To estimate the amount of water that flows in a river during a year, a section of the river is made to have a rectangular cross section as shown below. In the beginning of every month (starting at January 1st) the height h of the water and the speed v of the water flow are measured. The first day of measurement is taken as 1, and the last day which is January 1st of the next year is day 366. The following data was measured: Day h (m) ly/m/s) 1 32 2.0 2.1 20 22 60 2.3 25 91 121 152 2.4 3.0 2.9 27 150 h 7 182 213 244 274 305 2.7 2.6 2.5 2.3 2.2 И 1 3 8 3 7 28 25 335 2.1 23 366 2.0 20 UNC

To estimate the amount of water that flows in a river during a year, a section of the river is made to have a rectangular cross section as shown below. In the beginning of every month (starting at January 1st) the height h of the water and the speed v of the water flow are measured. The first day of measurement is taken as 1, and the last day which is January 1st of the next year is day 366. The following data was measured: Day h (m) ly/m/s) 1 32 2.0 2.1 20 22 60 2.3 25 91 121 152 2.4 3.0 2.9 27 150 h 7 182 213 244 274 305 2.7 2.6 2.5 2.3 2.2 И 1 3 8 3 7 28 25 335 2.1 23 366 2.0 20 UNC

Computer Networking: A Top-Down Approach (7th Edition)

7th Edition

ISBN:9780133594140

Author:James Kurose, Keith Ross

Publisher:James Kurose, Keith Ross

Chapter1: Computer Networks And The Internet

Section: Chapter Questions

Problem R1RQ: What is the difference between a host and an end system? List several different types of end...

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Question

please. use matlab.

To estimate the amount of water that flows in a river during a year, a section of the river is made to
have a rectangular cross section as shown below. In the beginning of every month (starting at January
1st) the height h of the water and the speed v of the water flow are measured. The first day of
measurement is taken as 1, and the last day which is January 1st of the next year is day 366. The
following data was measured:
Day
h (m)
v (m/s)
1
32
2.0 2.1
2.0 2.2
91 121 152 182
2.4 3.0 2.9 2.7
4.7 4.1 3.8 3.7 2.8 2.5
213 244 274 305
2.6 2.5 2.3 2.2
60
2.3
2.5 2.7 5.0
Use the data to calculate the flow rate, and then integrate the flow rate to obtain an estimate of the
total amount of water that flows in the river during the year. Apply applications of a single trapezoid
between each data point.
V
water
335 366
2.1 2.0
2.3 2.0
w = 8 m

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