alternating shallow and deep areas known as riffle‐pool sequences. The …

Riffle pools are fundamental units of many gravel bed rivers. Considerable debate exists as
to an appropriate hydrodynamic model for this bed form type. Sampling designs in previous …

The habitat complexity of a riverine ecosystem influences the bioenergetics of drift feeding
fish. We coupled hydrodynamic and bioenergetic models to assess the influence of habitat …

Field observations, experiments, and numerical simulations suggest that pool‐riffles along
gravel bed mountain streams develop due to downstream variations of channel width …

Floods are a key component of the ecology and management of riverine ecosystems around
the globe, but it is not clear whether floods have predictable effects on organisms that can …

Decades of research have demonstrated that gravel-bed rivers exhibit multiple spatial
scales of landform nonuniformity. Landform features such as valley wall oscillations, alluvial …

The relationships between flow hydrology, topography, and channel change in mountain
rivers is important to understanding landscape evolution, the structure and persistence of …

Channel topography in gravel‐bedded rivers interacts with the local flow and sediment
transport fields to produce “forced patches,” which are temporally stable areas on the bed …