WFM-6204: Hydrologic Statistics

Slides:



Advertisements
Similar presentations
Probability Distribution
Advertisements

STATISTICS Univariate Distributions
The Poisson distribution
WFM 6204: Hydrologic Statistics © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM-6204: Hydrologic Statistics Akm Saiful Islam Syllabus October, 2007 Institute.
WFM 6204: Hydrologic Statistics © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM-6204: Hydrologic Statistics Akm Saiful Islam Lecture-3: Probabilistic analysis:
Hydrologic Statistics Reading: Chapter 11, Sections 12-1 and 12-2 of Applied Hydrology 04/04/2006.
Special random variables Chapter 5 Some discrete or continuous probability distributions.
WFM-6204: Hydrologic Statistics
WFM 6204: Hydrologic Statistics © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM-6204: Hydrologic Statistics Akm Saiful Islam Lecture-2: Probability and.
Chapter 5 Discrete Random Variables and Probability Distributions
Hydrologic Statistics
Chapter 4: Probabilistic features of certain data Distributions Pages
WFM 6204: Hydrologic Statistics © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM-6204: Hydrologic Statistics Akm Saiful Islam Lecture-1: Characteristics.
FREQUENCY ANALYSIS Basic Problem: To relate the magnitude of extreme events to their frequency of occurrence through the use of probability distributions.
Chapter 4 Discrete Random Variables and Probability Distributions
WFM 5201: Data Management and Statistical Analysis © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM 5201: Data Management and Statistical Analysis Akm Saiful.
WFM 5201: Data Management and Statistical Analysis © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM 5201: Data Management and Statistical Analysis Akm Saiful.
WFM 5201: Data Management and Statistical Analysis © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM 5201: Data Management and Statistical Analysis Akm Saiful.
WFM 5201: Data Management and Statistical Analysis © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM 5201: Data Management and Statistical Analysis Akm Saiful.
WFM 5201: Data Management and Statistical Analysis © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM 5201: Data Management and Statistical Analysis Akm Saiful.
Chapter 4 Probability Distributions
WFM 5201: Data Management and Statistical Analysis
WFM 5201: Data Management and Statistical Analysis
WFM 5201: Data Management and Statistical Analysis © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM 5201: Data Management and Statistical Analysis Akm Saiful.
QBM117 Business Statistics
A random variable that has the following pmf is said to be a binomial random variable with parameters n, p The Binomial random variable.
CHAPTER 6 Statistical Analysis of Experimental Data
Statistics and Probability Theory Prof. Dr. Michael Havbro Faber
Class notes for ISE 201 San Jose State University
McGraw-Hill Ryerson Copyright © 2011 McGraw-Hill Ryerson Limited. Adapted by Peter Au, George Brown College.
Chapter 21 Random Variables Discrete: Bernoulli, Binomial, Geometric, Poisson Continuous: Uniform, Exponential, Gamma, Normal Expectation & Variance, Joint.
Flood Frequency Analysis
Hydrologic Statistics
Distributions Dr. Omar Al Jadaan Assistant Professor – Computer Science & Mathematics.
McGraw-Hill/Irwin Copyright © 2007 by The McGraw-Hill Companies, Inc. All rights reserved. Discrete Random Variables Chapter 4.
Discrete Distributions
WFM 5201: Data Management and Statistical Analysis © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM 5201: Data Management and Statistical Analysis Akm Saiful.
L Berkley Davis Copyright 2009 MER301: Engineering Reliability Lecture 5 1 MER301: Engineering Reliability LECTURE 5: Chapter 3: Probability Plotting,The.
Slide 1 Copyright © 2004 Pearson Education, Inc..
CE 3354 ENGINEERING HYDROLOGY Lecture 6: Probability Estimation Modeling.
Statistics & Flood Frequency Chapter 3 Dr. Philip B. Bedient Rice University 2006.
FREQUENCY ANALYSIS.
Continuous Distributions The Uniform distribution from a to b.
Random Variables. A random variable X is a real valued function defined on the sample space, X : S  R. The set { s  S : X ( s )  [ a, b ] is an event}.
ENGR 610 Applied Statistics Fall Week 3 Marshall University CITE Jack Smith.
Statistical Applications Binominal and Poisson’s Probability distributions E ( x ) =  =  xf ( x )
BINOMIALDISTRIBUTION AND ITS APPLICATION. Binomial Distribution  The binomial probability density function –f(x) = n C x p x q n-x for x=0,1,2,3…,n for.
Biostatistics Class 3 Discrete Probability Distributions 2/8/2000.
Copyright © 2010 by The McGraw-Hill Companies, Inc. All rights reserved. McGraw-Hill/Irwin Chapter 5 Discrete Random Variables.
Probability Definitions Dr. Dan Gilbert Associate Professor Tennessee Wesleyan College.
King Saud University Women Students
WFM 5201: Data Management and Statistical Analysis © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM 5201: Data Management and Statistical Analysis Akm Saiful.
Expectation. Let X denote a discrete random variable with probability function p(x) (probability density function f(x) if X is continuous) then the expected.
Topic 3 - Discrete distributions Basics of discrete distributions - pages Mean and variance of a discrete distribution - pages ,
Some Common Discrete Random Variables. Binomial Random Variables.
Probability and Distributions. Deterministic vs. Random Processes In deterministic processes, the outcome can be predicted exactly in advance Eg. Force.
Probability distributions
Copyright © 2011 by The McGraw-Hill Companies, Inc. All rights reserved. McGraw-Hill/Irwin Chapter 5 Discrete Random Variables.
MECH 373 Instrumentation and Measurements
Discrete Random Variables
Poisson Random Variables
Probability Distributions: a review
Statistical Hydrology and Flood Frequency
Flood Frequency Analysis
Statistics & Flood Frequency Chapter 3 – Part 1
Multinomial Distribution
Hydrologic Statistics
Statistics & Flood Frequency Chapter 3
Elementary Statistics
Presentation transcript:

WFM-6204: Hydrologic Statistics WFM 6204: Hydrologic Statistics © Dr. Akm Saiful Islam WFM-6204: Hydrologic Statistics Lecture-3: Probabilistic analysis: (Part-1) Akm Saiful Islam Institute of Water and Flood Management (IWFM) Bangladesh University of Engineering and Technology (BUET) December, 2006

Probability Distributions and Their Applications Discrete Distributions Binomial distribution Poisson distribution Continuous Distributions Normal distribution Lognormal distribution Gamma distribution Pearson Type III distribution Gumbel’s Extremal distribution

Binomial distribution Consider a discrete time scale. At each point on this time scale, an event may either occur or not occur. Let the probability of the event occurring be p for every point on the time scale. Thus, the occurrence of the event at any point on the time scale is independent of the history of any prior occurrences or non-occurrences. The probability of an occurrence at the i-th point on the time scale is p for i = 1,2,…... A process having these properties is said to be a Bernoulli process.

As an example of a Bernoulli process consider that during any year the probability of the maximum flow exceeding 10,000 cubic feet per second (cfs) on a particular river is p. Common terminology for a flow exceeding a given value is an exceedance. Further consider that the peak flow in any year is independent from year to year (a necessary condition for the process to be a Bernoulli process). Let be the probability of not exceeding 10,000 cfs. We can neglect the probability of a peak exactly 10000 cfs since the peak flow rates would be a continuous process so the probability of a peak exactly 10000 cfs would be zero. In this example, the time scale is discrete with the points nominally 1 year in time apart. We can now make certain probabilistic statements about the occurrence of a peak flow in excess of 10000 cfs (an exceedance).

For example, the probability of an exceedance occurring in year 3 and not in year 1 or 2 is since the process is independent from year to year. The probability of (exactly) one exceedance in any 3-year period is since the exceedance could occur in either the first, second, or third year. Thus the probability of (exactly) one exceedance in three years is . In a similar manner, the probability of 2 exceedances in 5 years can be found from the summation of the terms. It can be seen that each of theses terms is equivalent to and that the number of terms is equal to the number of ways of arranging 2 items (the p's) among 5 items (the p's and q's). Therefore the total number of terms is or 10 so that the probability of exactly 2 exceedances in 5 years is 10

This result can be generalized so that the probability of exceedances in n years is .The result is applicable to any Bernoulli process so that the probability of occurrences of an event in n independent trials if p is the probability of an occurrence in a single trial is given by: This equation is known as the binomial distribution. The binomial distribution and the Bernoulli process are not limited to a time scale. Any process that may occur with probability p at discrete points in time or space or in individual trials may be a Bernoulli process and follow the binomial distribution

The cumulative binomial distribution is and gives the probability of or fewer occurrences of an event in n independent trials if the probability of an occurrence in any trial is p. Continuing the above example, the probability of less than 3 exceedances in 5 years is The mean and variance of the binomial distribution are

The coefficient of skew is so that the distribution is symmetrical for skewed to the right for and skewed to the left for The binomial distribution has an additive property. That is if X has a binomial distribution with parameters n1 and p1 and Y has a binomial distribution with parameters n2 and p2, then Z=X+Y has a binomial distribution with parameters n=n1+n2 and p.

Example: In order to be 90 percent sure that a design storm is not exceeded in a 10 year period. What should be the return period of the design storm? Solution: Let p be the probability of the design storm being exceeded. The probability of no exceedances is given by: years.

Poisson distribution The Poisson distribution is like the binomial distribution in that it describes phenomena for which the average probability of an event is constant, independent of the number of previous events. In this case, how­ever, the system undergoes transitions randomly from one state with n occurrences of an event to another with (n+1) occurrences, in a process that is irreversible. That is, the ordering of the events cannot be inter­changed. Another distinction between the binomial and Poisson distribu­tions is that for the Poisson process the number of possible events should be large. The Poisson distribution may be inferred from the identity where the most probable number of occurrences of the event is .

If the factorial is expanded in a power series expansion, the probability P(r) that exactly r random occurrences will take place can be inferred as the th term in the series, i.e., This probability distribution leads directly to the interpretation that: = the probability that an event will not occur, = the probability that an event will occur exactly once, = the probability that an event will occur exactly twice, etc,

The mean and the variance of the Poisson distribution are: The coefficient of skew is so that as gets large, the distribution goes from a positively skewed distribution to a nearly symmetrical distribution. The cumulative Poisson probability that an event will occur x times or less is: Of course, the probability that the event will occur (x+1) or more times would be the complement of P(x).

Example: what is the probability that a storm with a return period of 20 years with occur once in 10-year period ? Solution:

Compare bi-nomial with Poissions The binomial distribution is useful for systems with two possible outcomes of events (failure–no failure) in cases where there is a known, finite number of (Bernoulli) trials and the ordering of the trials does not affect the outcome. The Poisson distribution treats systems in which randomly occurring phenomena cause irreversible transitions from one state to another.