The concept of channel-forming (Q cf) or dominant discharge is now a cornerstone of river
channel restoration design. Three measures of channel-forming discharge are most …

A floodplain is an area of low-lying land adjacent to a river, stream, or other water body that
is regularly inundated by water during periods of high flow. Floodplains typically have …

The overall influence of urbanization on how flows of different frequency might change over
time, while important in hydrologic design, remains imprecisely known. In this study, we …

Despite large advances in the state of the science of stream ecology and river mechanics,
the practitioner-driven field of stream restoration remains plagued by narrowly focused …

Effective discharge (Q e) for suspended sediment transport in the alluvial reaches of the
Ganga River in the western Ganga plains (WGP) has been computed using 'analytical'and …

Quantifying the spatial and temporal dynamics of stream metabolism across stream
networks is key to understanding carbon cycling and stream food web ecology. To better …

Semiarid channels exhibit an extreme sensitivity to upstream urban development,
particularly in unconfined valleys with unprotected grades. For example, one of our study …

Sediment output (solid and dissolved load) from two small Alpine rivers (Partnach and
Lahnenwiesgraben in the Bavarian Alps) was measured during three summer field seasons …

This study investigated the roles of variable daily discharges in controlling processes of
composite bank erosion in alpine meandering rivers located in the Zoige basin on the …

PURPOSE: The purpose of this Technical Note is to provide guidance and cautions to be
used in approximating channel-forming discharge with bankfull, specified recurrence …