Lecture 3 - 1 ERS 482/682 (Fall 2002) Information sources ERS 482/682 Small Watershed Hydrology.

Slides:



Advertisements
Similar presentations
Population vs. Sample Population: A large group of people to which we are interested in generalizing. parameter Sample: A smaller group drawn from a population.
Advertisements

Chapter 3 Properties of Random Variables
Hydrologic Statistics Reading: Chapter 11, Sections 12-1 and 12-2 of Applied Hydrology 04/04/2006.
Hydrologic Statistics
Probability and Statistics Mat 271E
MA-250 Probability and Statistics Nazar Khan PUCIT Lecture 3.
Statistics.
FREQUENCY ANALYSIS Basic Problem: To relate the magnitude of extreme events to their frequency of occurrence through the use of probability distributions.
Measures of Central Tendency. Central Tendency “Values that describe the middle, or central, characteristics of a set of data” Terms used to describe.
Review of Basics. REVIEW OF BASICS PART I Measurement Descriptive Statistics Frequency Distributions.
Review of Basics. REVIEW OF BASICS PART I Measurement Descriptive Statistics Frequency Distributions.
QUANTITATIVE DATA ANALYSIS
Lecture ERS 482/682 (Fall 2002) Precipitation ERS 482/682 Small Watershed Hydrology.
Chapter 13 Conducting & Reading Research Baumgartner et al Data Analysis.
Start Audio Lecture! FOR462: Watershed Science & Management 1 Streamflow Analysis Module 8.7.
Lecture ERS 482/682 (Fall 2002) Flood (and drought) prediction ERS 482/682 Small Watershed Hydrology.
Chapter 14 Analyzing Quantitative Data. LEVELS OF MEASUREMENT Nominal Measurement Nominal Measurement Ordinal Measurement Ordinal Measurement Interval.
Precipitation statistics Cumulative probability of events Exceedance probability Return period Depth-Duration-Frequency Analysis.
Descriptive Statistics
Probability and Statistics Review
Lecture II-2: Probability Review
CE 374K Hydrology Frequency Factors. Frequency Analysis using Frequency Factors f(x) x xTxT.
Flood Frequency Analysis
Hydrologic Statistics
Describing Data: Numerical
@ 2012 Wadsworth, Cengage Learning Chapter 5 Description of Behavior Through Numerical 2012 Wadsworth, Cengage Learning.
Fall 2013 Lecture 5: Chapter 5 Statistical Analysis of Data …yes the “S” word.
Estimation of Areal Precipitation from point measurements Most often interested in quantifying rainfall over an entire watershed. Has to be inferred from.
Areal Estimation techniques Two types of technique: 1. Direct weighted averages 2. Surface fitting methods DIRECT WEIGHTED AVERAGE METHODS use the equation:
Data Handbook Chapter 4 & 5. Data A series of readings that represents a natural population parameter A series of readings that represents a natural population.
Statistics Recording the results from our studies.
Measures of Dispersion
FREQUENCY ANALYSIS.
Lecture 5: Chapter 5: Part I: pg Statistical Analysis of Data …yes the “S” word.
Fundamentals of Data Analysis Lecture 3 Basics of statistics.
Determination of Sample Size: A Review of Statistical Theory
Statistics for Psychology!
DES 606 : Watershed Modeling with HEC-HMS Module 8 Theodore G. Cleveland, Ph.D., P.E 29 July 2011.
More Precipitation Hydrology Spring 2013 Instructor: Eric Peterson.
§ 5.3 Normal Distributions: Finding Values. Probability and Normal Distributions If a random variable, x, is normally distributed, you can find the probability.
Appendix B: Statistical Methods. Statistical Methods: Graphing Data Frequency distribution Histogram Frequency polygon.
PCB 3043L - General Ecology Data Analysis. PCB 3043L - General Ecology Data Analysis.
Summarizing Risk Analysis Results To quantify the risk of an output variable, 3 properties must be estimated: A measure of central tendency (e.g. µ ) A.
Statistics in Hydrology Mean, median and mode (central tendency) Dispersion: the spread of the items in a data set around its central value.
Statistical Analysis of Data. What is a Statistic???? Population Sample Parameter: value that describes a population Statistic: a value that describes.
Probability and Distributions. Deterministic vs. Random Processes In deterministic processes, the outcome can be predicted exactly in advance Eg. Force.
Quality Control: Analysis Of Data Pawan Angra MS Division of Laboratory Systems Public Health Practice Program Office Centers for Disease Control and.
1 Day 1 Quantitative Methods for Investment Management by Binam Ghimire.
GEOG 441 Watershed Systems Precipitation Monday 1/26/2009.
Module 10: Average Rainfall Theodore G. Cleveland, Ph.D., P.E, M. ASCE, F. EWRI August 2015 Module 10 1.
PROBABILITY DISTRIBUTION. Probability Distribution of a Continuous Variable.
AP PSYCHOLOGY: UNIT I Introductory Psychology: Statistical Analysis The use of mathematics to organize, summarize and interpret numerical data.
Simple Linear Regression
AP Biology Intro to Statistics
Summary of Prev. Lecture
Review of Descriptive Statistics
HYDROLOGY Lecture 12 Probability
Flood Frequency Analysis
Descriptive Statistics
More basics: central tendency, variability, populations and samples.
Central Tendency Central Tendency – measures of location for a distribution Mode – the commonly occurring number in a data set Median – the middle score.
Central Tendency.
Hydrologic Statistics
CHAPTER 5 Fundamentals of Statistics
Descriptive Statistics: Describing Data
Continuous Statistical Distributions: A Practical Guide for Detection, Description and Sense Making Unit 3.
Making Sense of Measures of Center Investigation 2
HYDROLOGY Lecture 12 Probability
BUSINESS MARKET RESEARCH
Descriptive statistics for groups:
Presentation transcript:

Lecture ERS 482/682 (Fall 2002) Information sources ERS 482/682 Small Watershed Hydrology

Lecture ERS 482/682 (Fall 2002) Issues Model errors –Assumptions –Function Water balance

Lecture ERS 482/682 (Fall 2002) Issues Model errors Measurement errors Figure 2 (Sullivan et al. 1996)

Lecture ERS 482/682 (Fall 2002) Issues Model errors Measurement errors Spatial variability Temporal variability Figure 2 (Sullivan et al. 1996)

Lecture ERS 482/682 (Fall 2002) Model errors Check and be aware of assumptions Calibration Validation Verification

Lecture ERS 482/682 (Fall 2002) Measurement errors Estimate the error –Instrument error –Data error Standard deviation of normal distribution  95% probability that an error will be between ±1.96 SD of the true value

Lecture ERS 482/682 (Fall 2002) frequency

Lecture ERS 482/682 (Fall 2002) RELATIVE frequency

Lecture ERS 482/682 (Fall 2002) Normal distribution Kurtosis: flat vs. peaked standard deviation mean particular error

Lecture ERS 482/682 (Fall 2002) Descriptive statistics Mean, For errors, we hope this is 0!

Lecture ERS 482/682 (Fall 2002) Measures of central tendency Mean Center of gravity Median Half the x-values are smaller and half are larger Mode Value of x with the largest frequency

Lecture ERS 482/682 (Fall 2002) Descriptive statistics Mean, WHY?

Lecture ERS 482/682 (Fall 2002) Descriptive statistics Mean, ss p =.95

Lecture ERS 482/682 (Fall 2002) Measurement errors Estimating missing data (Sec ) –Station-average method –Normal-ratio method –Inverse-distance weighting –Regression

Lecture ERS 482/682 (Fall 2002) Station-average method p1p1 p2p2 p3p3 p4p4 p5p5 p6p6 p7p7 G = # of gages with data Use when gage values are similar

Lecture ERS 482/682 (Fall 2002) Normal-ratio method p1p1 p2p2 p3p3 p4p4 p5p5 p6p6 p7p7 G = # of gages with data P 0 = average annual precip at gage 0 P g = average annual precip at gage g Use when gage values are not similar

Lecture ERS 482/682 (Fall 2002) Inverse-distance weighting p1p1 p2p2 p3p3 p4p4 p5p5 p6p6 p7p7 G = # of gages with data d g = distance of gage g from gage 0 b = 1 or 2

Lecture ERS 482/682 (Fall 2002) Regression p1p1 p2p2 p3p3 p4p4 p5p5 p6p6 p7p7 G = # of gages with data b g = regression coefficient for gage g Caution: Series and data must be independent

Lecture ERS 482/682 (Fall 2002) Spatial variability P = total precipitation on the watershed A = area of watershed

Lecture ERS 482/682 (Fall 2002) Weighted averages w g = weight of gage g

Lecture ERS 482/682 (Fall 2002) Weighted averages Thiessen polygons a g = area of subregion for gage g

Lecture ERS 482/682 (Fall 2002) Weighted averages Isohyetal methods –isohyet: contour of equal precipitation a i = area of subregion between p i- and p i+ isohyets p 0.5 p 1.0 p 1.5 p 2.0 a2a2

Lecture ERS 482/682 (Fall 2002) Temporal variability Exceedence probability or return period Stochastic hydrology (GEOL 702J) –PDF = probability distribution function f(x) = p (X = x) –1 – CDF exceedence probability1-F(x) = p(X > x) exceedence probability probability non-exceedence probability –CDF = cumulative distribution function F(x) = p (X  x)

Lecture ERS 482/682 (Fall 2002) Displaying cumulative frequency f(x) Discharge (cfs) More

Lecture ERS 482/682 (Fall 2002) Displaying cumulative frequency f(x) Discharge (cfs) More

Lecture ERS 482/682 (Fall 2002) Displaying cumulative frequency F(x) 0 1

Lecture ERS 482/682 (Fall 2002) Normal distribution CDF: Given x Find P(X  x)CDF PDF

Lecture ERS 482/682 (Fall 2002) Normal distribution Non-exceedence probability: P (X  x) Exceedence probability: P (X>x)

Lecture ERS 482/682 (Fall 2002) Return period 10-year design = or 1 – P(X  x) 50-year design = 100-year design = Does the 1-year storm occur every year???

Lecture ERS 482/682 (Fall 2002) Normal distribution 10-year design = Given F(x)=P(X  x) What is x?

Lecture ERS 482/682 (Fall 2002) Using the normal distribution as a model 70% non-exceedence probability

Lecture ERS 482/682 (Fall 2002) Using the normal distribution as a model % exceedence probability

Lecture ERS 482/682 (Fall 2002) Figures 2-7, 2-8, 2-9 (Dunne & Leopold 1978)