Graphic Approach

Once the data series is identified and ranked and the plotting position is calcu­lated, a graph of magnitude x versus probability [P(X > x), P(X < x), or T] can be plotted and a distribution fitted graphically. To facilitate this procedure, it is common to use some specially designed probability graph paper rather than linear graph paper. The probability scale in those special papers is chosen such that the resulting probability plot is a straight line. By plotting the data using a particular probability scale and constructing a best-fit straight line through the data, a graphic fit is made to the distribution used in constructing the prob­ability scale. This is a graphic approach to estimate the statistical parameters of the distribution.

Example 3.1 illustrates the graphic approach to the analysis of flood data. The general procedure is as follows: [2] [3] 3 [4]

5. Extend the line to the highest return-period value needed, and read all re­quired return-period values off the line.

Example 3.1 The Boneyard Creek stream gauging station was located near the fire station on the campus of the University of Illinois at Urbana-Champaign. From the USGS Water Supply Papers, the partial duration data of peak discharges above 400 ft3/s between the water years 1961 and 1975 were obtained and listed below. In addi­tion, for the years when there was no flow in a year exceeding 400 ft3/s, the peak flow for that year is given in parenthesis (e. g., 1961).

Year

Discharge, ft3/s

Year

Discharge, ft3 /s

1961

(390)

1969

549, 454

1962

(374)

1970

414, 410

1963

(342)

1971

434, 524

1964

507

1972

505, 415, 406

1965

579, 406, 596

1973

428, 447, 407

1966

416

1974

468, 543, 441

1967

533

1975

591, 497

1968

505

(a) List the ranked annual maximum series. Also compute and list the corresponding plotting positions (return period) and exceedance probability P (X > x).

(b) Plot the annual maximum series on (i) Gumbel paper and (ii) lognormal paper.

(c) Construct a best-fit line through the nonlinear plots, and estimate the flows for return periods of 2, 10, 25, and 50 years.

Solution n = 15 (a)

Annual Maximum Discharge (ft3/s)

Rank

(m)

‘T _ n+1 Tm = m

(years)

P(X > X(m))

= 1/Tm

P (X < x(m))

= 1 — 1/Tm

596

1

16.00

0.0625

0.9375

591

2

8.00

0.1250

0.8750

549

3

5.33

0.1875

0.8125

543

4

4.00

0.2500

0.7500

533

5

3.20

0.3125

0.6875

524

6

2.67

0.3750

0.6250

507

7

2.29

0.4375

0.5625

505

8

2.00

0.5000

0.5000

505

9

1.78

0.5625

0.4375

447

10

1.60

0.6250

0.3750

416

11

1.46

0.6875

0.3125

414

12

1.33

0.7500

0.2500

390

13

1.23

0.8125

0.1875

374

14

1.14

0.8750

0.1250

342

15

1.06

0.9375

0.0625

(b) Plots of the annual maximum flow series on the Gumbel and lognormal probability papers are shown in Fig. 3.2.

Graphic Approach

Graphic Approach

Figure 3.2 Probability plot for the annual maximum series for 1961-1975 on the Boneyard Creek at Urbana, IL: (a) Gumbel probability plot; (b) lognormal probability plot.

 

(c) The following table summarizes the results read from the plots:

 

Return Period (years)

Distribution

2

10

25

50

Gumbel

470

610

680

730

Lognormal

475

590

650

700

 

Graphic Approach

Updated: 16 ноября, 2015 — 12:32 дп