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At-a-station (a particular cross section) variations in width, depth, and velocity with variation in discharge in ephemeral streams resemble the corresponding variations in perennial streams.
Herein, we describe the depth and velocity structure that was obtained via the PSDM analysis.
Sediments are deposited due to change in depth and velocity in the foothill region.
Unique combinations of depth and velocity at each WWP structure reflect variation in passage success.
The second, is that spatial distributions of water depth and velocity can be obtained.
Table 1 shows reach-wise decadal average of the flow of point abstraction, point inflow, length, width, depth, and velocity.
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Deposition of suspended carbonate matter is calculated as a function of flow velocity, water depth and settling velocity of suspended carbonate matter.
Bubble clouds are described in terms of depth, area and velocity for both vortex shedding and breaking wave bubble clouds.
We found that the modelled predictions of depth, discharge and velocity matched observational data collected as part of an intensive CSIRO monitoring program.
Moreover, the depths and velocities of each computational node in the flow domain are considered as the model outputs.
We vary the inflow volume, inflow location, discharge rate, water-loss rate (water-rich models only), and simulation time and examine the resulting maximum flow depths and velocities.
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