Question: Question: Depth - averaged velocity observations from a Red River cross - section are given below. Here, x is the distance from the left bank
Question: Depthaveraged velocity observations from a Red River crosssection are given
below. Here, x is the distance from the left bank m U is the depthaveraged velocity ms
and H is the flow depth m
x
U
H ;
Step : Plot the shape of the measured crosssection.
Step : Interpolate spline the measured data for a
smoother crosssection using increment.
Step : Include the interpolated crosssection in the
plot.
Step : Follow the same steps for the lateral velocity
distribution. Please note that you need to label your
figures as follows if you need to publish multiple figures
from the same script:
figure
plot
figure
plot
Step : Perform a basic fit analysis to find the best equation of the interpolated velocity curve.
Use only linear, cubic, and quadratic options. After you make the choice based on R
please
plot that equation versus the interpolated velocity curve as the third plot.
Step : Calculate the average velocity V for the crosssection. Please use interpolated U to
calculate the mean value.
Step : Write an interactive section for the parameters V in your script to calculate the
GaucklerManning coefficient n using the following equation.
Here:
V : crosssectional averaged velocity ms
n : GaucklerManning coefficient
Rh : hydraulic radius Rh m
S : channel bed slope S
Step : First, use the calculated V as the input and compute n Then double the V and re
compute n Finally, make a short comment based on the difference. The most important
outcome of this test is to understand how n changes based on V
Show Matlab script of solution.
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