Introduction to Hydrology (Geog 3511) Fall 2002 Assignment 10: Streamflow Analysis

Size: px
Start display at page:

Download "Introduction to Hydrology (Geog 3511) Fall 2002 Assignment 10: Streamflow Analysis"

Transcription

1 Introduction to Hydrology (Geog 3511) Fall 22 Assignment 1: Streamflow Analysis Assigned: November 26 Due: December 5 4 possible points. SHOW ALL YOUR WORK. CITE SOURCES OF EQUATIONS USED. WRITE THE QUESTION AT THE START OF EACH ANSWER. Data This lab is based on data that was collected in the Martinelli drainage, at Niwot Ridge. Surface water samples were collected from a seasonal stream draining the 8-ha Martinelli catchment about 4m from the experimental area on Niwot Ridge. The Martinelli catchment has a poorly developed soil structure with little vegetation and is dominated by a late-melting snowpatch [Caine, 1989]. To look at the area on the web, go to: Stage Rating Curve The following stage-discharge data were collected in order to define the stage-rating curve. Stage(cm) Discharge(l/s) Q1) Develop a rating curve for the recorded data. The rating curve should be of the form Q! as b where a and b are parameters that are fit using a power regression, S is stage height in centimeters, and Q is the discharge in L/s. Plot the data and the rating curve using linear axes for both the stage and discharge. What is the rating curve (using the variables Q and S)? (4 points) Taking the logarithm of each side of the equation gives us log!q"! log!a" " b log!s" Fit a linear line to the log-log data. log!q"!!1.129 " log!S" Extract the coefficients a! 1!1.129! # 1!2 Therefore the rating curve is b! Q# l s $!.789!S#cm$" This equation can also be determined by fitting a power trendline in Excel to the data.

2 Comparison of records and rating curve Rating Records Rating Curve: Power (Rating Records) y =.789x R 2 = stage [cm] Q2) Plot the rating curve on log-log coordinates and show the stage - discharge records on the same plot. How well do these data (visually) match the curve when plotted in a log-log format? (3 points) Comparison of records and rating curve y =.789x R 2 =.918 Rating Records Rating Curve: Power (Rating Records) stage [cm] The model appears to fit the data better when displayed in log-log coordinates, which minimize the appearance of the error at large stage heights. Stage-Discharge records Some stage - discharge records for the channel at Martinelli Snowpatch, Niwot Ridge, Indian Peaks are included in the attached file Q3) Plot the discharge hydrograph for July 4 to 18 inc. (use a 1 minute sampling interval) (3 points) Q4) Use the rating curve to determine the stage readings from July 4 to 18 inclusive. (use a 1-minute sampling interval) (4 points)

3 Q5) Plot the air temperature for the same time period. (3 points) Martnelli Time Series 3 air temperature [deg C] or stage level [cm] or Water level [cm] air temperature [deg C] -5 7/4/94 7/5/94 7/6/94 7/7/94 7/8/94 7/9/94 7/1/94 7/11/94 7/12/94 7/13/94 7/14/94 7/15/94 7/16/94 7/17/94 7/18/94 7/19/94 Q6) What date recorded peak flow during this period? Describe the variation in peak flow timing over the two weeks? How is it related to the temperature? (4 points) On 7/4/1994 at 2:15pm, the peak discharge was estimated to be L/s. The peak flow generally occurs between 1 and 3pm. The timing of the peak discharge is illustrated in the graph below. Maximum Daily Discharge Timing 16: 15: Time of Day 14: 13: 12: 7/3/1994 7/5/1994 7/7/1994 7/9/1994 7/11/1994 7/13/1994 7/15/1994 7/17/1994 7/19/1994 Date The timing of the daily peak is related to the temperature. Increased temperatures correspond with earlier discharge peaks. (see the graph below)

4 Maximum Daily Discharge vs. Temperature 16: 15: Time of Day 14: 13: y = -.61x R 2 = : Temperature [deg C] Seasonal Discharge Hydrograph Lets make a seasonal hydrography using real data from the Martinelli catchment for You ll need to obtain this data from the Niwot Ridge LTER website: select "Data" select "Data set catalog and keyword/investigator search" select "Hydrology and Geomorphology" select "Martinelli Streamflow" save as text or ascii file (should be the default). read the metadata for information on units, etc. cut out the 1985 data in EXCEL or whatever software package you prefer. Q7) Make a seasonal hydrograph for 1994 using these data. Be sure to label axes and include units. Identify the rising limb and recession limb of the hydrograph. (3 points)

5 1994 Martinelli Daily Discharge Volume 3 25 daily discharge volume [m3] rising limb recession limb 5 4/16/1994 5/6/1994 5/26/1994 6/15/1994 7/5/1994 7/25/1994 8/14/1994 9/3/1994 9/23/1994 Q8) On what day or days was peak discharge and what was the amount of peak discharge? (2 points) Peak discharge was on 6/1/94 and was 2759 cubic meters per day. Q9) Estimate the recession coefficient as an average for the falling flows of the record. Use the data from period 7/14-8/6. The regression equation is of the form Q! Q e!ct where Q is the discharge at the start of the regression time period and c is the exponential regression coefficient. (Hint: the regression coeffiecient has units!) Plot the regression curve against the data for this time period. (4 points) By visually fitting the curve by altering the Q and c parameters, we can arrive at the regression equation of Q!!32 m 3 "e!.5 1 t d

UNIT HYDROGRAPH AND EFFECTIVE RAINFALL S INFLUENCE OVER THE STORM RUNOFF HYDROGRAPH

UNIT HYDROGRAPH AND EFFECTIVE RAINFALL S INFLUENCE OVER THE STORM RUNOFF HYDROGRAPH UNIT HYDROGRAPH AND EFFECTIVE RAINFALL S INFLUENCE OVER THE STORM RUNOFF HYDROGRAPH INTRODUCTION Water is a common chemical substance essential for the existence of life and exhibits many notable and unique

More information

Quadratic Regressions Group Acitivity 2 Business Project Week #4

Quadratic Regressions Group Acitivity 2 Business Project Week #4 Quadratic Regressions Group Acitivity 2 Business Project Week #4 In activity 1 we created a scatter plot on the calculator using a table of values that were given. Some of you were able to create a linear

More information

Introduction to Hydrology, Part 2. Notes, Handouts

Introduction to Hydrology, Part 2. Notes, Handouts Introduction to Hydrology, Part 2 Notes, Handouts Precipitation Much of hydrology deals with precipitation How much? How frequently/infrequently? What form? How quickly? Seasonal variation? Drought frequency?

More information

Correlation between infiltration capacity and permeability of soil

Correlation between infiltration capacity and permeability of soil International Journal of Technical Innovation in Modern Engineering & Science (IJTIMES) Impact Factor: 5.22 (SJIF-2017), e-issn: 2455-2585 Volume 4, Issue 7, July-2018 Correlation between infiltration

More information

Module 3. Lecture 6: Synthetic unit hydrograph

Module 3. Lecture 6: Synthetic unit hydrograph Lecture 6: Synthetic unit hydrograph Synthetic Unit Hydrograph In India, only a small number of streams are gauged (i.e., stream flows due to single and multiple storms, are measured) There are many drainage

More information

Monitoring of water levels and flood discharge

Monitoring of water levels and flood discharge Monitoring of water levels and flood discharge Changes Workshop TS-02 & 11 th edition International Summer School Environmental Hazards & Sustainable Development in Mountain Regions Thom Bogaard Delft

More information

Stream Hydrology. Watershed 8/29/13. Area that contributes water to a point on a stream Scale is user-defined Other names: Catchment Drainage basin

Stream Hydrology. Watershed 8/29/13. Area that contributes water to a point on a stream Scale is user-defined Other names: Catchment Drainage basin Stream Hydrology Watershed Area that contributes water to a point on a stream Scale is user-defined Other names: Catchment Drainage basin http://warnercnr.colostate.edu/geo/front_range/poudre.php# 1 Basics

More information

M. Meering. 1 Note for the authors and editor

M. Meering. 1 Note for the authors and editor Hydrol. Earth Syst. Sci. Discuss., 12, C4732 C4741, 2015 www.hydrol-earth-syst-sci-discuss.net/12/c4732/2015/ Author(s) 2015. This work is distributed under the Creative Commons Attribute 3.0 License.

More information

2.f. Two Parameter Comparisons

2.f. Two Parameter Comparisons 2.f. Two Parameter Comparisons http://wql-data.heidelberg.edu/index2.html 9/27/05 Introduction Sometimes it is useful to study the relationships between two parameters in a stream. For example the relationships

More information

Comparison of Recharge Estimation Methods Used in Minnesota

Comparison of Recharge Estimation Methods Used in Minnesota Comparison of Recharge Estimation Methods Used in Minnesota by Geoffrey Delin, Richard Healy, David Lorenz, and John Nimmo Minnesota Ground Water Association Spring Conference Methods for Solving Complex

More information

Introduction, HYDROGRAPHS

Introduction, HYDROGRAPHS HYDROGRAPHS Sequence of lecture Introduction Types of Hydrograph Components of Hydrograph Effective Rainfall Basin Lag or Time Lag Parts of Hydrograph Hydrograph Analysis Factors Affecting Hydrograph Shape

More information

Stream hydrographs. Stream hydrographs. Baseflow. Graphs of river stage or discharge at a single location as a function of time

Stream hydrographs. Stream hydrographs. Baseflow. Graphs of river stage or discharge at a single location as a function of time Stream hydrographs Graphs of river stage or discharge at a single location as a function of time Hydrologic og budget Discharge: units? How is it measured? Show fluctuating water levels in response to

More information

The Drainage Basin System

The Drainage Basin System The Drainage Basin System These icons indicate that teacher s notes or useful web addresses are available in the Notes Page. This icon indicates that the slide contains activities created in Flash. These

More information

CS130 Software Tools. Fall 2010 Regression and Excel

CS130 Software Tools. Fall 2010 Regression and Excel Software Tools Regression and Excel 1 Regression Analysis (Part 1) Regression Analysis The statistical crystal ball Regression analysis is a form of statistical analysis used for forecasting. We are going

More information

Statistics: Data Analysis and Presentation. Fr Clinic II

Statistics: Data Analysis and Presentation. Fr Clinic II Statistics: Data Analysis and Presentation Fr Clinic II Overview Tables and Graphs Populations and Samples Mean, Median, and Standard Deviation Standard Error & 95% Confidence Interval (CI) Error Bars

More information

CHAPTER FIVE Runoff. Engineering Hydrology (ECIV 4323) Instructors: Dr. Yunes Mogheir Dr. Ramadan Al Khatib. Overland flow interflow

CHAPTER FIVE Runoff. Engineering Hydrology (ECIV 4323) Instructors: Dr. Yunes Mogheir Dr. Ramadan Al Khatib. Overland flow interflow Engineering Hydrology (ECIV 4323) CHAPTER FIVE Runoff Instructors: Dr. Yunes Mogheir Dr. Ramadan Al Khatib Overland flow interflow Base flow Saturated overland flow ١ ٢ 5.1 Introduction To Runoff Runoff

More information

2. Potential Extreme Peak Discharge in Texas

2. Potential Extreme Peak Discharge in Texas 2. Potential Extreme Peak Discharge in Texas This part of the work is focused on using GIS to apply the latest USGS peak discharge equations to create a 500m grid that stores the potential peak discharge

More information

1. Stream Network. The most common approach to quantitatively describing stream networks was postulated by Strahler (1952).

1. Stream Network. The most common approach to quantitatively describing stream networks was postulated by Strahler (1952). 1. Stream Network The most common approach to quantitatively describing stream networks was postulated by Strahler (1952). First Order Streams streams with no tributaries. Second Order Streams begin at

More information

Homework # 3 1. (5 pts) (A) (B) 2. (5 pts) (A) (B) 3. (5 pts) 4. (5 pts) 5. (5 pts) 6. (5 pts)

Homework # 3 1. (5 pts) (A) (B) 2. (5 pts) (A) (B) 3. (5 pts) 4. (5 pts) 5. (5 pts) 6. (5 pts) Homework # 3 (6 pages!) Introduction to Hydrogeology (GEO 346C), Spring 2010 Due: 2/19/2010 (5 pm) Instructor: Bayani Cardenas, cardenas@jsg.utexas.edu, EPS 3.160 TA: Travis Swanson, tswanson@mail.utexas.edu,

More information

FAST WATER / SLOW WATER AN EVALUATION OF ESTIMATING TIME FOR STORMWATER RUNOFF

FAST WATER / SLOW WATER AN EVALUATION OF ESTIMATING TIME FOR STORMWATER RUNOFF FAST WATER / SLOW WATER AN EVALUATION OF ESTIMATING TIME FOR STORMWATER RUNOFF Factors Affecting Stormwater Runoff: Rainfall intensity % Impervious surfaces Watershed size Slope Soil type, soil compaction

More information

Indicators of Hydrologic Alteration (IHA) software, Version 7.1

Indicators of Hydrologic Alteration (IHA) software, Version 7.1 Indicators of Hydrologic Alteration (IHA) software, Version 7.1 IHA Software Analyzes hydrologic characteristics and their changes over time. Computes 67 ecologicallyrelevant flow statistics using daily

More information

Runoff Hydrographs. The Unit Hydrograph Approach

Runoff Hydrographs. The Unit Hydrograph Approach Runoff Hydrographs The Unit Hydrograph Approach Announcements HW#6 assigned Storm Water Hydrographs Graphically represent runoff rates vs. time Peak runoff rates Volume of runoff Measured hydrographs are

More information

Density Measurements Background

Density Measurements Background Density Measurements Background The density (ρ) of a substance or an object is defined by its mass (m) divided by its volume (V):!"#$%&' =!"##!"#$%&!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! =!! The units used

More information

CIVE22 BASIC HYDROLOGY Jorge A. Ramírez Homework No 7

CIVE22 BASIC HYDROLOGY Jorge A. Ramírez Homework No 7 Hydrologic Science and Engineering Civil and Environmental Engineering Department Fort Collins, CO 80523-1372 (970) 491-7621 CIVE22 BASIC HYDROLOGY Jorge A. Ramírez Homework No 7 1. Obtain a Unit Hydrograph

More information

How to extrapolate rating curve

How to extrapolate rating curve World Bank & Government of The Netherlands funded Training module # SWDP - 31 How to extrapolate rating curve New Delhi, November 1999 CSMRS Building, 4th Floor, Olof Palme Marg, Hauz Khas, New Delhi 11

More information

= = Intro to Statistics for the Social Sciences. Name: Lab Session: Spring, 2015, Dr. Suzanne Delaney

= = Intro to Statistics for the Social Sciences. Name: Lab Session: Spring, 2015, Dr. Suzanne Delaney Name: Intro to Statistics for the Social Sciences Lab Session: Spring, 2015, Dr. Suzanne Delaney CID Number: _ Homework #22 You have been hired as a statistical consultant by Donald who is a used car dealer

More information

What is runoff? Runoff. Runoff is often defined as the portion of rainfall, that runs over and under the soil surface toward the stream

What is runoff? Runoff. Runoff is often defined as the portion of rainfall, that runs over and under the soil surface toward the stream What is runoff? Runoff Runoff is often defined as the portion of rainfall, that runs over and under the soil surface toward the stream 1 COMPONENTS OF Runoff or STREAM FLOW 2 Cont. The types of runoff

More information

Introduction. Keywords: Oil Palm, hydrology, HEC-HMS, HEC-RAS. a * b*

Introduction. Keywords: Oil Palm, hydrology, HEC-HMS, HEC-RAS. a * b* The Effect of Land Changes Towards in Sg. Pandan Perwira Bin Khusairi Rahman 1,a* and Kamarul Azlan bin Mohd Nasir 1,b 1 Faculty of Civil Engineering, Universiti Teknologi Malaysia, Malaysia a * wirakhusairirahman@gmail.com,

More information

Measuring discharge. Climatological and hydrological field work

Measuring discharge. Climatological and hydrological field work Measuring discharge Climatological and hydrological field work 1. Background Discharge (or surface runoff Q s) refers to the horizontal water flow occurring at the surface in rivers and streams. It does

More information

HERPIC County Storm Drainage Manual

HERPIC County Storm Drainage Manual HERPIC County Storm Drainage Manual C h r is t o p h e r B. B u r k e Research Assistant Highway Extension and Research Project for Indiana Counties Purdue University The HERPIC (Highway Extension and

More information

Module 3. Lecture 4: Introduction to unit hydrograph

Module 3. Lecture 4: Introduction to unit hydrograph Lecture 4: Introduction to unit hydrograph (UH) The unit hydrograph is the unit pulse response function of a linear hydrologic system. First proposed by Sherman (1932), the unit hydrograph (originally

More information

CE 115 Introduction to Civil Engineering Graphics and Data Presentation Application in CE Materials

CE 115 Introduction to Civil Engineering Graphics and Data Presentation Application in CE Materials CE 115 Introduction to Civil Engineering Graphics and Data Presentation Application in CE Materials Dr. Fouad M. Bayomy, PE Professor of Civil Engineering University of Idaho Moscow, ID 83844-1022 Graphics

More information

GRACE: Tracking Water from Space. Groundwater Storage Changes in California s Central Valley Data Analysis Protocol for Excel: PC

GRACE: Tracking Water from Space. Groundwater Storage Changes in California s Central Valley Data Analysis Protocol for Excel: PC Groundwater Storage Changes in California s Central Valley Data Analysis Protocol for Excel: PC 2007-10 Before GRACE it was very difficult to estimate how the total volumes of groundwater are changing.

More information

SEES 503 SUSTAINABLE WATER RESOURCES. Floods. Instructor. Assist. Prof. Dr. Bertuğ Akıntuğ

SEES 503 SUSTAINABLE WATER RESOURCES. Floods. Instructor. Assist. Prof. Dr. Bertuğ Akıntuğ SEES 503 SUSTAINABLE WATER RESOURCES Floods Instructor Assist. Prof. Dr. Bertuğ Akıntuğ Civil Engineering Program Middle East Technical University Northern Cyprus Campus SEES 503 Sustainable Water Resources

More information

Development of Rating Curve for Ofu River at Oforachi Hydrometric Station M. I. Alfa 1*, D. B. Adie 2, M. A. Ajibike 2, O. J.

Development of Rating Curve for Ofu River at Oforachi Hydrometric Station M. I. Alfa 1*, D. B. Adie 2, M. A. Ajibike 2, O. J. 14 NIGERIAN JOURNAL OF TECHNOLOGICAL DEVELOPMENT, VOL. 15, NO. 1, MARCH 2018 Development of Rating Curve for Ofu River at Oforachi Hydrometric Station M. I. Alfa 1*, D. B. Adie 2, M. A. Ajibike 2, O. J.

More information

ENGINEERING HYDROLOGY

ENGINEERING HYDROLOGY ENGINEERING HYDROLOGY Prof. Rajesh Bhagat Asst. Professor Civil Engineering Department Yeshwantrao Chavan College Of Engineering Nagpur B. E. (Civil Engg.) M. Tech. (Enviro. Engg.) GCOE, Amravati VNIT,

More information

Pipe Flow Hydraulics

Pipe Flow Hydraulics CHE- 3115 Chemical Engineering Processes I - Laboratory Experiment 1 Pipe Flow Hydraulics BACKGROUND The conveyance of fluids through fixed conduits is the most common unit operation in engineering practice.

More information

Appendix 1: Baseflow and Baseflow Metrics

Appendix 1: Baseflow and Baseflow Metrics Page 1 of 12 Appendix 1: Baseflow and Baseflow Metrics Contents A.1 Baseflow Separation Techniques... 2 A.1.1 HYSEP... 2 A.1.2 PART... 3 A.1.3 Digital Filter... 4 A.2 Estimating Recharge... 7 A.2.1 Baseflow

More information

Examination of PRZM5.0 Storm Rainfall Depth and Distribution Algorithms Compared to Current U.S. Storm Trends

Examination of PRZM5.0 Storm Rainfall Depth and Distribution Algorithms Compared to Current U.S. Storm Trends Examination of PRZM5.0 Storm Rainfall Depth and Distribution Algorithms Compared to Current U.S. Storm Trends August 24, 2016 Tammara L. Estes (Stone Environmental Inc.) Kevin L. Armbrust, Ph.D. (Louisiana

More information

= = Name: Lab Session: CID Number: The database can be found on our class website: Donald s used car data

= = Name: Lab Session: CID Number: The database can be found on our class website: Donald s used car data Intro to Statistics for the Social Sciences Fall, 2017, Dr. Suzanne Delaney Extra Credit Assignment Instructions: You have been hired as a statistical consultant by Donald who is a used car dealer to help

More information

Learning objectives. Upon successful completion of this lecture, the participants will be able to describe:

Learning objectives. Upon successful completion of this lecture, the participants will be able to describe: Solomon Seyoum Learning objectives Upon successful completion of this lecture, the participants will be able to describe: The different approaches for estimating peak runoff for urban drainage network

More information

A comparative study of the methods for estimating streamflow at ungauged sites

A comparative study of the methods for estimating streamflow at ungauged sites 22nd International Congress on Modelling and Simulation, Hobart, Tasmania, Australia, 3 to 8 December 2017 mssanz.org.au/modsim2017 A comparative study of the methods for estimating streamflow at ungauged

More information

A simple model for low flow forecasting in Mediterranean streams

A simple model for low flow forecasting in Mediterranean streams European Water 57: 337-343, 2017. 2017 E.W. Publications A simple model for low flow forecasting in Mediterranean streams K. Risva 1, D. Nikolopoulos 2, A. Efstratiadis 2 and I. Nalbantis 1* 1 School of

More information

Unit 2: Geomorphologic and Hydrologic Characteristics of Watersheds. ENVS 435: Watershed Management INSTR.: Dr. R.M. Bajracharya

Unit 2: Geomorphologic and Hydrologic Characteristics of Watersheds. ENVS 435: Watershed Management INSTR.: Dr. R.M. Bajracharya Unit 2: Geomorphologic and Hydrologic Characteristics of Watersheds ENVS 435: Watershed Management INSTR.: Dr. R.M. Bajracharya Watersheds are hydro-geologic units Water flow and cycling are basic and

More information

Term Project. NFIE-River: Cross section approximations for hydraulic channel routing model in the San Antonio and Guadalupe River Basins.

Term Project. NFIE-River: Cross section approximations for hydraulic channel routing model in the San Antonio and Guadalupe River Basins. Flood Forecasting Spring - 2015 Due Friday 05/08/2015 Alfredo Hijar Term Project NFIE-River: Cross section approximations for hydraulic channel routing model in the San Antonio and Guadalupe River Basins.

More information

WHAT IS SOIL? soil is a complex system of organic and inorganic (mineral) compounds Soil properties depend on formation process particle size climate

WHAT IS SOIL? soil is a complex system of organic and inorganic (mineral) compounds Soil properties depend on formation process particle size climate Lecture 5, Soil water and infiltration WHAT IS SOIL? soil is a complex system of organic and inorganic (mineral) compounds Soil properties depend on formation process particle size climate THE IMPORTANCE

More information

Outline of Teton Valley diversion model

Outline of Teton Valley diversion model Outline of Teton Valley diversion model Rob Van Kirk, Department of Mathematics, Humboldt State University October 21, 2011 R script diversions.r Input files 1. "StreamQ_from_1962.csv" This file contains

More information

TECHNICAL MEMORANDUM. SUBJECT: Determination of watershed historic peak flow rates as the basis for detention basin design

TECHNICAL MEMORANDUM. SUBJECT: Determination of watershed historic peak flow rates as the basis for detention basin design TECHNICAL MEMORANDUM FROM: Ken MacKenzie and Ryan Taylor SUBJECT: Determination of watershed historic peak flow rates as the basis for detention basin design DATE: June 7, 2012 The purpose of this memorandum

More information

University. San Luis Obispo, CA Irrigation Training and Research Center (ITRC)

University. San Luis Obispo, CA Irrigation Training and Research Center (ITRC) NON-STANDARD STRUCTURE FLOW MEASUREMENT EVALUATION USING THE FLOW RATE INDEXING PROCEDURE QIP Stuart Styles 1 Presented at USCID Third International Conference on Irrigation and Drainage San Diego, CA,

More information

RAINFALL-RUNOFF RELATIONSHIPS AND FLOW FORECASTING, OGUN RIVER, NIGERIA

RAINFALL-RUNOFF RELATIONSHIPS AND FLOW FORECASTING, OGUN RIVER, NIGERIA JOURNAL OF ENVIRONMENTAL HYDROLOGY The Electronic Journal of the International Association for Environmental Hydrology On the World Wide Web at http://www.hydroweb.com VOLUME 16 008 RAINFALL-RUNOFF RELATIONSHIPS

More information

9.7 Getting Schooled. A Solidify Understanding Task

9.7 Getting Schooled. A Solidify Understanding Task 35 9.7 Getting Schooled A Solidify Understanding Task In Getting More $, Leo and Araceli noticed a difference in men s and women s salaries. Araceli thought that it was unfair that women were paid less

More information

Water Budget III: Stream Flow P = Q + ET + G + ΔS

Water Budget III: Stream Flow P = Q + ET + G + ΔS Water Budget III: Stream Flow P = Q + ET + G + ΔS Why Measure Streamflow? Water supply planning How much water can we take out (without harming ecosystems we want to protect) Flood protection How much

More information

Water Budget III: Stream Flow P = Q + ET + G + ΔS

Water Budget III: Stream Flow P = Q + ET + G + ΔS Water Budget III: Stream Flow P = Q + ET + G + ΔS Why Measure Streamflow? Water supply planning How much water can we take out (without harming ecosystems we want to protect) Flood protection How much

More information

SECTION III: WATERSHED TECHNICAL ANALYSIS

SECTION III: WATERSHED TECHNICAL ANALYSIS Trout Creek Watershed Stormwater Management Plan SECTION III: WATERSHED TECHNICAL ANALYSIS A. Watershed Modeling An initial step this study of the Trout Creek watershed was the selection of a stormwater

More information

Water Budget III: Stream Flow P = Q + ET + G + ΔS

Water Budget III: Stream Flow P = Q + ET + G + ΔS Water Budget III: Stream Flow P = Q + ET + G + ΔS Why Measure Streamflow? Water supply planning How much water can we take out (without harming ecosystems we want to protect) Flood protection How much

More information

Alberta Flood Envelope Curve Analysis

Alberta Flood Envelope Curve Analysis Alberta Flood Envelope Curve Analysis Introduction : Flood envelope curves have been used for many years as an attempt to provide context on the magnitude of flood events or design values. One common envelope

More information

Water Budget III: Stream Flow P = Q + ET + G + ΔS

Water Budget III: Stream Flow P = Q + ET + G + ΔS Water Budget III: Stream Flow P = Q + ET + G + ΔS Why Measure Streamflow? Water supply planning How much water can we take out (without harming ecosystems we want to protect) Flood protection How much

More information

Appendix C: Flow Estimation and Measurement Techniques of the Scenic Rivers Monitoring Program. Ungaged Stream Flow Estimation

Appendix C: Flow Estimation and Measurement Techniques of the Scenic Rivers Monitoring Program. Ungaged Stream Flow Estimation Appendix C: Flow Estimation and Measurement Techniques of the Scenic Rivers Monitoring Program Eric Wentz and Robert Limbeck Ungaged Stream Flow Estimation Two USGS computer applications were used by DRBC

More information

Lab 6 - Pumping Test. Pumping Test. Laboratory 6 HWR 431/

Lab 6 - Pumping Test. Pumping Test. Laboratory 6 HWR 431/ Pumping Test Laboratory 6 HWR 431/531 7-1 Introduction: Aquifer tests are performed to evaluate the capacity of an aquifer to meet municipal or industrial water requirements. Hydraulic characteristics

More information

HYDROLOGIC & HYDRAULIC ASPECTS of the Walnut Street Bridge over the Schuylkill River Philadelphia, PA

HYDROLOGIC & HYDRAULIC ASPECTS of the Walnut Street Bridge over the Schuylkill River Philadelphia, PA HYDROLOGIC & HYDRAULIC ASPECTS of the Walnut Street Bridge over the Schuylkill River Philadelphia, PA J. Richard Weggel CAEE201 Lectures 30 April & 2 May 2007 HYDROLOGY (Natural Science) Study of the waters

More information

Engineering Hydrology. Class 16: Direct Runoff (DRO) and Unit Hydrographs

Engineering Hydrology. Class 16: Direct Runoff (DRO) and Unit Hydrographs Engineering Hydrology Class 16: and s Topics and Goals: 1. Calculate volume of DRO from a hydrograph; 2. Complete all steps to develop a. Class 14: s? HG? Develop Ocean Class 14: s? HG? Develop Timing

More information

Examining the Parameters of the Hardy-Weinberg Equation using an Excel Spreadsheet Part 1

Examining the Parameters of the Hardy-Weinberg Equation using an Excel Spreadsheet Part 1 Examining the Parameters of the Hardy-Weinberg Equation using an Excel Spreadsheet Part 1 Part A - Essential Knowledge Background Information 1 Key Vocabulary Hardy-Weinberg Equation Hardy-Weinberg Equilibrium

More information

5/11/2007. WinTR-55 for Plan Reviewers Small Watershed Hydrology Hydrology Terms and Definitions

5/11/2007. WinTR-55 for Plan Reviewers Small Watershed Hydrology Hydrology Terms and Definitions WinTR-55 for Plan Reviewers Small Watershed Hydrology Hydrology Terms and Definitions 1 Course Outline Overview Review of Hydrology Terms and Definitions Modeling Single Sub-area Watersheds Multiple Sub-area

More information

Development of Runoff Depth Map for Alberta

Development of Runoff Depth Map for Alberta Development of Runoff Depth Map for Alberta Introduction Assessment of basin runoff potential is an important component of the Hydrotechnical Design Guidelines for highway projects interacting with streams.

More information

OTHA Omaha Tools for Hydrologic Analysis - Time-Series/Statistical Analysis Programs for Water Resources

OTHA Omaha Tools for Hydrologic Analysis - Time-Series/Statistical Analysis Programs for Water Resources Hydrology Days 004 OTHA Omaha Tools for Hydrologic Analysis - Time-Series/Statistical Analysis Programs for Water Resources William Doan, P.E. Hydraulic Engineer, U.S. Army Corps of Engineers, Omaha District,

More information

Question 1: How does variation in the amount of remaining organic matter following fire affect permafrost temperature?

Question 1: How does variation in the amount of remaining organic matter following fire affect permafrost temperature? characteristics modulate both climate change disturbances to permafrost, and the ecological and hydrological outcomes of changing permafrost Question 1: How does variation in the amount of remaining organic

More information

Chapter 1 Introduction

Chapter 1 Introduction Engineering Hydrology Chapter 1 Introduction 2016-2017 Hydrologic Cycle Hydrologic Cycle Processes Processes Precipitation Atmospheric water Evaporation Infiltration Surface Runoff Land Surface Soil water

More information

Rainfall - runoff: Unit Hydrograph. Manuel Gómez Valentín E.T.S. Ing. Caminos, Canales y Puertos de Barcelona

Rainfall - runoff: Unit Hydrograph. Manuel Gómez Valentín E.T.S. Ing. Caminos, Canales y Puertos de Barcelona Rainfall - runoff: Unit Hydrograph Manuel Gómez Valentín E.T.S. ng. Caminos, Canales y Puertos de Barcelona Options in many commercial codes,, HMS and others HMS Menu Transform method, User specified,

More information

SECTION IV WATERSHED TECHNICAL ANALYSIS

SECTION IV WATERSHED TECHNICAL ANALYSIS A. Watershed Modeling SECTION IV WATERSHED TECHNICAL ANALYSIS An initial step in the preparation of this stormwater management plan was the selection of a stormwater simulation model to be utilized. It

More information

SURFACE-RUNOFF CHARACTERISTICS UNDER SIMULATED RAINFALL CONDITIONS ABSTRACT

SURFACE-RUNOFF CHARACTERISTICS UNDER SIMULATED RAINFALL CONDITIONS ABSTRACT Progress. Agric. 24(1 & 2): 219 227, 2013 ISSN 1017-8139 SURFACE-RUNOFF CHARACTERISTICS UNDER SIMULATED RAINFALL CONDITIONS P. Das 1, K. Mahmud 2* and S. Karmaker 1 Department of Irrigation and Water Management,

More information

Monitoring and Data Collection

Monitoring and Data Collection Setting the Course for Improved Water Quality Monitoring and Data Collection A TMDL training program for local government leaders and other water resource managers Session 8 wq-iw3-58 Your project to date

More information

River Processes River action (fluvial)

River Processes River action (fluvial) River action (fluvial) is probably the single most important geomorphic agent and their influence in geomorphology can hardly be overestimated. 1 To understand the complexity associated with river flow

More information

COE Flood Control. Design and development of enhancements to support modeling of COE flood control releases in RiverWare

COE Flood Control. Design and development of enhancements to support modeling of COE flood control releases in RiverWare COE Flood Control Design and development of enhancements to support modeling of COE flood control releases in RiverWare Edie Zagona Steve Setzer Neil Wilson Nancy Hall CADSWES Objective of flood control

More information

U.S. Geological Survey Streamflow data in Michigan Using the USGS NWIS database MDOT Bridge Scour Conference October 5, 2017

U.S. Geological Survey Streamflow data in Michigan Using the USGS NWIS database MDOT Bridge Scour Conference October 5, 2017 U.S. Geological Survey Streamflow data in Michigan Using the USGS NWIS database MDOT Bridge Scour Conference October 5, 2017 Tom Weaver Eastern Hydrologic Data Chief Upper Midwest Water Science Center

More information

Estimation of Channel Discharges under Complete Ice Cover

Estimation of Channel Discharges under Complete Ice Cover CGU HS Committee on River Ice Processes and the Environment 16th Workshop on the Hydraulics of Ice Covered Rivers Winnipeg, September 18-22, 201 Estimation of Channel Discharges under Complete Ice Cover

More information

Modeling Using Exponential Functions

Modeling Using Exponential Functions People, Tea, and.3 Carbon Dioxide Modeling Using Exponential Functions LEARNING GOALS In this lesson, you will: Write exponential models from data sets. Use models to solve problems. It can be amazing

More information

Characterization of Stream Flow in South Florida Application to Managing Flow in Artificial Tributaries

Characterization of Stream Flow in South Florida Application to Managing Flow in Artificial Tributaries Characterization of Stream Flow in South Florida Application to Managing Flow in Artificial Tributaries Richard Alleman Florida Bay and Adjacent Marine Systems Conference December 9, 28 Historical Tributaries

More information

Runoff Processes. Daene C. McKinney

Runoff Processes. Daene C. McKinney CE 374 K Hydrology Runoff Processes Daene C. McKinney Watershed Watershed Area draining to a stream Streamflow generated by water entering surface channels Affected by Physical, vegetative, and climatic

More information

Analysis of Flood Routing

Analysis of Flood Routing Dhaka Univ. J. Sci. 6(): 69-73, 014 (July) Analysis of Flood Routing Md. Motaleb Hossain Department of Mathematics, Dhaka University, Dhaka 1000, Bangladesh (Received: 6 May 01; Accepted: 4 May 014) Abstract

More information

Norman Maclean Snowmelt Flow rate Storm flows fs (c flow m a tre S

Norman Maclean Snowmelt Flow rate Storm flows fs (c flow m a tre S Eventually, all things merge into one, and a river runs through it. Norman Maclean Understanding Streamflow ADEQ SW Short Course June 13, 213 Phoenix, AZ Hydrographs Discharge (Q) USGS flow data & plots

More information

Adapting to the Weather: Lessons from U.S. History. December 31, Abstract

Adapting to the Weather: Lessons from U.S. History. December 31, Abstract Adapting to the Weather: Lessons from U.S. History Hoyt Bleakley Sok Chul Hong December 31, 2009 Abstract An important unknown in understanding the impact of climate change is the scope for adaptation,

More information

Basic Hydrology Runoff Curve Numbers

Basic Hydrology Runoff Curve Numbers Basic Hydrology Runoff Curve Numbers By: Paul Schiariti, P.E., CPESC Mercer County Soil Conservation District The SCS Runoff Curve Number The RCN (Runoff Curve Number) method was originally established

More information

Hydrology and Water Resources Engineering

Hydrology and Water Resources Engineering Hydrology and Water Resources Engineering SUB GSttingen 214 868 613 K.C. Patra 't'v Mai Narosa Publishing House New Delhi Chennai Mumbai Calcutta CONTENTS Preface vii 1. Introduction 1 1.1 General 1 1.2

More information

Lights Light Up Your Life Data Sheet

Lights Light Up Your Life Data Sheet Lights Light Up Your Life Data Sheet NAME: Purpose: Compare CFL to incandescent lightbulbs Research: Read and record facts from outside experts about the differences between the two types of bulbs. Compare

More information

ANALYZING THE EFFECTS OF THE SALUDA DAM ON THE SURFACE- WATER HYDROLOGY OF THE CONGAREE NATIONAL PARK FLOODPLAIN, SOUTH CAROLINA

ANALYZING THE EFFECTS OF THE SALUDA DAM ON THE SURFACE- WATER HYDROLOGY OF THE CONGAREE NATIONAL PARK FLOODPLAIN, SOUTH CAROLINA ANALYZING THE EFFECTS OF THE SALUDA DAM ON THE SURFACE- WATER HYDROLOGY OF THE CONGAREE NATIONAL PARK FLOODPLAIN, SOUTH CAROLINA Paul A. Conrads 1, Toby D. Feaster 2, and Larry G. Harrelson 3 AUTHORS:

More information

HYDROLOGICAL IMPACTS OF URBANIZATION: WHITE ROCK CREEK, DALLAS TEXAS. Julie Anne Groening Vicars, B.A. Thesis Prepared for the Degree of

HYDROLOGICAL IMPACTS OF URBANIZATION: WHITE ROCK CREEK, DALLAS TEXAS. Julie Anne Groening Vicars, B.A. Thesis Prepared for the Degree of HYDROLOGICAL IMPACTS OF URBANIZATION: WHITE ROCK CREEK, DALLAS TEXAS Julie Anne Groening Vicars, B.A. Thesis Prepared for the Degree of MASTER OF SCIENCE UNIVERSITY OF NORTH TEXAS December 25 APPROVED:

More information

FLUID MECHANICS CIVIL ENGINEERING VIRTUAL LABORATORY

FLUID MECHANICS CIVIL ENGINEERING VIRTUAL LABORATORY FLUID MECHANICS CIVIL ENGINEERING VIRTUAL LABORATORY EXPERIMENT: 2 VENTURI METER INTRODUCTION: The Ventura meter used in this experiment consists of successive converging, uniform and diverging sections

More information

Construction. Analysis. Hydrographs

Construction. Analysis. Hydrographs Construction And Analysis Of Hydrographs Hydrographs Special graphs that show a changes in a river s discharge over a period of time, usually in relation to a rainfall event. River Discharge Is the amount

More information

Chapter 6. The Empirical version of the Rational Method

Chapter 6. The Empirical version of the Rational Method Chapter 6 The Empirical version of the Rational Method The Empirical version is named because the parameters it uses (apart from rainfall data) are arbitrary and are generally based on experience or observation

More information

THE RATIONAL METHOD FREQUENTLY USED, OFTEN MISUSED

THE RATIONAL METHOD FREQUENTLY USED, OFTEN MISUSED THE RATIONAL METHOD FREQUENTLY USED, OFTEN MISUSED Mark Pennington, Engineer, Pattle Delamore Partners Ltd, Tauranga ABSTRACT The Rational Method has been in use in some form or another at least since

More information

The critical information from this document has been included in the ARD Pipe Help system.

The critical information from this document has been included in the ARD Pipe Help system. Introduction This command is used to set the way is treated with respect to Pipe flow. There are three (3) methods, along with the ability to change the method on existing networks. flows have always been

More information

EMPIRICAL PROJECT 7 SUPPLY AND DEMAND

EMPIRICAL PROJECT 7 SUPPLY AND DEMAND EMPIRICAL PROJECT 7 SUPPLY AND DEMAND LEARNING OBJECTIVES In this project you will: convert values from natural logarithms to base 10 logarithms draw graphs based on equations give an economic interpretation

More information

I(n)Kn. A Qp = (PRF) --- (8) tp Where A is the watershed area in square miles and PRF is the unit hydrograph peak rate factor.

I(n)Kn. A Qp = (PRF) --- (8) tp Where A is the watershed area in square miles and PRF is the unit hydrograph peak rate factor. AN ALTERNATE APPROACH FOR ESTIMATING SCS UNIT HYDROGRAPH PEAK RATE FACTORS (PRFS) IN SOUTHWEST FLORIDA Himat Solanki Southwest Florida Water Management District 115 Corporation Way, Venice, Florida 34292

More information

A DESIGN FLOOD ESTIMATION PROCEDURE USING DATA GENERATION AND A DAILY WATER BALANCE MODEL

A DESIGN FLOOD ESTIMATION PROCEDURE USING DATA GENERATION AND A DAILY WATER BALANCE MODEL A DESIGN FLOOD ESTIMATION PROCEDURE USING DATA GENERATION AND A DAILY WATER BALANCE MODEL W. C. Boughton P. I. Hill Report 97/8 October 1997 Boughton, W.C. (Walter C.) A design flood estimation procedure

More information

2.2.1 Statistical methods (Frequency Analysis)

2.2.1 Statistical methods (Frequency Analysis) 2.' LITERATURE SURVEY 2.1 General Flood is considered as unusually high stage of the river. It is perhaps better described as that stage at which the stream channel gets filled and above which it overflows

More information

Rainfall, Runoff and Peak Flows: Calibration of Hydrologic Design Methods for the Kansas City Area

Rainfall, Runoff and Peak Flows: Calibration of Hydrologic Design Methods for the Kansas City Area Rainfall, Runoff and Peak Flows: Calibration of Hydrologic Design Methods for the Kansas City Area Bruce McEnroe, Bryan Young, Ricardo Gamarra and Ryan Pohl Department of Civil, Environmental, and Architectural

More information

Generalization of parameters in the storage discharge relation for a low flow based on the hydrological analysis of sensitivity

Generalization of parameters in the storage discharge relation for a low flow based on the hydrological analysis of sensitivity Proc. IAHS, 371, 69 73, 2015 doi:10.5194/piahs-371-69-2015 Author(s) 2015. CC Attribution 3.0 License. Generalization of parameters in the storage discharge relation for a low flow based on the hydrological

More information

Names: ESS 315. Lab #6, Floods and Runoff Part I Flood frequency

Names: ESS 315. Lab #6, Floods and Runoff Part I Flood frequency Names: ESS 315 Lab #6, Floods and Runoff Part I Flood frequency A flood is any relatively high flow of water over land that is not normally under water. Floods occur at streams and rivers but can also

More information

OFFICE OF STRUCTURES MANUAL ON HYDROLOGIC AND HYDRAULIC DESIGN CHAPTER 3 POLICY AND PROCEDURES

OFFICE OF STRUCTURES MANUAL ON HYDROLOGIC AND HYDRAULIC DESIGN CHAPTER 3 POLICY AND PROCEDURES OFFICE OF STRUCTURES MANUAL ON HYDROLOGIC AND HYDRAULIC DESIGN CHAPTER 3 POLICY AND PROCEDURES April 28, 2016 Table of Contents 3.1 Introduction... 2 3.1.1 Purpose of Chapter 3... 2 3.1.2 Policy vs. Design

More information

DENSITY of Solids and Liquids

DENSITY of Solids and Liquids Regents Earth Science Name: Date: Lab # DENSITY of Solids and Liquids Introduction: Density is the term used to describe the relationship between the mass of an object and its volume. Under given conditions

More information