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WFM 5201: Data Management and Statistical Analysis Lecture-11: Frequency Analysis Akm Saiful Islam Institute of Water and Flood Management (IWFM) – PowerPoint PPT presentation

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Title: WFM 5201: Data Management and Statistical Analysis


1
WFM 5201 Data Management and Statistical Analysis
Lecture-11 Frequency Analysis
  • Akm Saiful Islam

Institute of Water and Flood Management
(IWFM) Bangladesh University of Engineering and
Technology (BUET)
June, 2008
2
Frequency Analysis
  • Probability Position Formula and Probability Plot
  • Analytical Frequency Analysis
  • Normal and Log-normal distribution
  • Gumbels Extreme Value distributions Type I
  • Log Pearsons Type III distribution

3
Introduction to Frequency Analysis
  • The magnitude of an extreme event is inversely
    related to its frequency of occurrence, very
    severe events occurring less frequently than more
    moderate events.
  • The objective of frequency analysis is to relate
    the magnitude of extreme events to their
    frequency of occurrence through the use of
    probability distributions.
  • Frequency analysis is defined as the
    investigation of population sample data to
    estimate recurrence or probabilities of
    magnitudes.
  • It is one of the earliest and most frequent uses
    of statistics in hydrology and natural sciences.
  • Early applications of frequency analysis were
    largely in the area of flood flow estimation.
  • Today nearly every phase of hydrology and natural
    sciences is subjected to frequency analyses.

4
Methods
  • Two methods of frequency analysis are described
    one is a straightforward plotting technique to
    obtain the cumulative distribution and the other
    uses the frequency factors.
  • The cumulative distribution function provides a
    rapid means of determining the probability of an
    event equal to or less than some specified
    quantity. The inverse is used to obtain the
    recurrence intervals.
  • The analytical frequency analysis is a simplified
    technique based on frequency factors depending on
    the distributional assumption that is made and of
    the mean, variance and for some distributions the
    coefficient of skew of the data.

5
Plotting Position Formula
  • The frequency of an even can be obtained by use
    of plotting position formulas. Where,
  • P the probability of occurrence
  • n the number of values
  • m the rank of descending values with largest
    equal to 1
  • T 1-P the mean number of exceedances
  • ac parameters depending on n

6
Plotting Position relationship
7
Parameters
n 10 20 30 40 50
a 0.448 0.443 0.442 0.441 0.440
n 60 70 80 90 100
a 0.440 0.440 0.440 0.439 0.439
a is generally recommended as 0.4 . For normal
distribution a 3/8 For Gumbels (EV1)
distribution a 0.4
8
Exercise-1
  • Using the 23 years of annual precipitation depths
    for a station given in the table below,
    estimation the exceedance frequency and
    recurrence intervals of the highest ten values
    using Weibull equation

9
Here, n 23
Year Rain depth (in) Rank, m P (m/(n1)) Tr (year)
1981 24 1 0.042 24
1986 23 3
1988 23 3 0.125 8
1978 21 4 0.167 6
1993 20 5 0.208 4.8
1999 19 8
1998 19 8
1980 19 8 0.333 3
1990 18 10
1983 18 10 0.417 2.4
10
Probability plot
  • A probability plot is a plot of a magnitude
    versus a probability.
  • Determining the probability to assign a data
    point is commonly referred to as determining the
    plotting position.

11
  • Plotting position may be expressed as a
    probability from 0 to 1 or a percent from 0 to
    100. Which method is being used should be clear
    from the context. In some discussions of
    probability plotting, especially in hydrologic
    literature, the probability scale is used to
    denote prob or . One
    can always transform the probability scale
    to or even
  • if desired.

12
Gumbels (1958) Criteria
  • The plotting position must be such that all
    observations can be plotted.
  • The plotting position should lie between the
    observed frequencies m-1/n of m/n and n where is
    the rank of the observation beginning with m1
    for the largest (smallest) value and n is the
    number of years of record (if applicable) or the
    number of observations.
  • The return period of a value equal to or larger
    than the largest observation and the return
    period of a value equal to or smaller than the
    smallest observation should converge toward n .
  • The observations should be equally spaced on the
    frequency scale.
  • The plotting position should have an initiative
    meaning, be analytically simple, and be easy to
    use.

13
Steps for probability plot
  • Rank the data from the largest (smallest) to the
    smallest (largest) value. If two or more
    observations have the same value, several
    procedures can be used for assigning a plotting
    position.
  • Calculate the plotting position of each data
    point from relationship Table presented in
    earlier slide.
  • Select the type of probability paper to be used.
  • Plot the observations on the probability paper.
  • A theoretical normal line is drawn. For normal
    distribution, the line should pass through the
    mean plus one standard deviation at 84.1 and the
    mean minus one standard deviation at 15.9.

14
Analytical Frequency Analysis
  • Chow has proposed
  • where, K is the frequency factor
  • s is the standard deviation and x bar is the
    mean value.

15
Methods of Analytical Frequency Analysis
  • Normal distribution
  • Log-normal distribution
  • Gumbels Extreme Value distributions Type I
  • Log Pearsons Type III distribution

16
Normal Distribution
  • The probability that X is less than or equal to x
    when X can be evaluated from
  • The parameters (mean) and
    (variance) are denoted as location and scale
    parameters, respectively. The normal distribution
    is a bell-shaped, continuous and symmetrical
    distribution (the coefficient of skew is zero).

(4.9)
17
Standard normal distribution
  • The probability that X is less than or equal to x
    when X is can be evaluated from
  • (4.9)

18
  • The equation (4.9) cannot be evaluated
    analytically so that approximate methods of
    integration arc required. If a tabulation of the
    integral was made, a separate table would be
    required for each value of and . By using
    the liner transformation , the random
    variable Z will be N(0,1). The random variable Z
    is said to be standardized (has and )
    and N(0,1) is said to be the standard normal
    distribution. The standard normal distribution is
    given by
  • (4.10)
  • and the cumulative standard normal is given
    by
  • (4.11)

19
Figure 4.2.1.3 Standard normal distribution
20
  • Figure 4.2.1.3 shows the standard normal
    distribution which along with the transformation
  • contains all of the
    information shown in Figures 4.1 and 4.2.
  • Both and are widely
    tabulated.
  • Most tables utilize the symmetry of the normal
    distribution so that only positive values of Z
    are shown.
  • Tables of may show or
  • prob
  • Care must be exercised when using normal
    probability tables to see what values are
    tabulated.

21
  • Exercise-2 Assume the following data follows a
    normal distribution. Find the rain depth that
    would have a recurrence interval of 100 years.
  • Year Annual Rainfall (in)
  • 2000 43
  • 1999 44
  • 1998 38
  • 1997 31
  • 1996 47
  • .. ..

22
  • Solution
  • Mean 41.5, St. Dev 6.7 in (given)
  • x Mean Std.Dev z
  • x 41.5 z(6.7)
  • P(z) 1/T 1/100 0.01
  • F(z) 1.0 P(z) 0.99
  • From Interpolation using Tables E.4
  • Z 2.33
  • X 41.5 (2.33 x 6.7) 57.11 in

23
Table Area under standardized normal
distribution
24
Linear Interpolation from Z-table
  • For, p0.99 , find z ?
  • From table, z1 2.32 , p1 0.9898 and z2 2.33
    p20.9901
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