CEE 3430, Engineering Hydrology David Tarboton. Overview Handouts –Syllabus –Schedule –Student Information Sheet –Homework 1 Web: https://usu.instructure.com/courses/392804https://usu.instructure.com/courses/392804.

Slides:



Advertisements
Similar presentations
1. Basic Hydrology Concept
Advertisements

Unit 1: Water Systems on Earth Chapter 1
Engineering Hydrology (ECIV 4323)
HYDROLOGY - BASIC CONCEPTS
OKLAHOMA STATE UNIVERSITY Biosystems and Agricultural Engineering Department Hydrology 101 OKLAHOMA STATE UNIVERSITY Biosystems and Agricultural Engineering.
U.S. Department of the Interior U.S. Geological Survey Lake Evaporation using Energy Budget Method: Walker Lake, NV - a case study In cooperation with.
Dr. Nicolas Zegre Understanding the Hydrologic Cycle.
Last time… Key questions 1.Why does air move? 2.Are movements of winds random across Earth’s surface, or do they follow regular patterns? 3.Implications.
One estimate of global water distribution Volume (1000 km 3 ) Percent of Total Water Percent of Fresh Water Oceans, Seas, & Bays1,338, Ice caps,
Chapter One Hydrologic Principles Flashlight and globe.
Engineering Hydrology (ECIV 4323)
Urban Hydrology and Water Budget Calculation Geog310 Urban Climatology.
Hydrologic Cycle/Water Balances. Earth’s Water Covers approximately 75% of the surface Volcanic emissions Only known substance that naturally exists as.
Jefferson High School Compton Creek Research Project UCLA and Los Angeles Waterkeeper Funded by the Environmental Protection Agency.
Water Systems Mrs. Bader. Water Systems In this exercise, you will learn more about what makes up a watershed, track the movement of water through the.
Unit 1: Water Systems on Earth Chapter 1
Grade 8 Science Unit 1: Water Systems on Earth Chapter 1
CE 394K.2 Hydrology – Lecture 1 Syllabus, term paper, sequence of topics Hydrology as a science and as a profession Hydrologic cycle and world water balance.
EEOS 350: Quantitative hydrogeology Lecture 2 Water balance.
Applying Methods for Assessing the Costs and Benefits of CCA 2 nd Regional Training Agenda, 30 September – 4 October 2013 Priyanka Dissanayake- Regional.
Physical Hydrology & Hydroclimatology (Multiscale Hydrology)
Hydrology Chia-Ming Fan Department of Harbor and River Engineering
The Water Cycle… from clouds to sea.. from sea to clouds…
Watershed Assessment and Diagnosis of Condition for August 20, 2007 Joe Magner and Greg Johnson MPCA.
GEO/ENV 315/GEO 514 Hydrogeology Class meets: Time: Mondays: 5:30 pm – 8:30 pm. Location: ESS 183 Office Hours: Wednesdays and Fridays 3:00 – 4:00 pm ESS.
These notes are provided to help you pay attention IN class. If I notice poor attendance, fewer notes will begin to appear on these pages 1.
CE 424 HYDROLOGY 1 Instructor: Dr. Saleh A. AlHassoun.
Hydrologic Equation Inflow = outflow +/- Changes in storage Equation is simple statement of mass conservation.
1. What is the water cycle? 2. What are sources of water on Earth? 3. How does ocean water move? 4. How do oceans affect the weather? 5. In what ways.
Engineering Hydrology (ECIV 4323)
“ All the rivers run into the sea; yet the sea is not full; unto the place from whence the rivers come, thither they return again. ” Ecclesiastes 1:7.
Higher Hydrosphere Drainage Basins[Date] Today I will: - Know what a drainage basin is - Be able to explain it in terms of inputs, processes or outputs.
INTRODUCTION HYDROLOGY AND WATER RESOURCES HYDROLOGY AND WATER RESOURCES RG744 INSTITUTE OF SPACE TECHNOLOGY SEPTEMBER 09, 2015.
AOM 4643 Principles and Issues in Environmental Hydrology.
CE 374K Hydrology – Lecture 1 Syllabus, sequence of topics Hydrology as a science and as a profession Hydrologic cycle and world water balance Water as.
AIM: How the “spheres” interact: The Water Cycle
The Hydrological Cycle
© 2016 Cengage Learning. All Rights Reserved. 7 Oceanography, An Invitation to Marine Science | 9e Tom Garrison Ocean Chemistry.
ENERGY AND THE WATER CYCLE (NASA Animation) 2 AIM: HOW THE “SPHERES” INTERACT: THE WATER CYCLE.
Chapter 21 Water Supply, Use and Management. Groundwater and Streams Groundwater –Water found below the Earth’s surface, within the zone of saturation,
CE 3354 Engineering Hydrology Lecture 2: Surface and Groundwater Hydrologic Systems.
© 2014 Pearson Education, Inc. Chapter 5 Water and Seawater Salinity.
Sanitary Engineering Lecture 4
C.K.PITHAWALA COLLEGE OF ENGINEERING AND TECHNOLOGY.
CEE 3430, Engineering Hydrology David Tarboton (Richard Peralta today)
CEE 3430, Engineering Hydrology David Tarboton
What makes the Great Salt Lake level go up and down ?
Integrated Water Science in the Great Salt Lake Basin
CEE6400 Physical Hydrology
Fresh Water Sustainable Use.
Precipitation-Runoff Modeling System (PRMS)
Unit 1: Water Systems on Earth Chapter 1
Engineering Hydrology
Basic Hydrology & Hydraulics: DES 601
Engineering Hydrology (ECIV 4323)
CEE 3430, Engineering Hydrology David Tarboton
Salinity, Evaporation and the Rise and Fall of the Great Salt Lake
CE 394K.2 Hydrology – Lecture 1
Hydrologic Losses - Evaporation
Water on Earth.
Grade 8 Science Unit 1: Water Systems on Earth Chapter 1.
Unit 1: Water Systems on Earth
INTRODUCTION TO HYDROLOGY
Water on Earth.
Hydrology CIVL341.
Running Water and Groundwater
Engineering Hydrology (ECIV 4323)
1. Engineering Hydrology by H.M. Raghunath
Hydrology CIVL341 Introduction
Engineering Hydrology (ECIV 4323)
Presentation transcript:

CEE 3430, Engineering Hydrology David Tarboton

Overview Handouts –Syllabus –Schedule –Student Information Sheet –Homework 1 Web: Outline for today –Review Syllabus and Schedule –Introduce the Hydrologic Cycle and Water Balance Concepts (Great Salt Lake Example)

Texts Ground and Surface Water Hydrology, by Mays, 2011 (Chapters 1-4 and 7-9) Either full text ($189) or Custom book with just these chapters ($55) HEC-HMS Manual (last part of class only) /hec-hms/documentation.aspx /hec-hms/documentation.aspx HydroViz Logan Dry Canyon Flash Flood Protection Module

Course Learning Objective Upon successful completion of the course you should be able to apply the principles of hydrology to solve engineering hydrology design problems involving hydrologic modeling and analysis.

What is Hydrology? A science dealing with the properties, distribution and circulation of water. Engineering Hydrology involves the application of the knowledge of hydrologic science for practical uses, the solution of engineering problems and the betterment of mankind. The availability of water to sustain life is perhaps the most recurrent constraint in human history and will remain so in the foreseeable future.

From

Engineering Hydrology and Hydrologic Science in the hierarchy from basic sciences to water resources management Basic Sciences Mathematics Statistics Physics Chemistry Biology Geosciences Geology Soil Science Atmospheric Science Ocean Science Glaciology Geochemistry – Fluid Mechanics Hydraulic Engineering Meteorology Hydrologic Science Economics Law Sociology Political Science Engineering Hydrology Agriculture Forestry Water Resources Management Modified From: National Research Council Committee on Opportunities in the Hydrologic Sciences (COHS), (1991), Opportunities in the Hydrologic Sciences, Editor, P. S. Eagleson, National Academy Press, Washington, D.C.

The Hydrologic Cycle P Runoff Evap ET Evap Streams Lake Reservoir GW Atmospheric Moisture Snow melt Figure 1-1 from Bedient:

Atmospheric Water Soil WaterSurface Water Groundwater Water Balance Change of Storage Inflow – Outflow =

Great Salt Lake Evaporation The Great Salt Lake has an average inflow from streamflow of 2,316,220 acre ft / year The area is about 1 million acres Average annual precipitation on the lake is about 10 inches/year It is a closed basin with no outflows other than evaporation Assuming the level is not changing what is the average annual evaporation ?

Area, A Level Inflows I E x A Evaporation depth E Evaporation volume E x A

More Effects of Management Change A lower level has implications for –Brine shrimp –Bird habitat –Boating and other users A more comprehensive analysis has to consider additional factors –Climate variability and lake fluctuations –Salinity. A lower lake has smaller volume, but the amount of salt is the same (apart from what the mineral co. is taking), so the salinity is more. This reduced evaporation –Evaporation ponds actually occupy part of the lake –The railway causeway splits the lake into two water bodies with different levels

Area, A E x A How a closed basin (e.g. GSL works) Level Inflows I I E x A If I > E x A level rises If I < E x A level falls Level adjusts to fluctuating inputs so that on average I = E x A I includes inflows from streams and precipitation on the lake I = Q + P x A Subject to climate variability. E is less variable, but also depends on climate and salinity, C. As C increases E decreases Evaporation depth E Evaporation volume E x A Volume, V Salt Load L Salt Concentration C=L/V

Concepts Discussed Fundamental equation in hydrology - mass balance (eqn 1.5.1) Expressing quantities in units that are easier to interpret, such as depth for evaporation rather than volume Equilibrium or steady-state assumption

Summary The engineering hydrologist must be able to calculate or estimate various components of the hydrologic cycle to solve hydrologic problems –Drainage design, flood protection, water supply The concept of the water balance is fundamental to much hydrologic analysis Become comfortable converting units and working with “incompatible” units, it is an unfortunate fact of life