Using what has become a celebrated catchphrase, Philip W. Anderson once wrote that
“more is different”(Science, Vol. 177, Issue 4047, pp. 393–396, 1972). First formulated in the …

This paper outlines the various approaches used to calculate bedload transport. As bedload
transport exhibits considerable spatial and temporal variations, computing the bedload …

Morphological evolution of river deltas depends to a large extent on river discharges, which
are usually highly unsteady due to natural hydrological cycles and anthropogenic …

The prediction of bedload transport capacity in riverbed with aquatic vegetation is a pressing
need for river restoration. Laboratory experiments were conducted to investigate the weak …

There is a paradox in the relationship between bedload transport rates and flow variables:
laboratory and field studies have reported on how bedload transport rates depend on flow …

Measuring bedload transport rates usually involves measuring the flux of sediment or
collecting sediment during a certain interval of time Δ t. Because bedload transport rates …

In this article we apply the CASCADE network‐scale sediment connectivity model to the
Vjosa River in Albania. The Vjosa is one of the last unimpaired braided rivers in Europe and …

During the last 20 years, flume and field experiments have shown that grain sorting
contributes to bed‐level fluctuations and bedload pulses. In this work, we propose a new …

The Swiss plate geophone is a bedload surrogate monitoring system that has been
calibrated in several gravel‐bed streams using direct sampling techniques. Past systematic …

Mountainous gravel-bed stream characterized by large-scale roughness generally goes
through the seasonal flow, including flood and interevent periods. Recent studies suggest …