James River in Richmond, Virginia looking upriver from the Robert E. Lee bridge. Belle Isle is on the right, November 1985. 1. What is happening in this.

Slides:



Advertisements
Similar presentations
RIVER DRAINAGE BASINS.
Advertisements

Analysis of Hydrographs
Factors that affect flood risk…
The Causes,Effects and Management of Flooding in Loughton
Flash Floods 6 th Grade. FLASH FLOODS Flash Flood: #1 weather- related killer in the United States!
CHARACTERISTICS OF RUNOFF
CE 515 Railroad Engineering
OKLAHOMA STATE UNIVERSITY Biosystems and Agricultural Engineering Department Hydrology 101 OKLAHOMA STATE UNIVERSITY Biosystems and Agricultural Engineering.
Hydrograph Interpretation.
Hydrology: Discharge, Hydrographs, Floods, and Sediment Transport Unit 1: Module 4, Lecture 2.
River Hydrographs Why do we use hydrographs?
Construction And Analysis Of Hydrographs. Hydrograph Record of River Discharge over a period of time River Discharge = cross sectional area rivers mean.
Analysis of Hydrographs
Earth’s six water reservoirs Reservoir% Earth's Water% Usable Water Oceans97.54%----- Glaciers2.15%----- Shallow Groundwater0.31%96.9% Fresh Lakes/Streams0.009%2.8%
Watershed and its divide What’s the situation at points A and B in terms of: a. gradient b. stream velocity c. erosive power? Headwaters.
Construction Analysis Hydrographs
The Hydrologic (Water) Cycle. Surface Water Oceans Rivers and streams Lakes and ponds Springs – groundwater becomes surface water.
Water and Floods. Groundwater and Floods The Hydrologic Cycle & Earth’s water Drainage systems — Drainage basins & Rivers Floodplains and levees Floods.
Storm Hydrographs Yr12IB Drainage Basins.
FLOOD HYDROGRAPHS FOR GCSE GEOGRAPHY.
Copyright [insert date set by system] by [CH2M HILL entity] Company Confidential Hydrologic Evaluation of the Little Thompson River Phase 2: Little Thompson.
Alluvial Fan 8-7 Delta.
Flood hydrographsHydrosphere. Flood hydrographs show the effect that precipitation has on the water levels in a river. After a storm the water levels.
Construction And Analysis Of Hydrographs Hours from start of rain storm Discharge (m 3 /s) Base flow Through flow Overland.
Construction And Analysis of Hydrographs ©Microsoft Word clipart.
Principles of Flash Flood Development: An Introduction to Hydrometeorology Anthony Phillips GEOG 490/590 Ball State University  Hazards associated with.
RIVER PROCESSES Introduction to Watershed Science Merritt College Marc Epstein, Instructor.
Exeter 8/12/00.
Matthew Kelsch NWA Annual Meeting,18 October 2006 Hydrometeorological Training: What Makes a Flood a Flash Flood? Matt Kelsch UCAR/COMET ®
Flooding New Orleans, Aug Flooding –Varies with intensity and amount of rainfall –Perhaps the most universally experienced natural hazard Flood.
© 2012 Pearson Education, Inc. Lecture Presentation Chapter 6 Flooding.
Floods Week 4. Questions for Homework & Discussion  Would you live in a flood-prone area?)  What level of risk from flooding is acceptable to you? 
Streams and Flooding Chapter 6  Water shapes the earth’s surface  Water also plays a role in human affairs  Floods are the most widely experienced catastrophic.
Streams and Flooding Chapter 6 Water shapes the earth’s surface
Chapter 11 – WATER ON THE GROUND
RIVER DRAINAGE BASINS. A RIVER SYSTEM ACTS LIKE A SYSTEM OF DOWNPIPES AND GUTTERING ON A HOUSE - IT ALLOWS THE MOVEMENT OF RAINWATER INTO THE SEA.
Construction And Analysis of Hydrographs ©Microsoft Word clipart Ballakermeen High School.
FLOODS.
Hydrologic Hazards at the Earth’s Surface
Fluvial Geomorphology GRG 338-C Streamflow (Discharge)
WATER ON AND UNDER GROUND. Objectives Define and describe the hydrologic cycle. Identify the basic characteristics of streams. Define drainage basin.
The July 28,1997 Fort Collins Flood: Putting the Stormwater System to the Test How Did it Serve to Minimize Societal Impact? Matt Kelsch Hydrometeorologist.
Hazards, Vulnerability, and Mitigation Sub-Committee.
Living with Streams in Flood
Harrisburg Flood Inundation Mapping Project – Many Agencies Working Together USACE Flood Risk Management and Silver Jackets Workshop 23 August 2012 Presented.
Surface Water Surface runoff - Precipitation or snowmelt which moves across the land surface ultimately channelizing into streams or rivers or discharging.
Hydrograph Analysis. Components of river flow Contributions into a river/stream Overland flow – Flow over land surface due to precipitation (runoff)
MAINE DEPARTMENT OF ENVIRONMENTAL PROTECTION MAINE DEPARTMENT OF ENVIRONMENTAL PROTECTION Protecting Maine’s Air, Land and Water MAINE.
Sanitary Engineering Lecture 4
A RIVER SYSTEM ACTS LIKE A SYSTEM OF DOWNPIPES AND GUTTERING ON A HOUSE - IT ALLOWS THE MOVEMENT OF RAINWATER INTO THE SEA.
Nicolson Institute - Geography Department The objectives of this PowerPoint presentation and the accompanying work sheet are to - introduce storm hydrographs.
HYDROGRAPHS: CONSTRUCTION AND ANALYSIS 01/10/2016.
HYDROLOGY Lecture 10 Unit Hydrograph
Flood Hydrographs How do we know if a river will flood?
Analysis of Hydrographs
Construction Analysis Hydrographs
Why do people try to manage rivers?.
HIGHER GEOGRAPHY Hydrosphere - Hydrographs.
Analysis of Hydrographs
Brian McInerney Hydrologist National Weather Service
Flood Frequency Analysis
Streams Hydrodynamics
Floods and Flood Routing
Weekly lesson objectives
Analysis of Hydrographs
Analysis of Hydrographs
Definition of Floods Flood: Overflows of large amounts of water onto land that is normally dry. Coastal flood: Happens near a coast River flood: River.
Chapter 6 Flooding.
Today we are learning this content:
Presentation transcript:

James River in Richmond, Virginia looking upriver from the Robert E. Lee bridge. Belle Isle is on the right, November What is happening in this picture? 2. What makes the water so brown?

James River in Richmond, Virginia. The Robert E. Lee bridge and the bridge in the previous photo are in the background. 3. Estimate the height of the river during the flood shown in the previous image. 4. How could we obtain or estimate past flooding? 5. How can we predict the future flood potential?

Potholes along the James River at Belle Isle, the same location as previous images. 6. Describe the shape of the bedrock river channel. 7. How were those holes formed?

Presidential disaster declarations related to flooding in the United States, shown by county, between June 1, 1965, and June 1, 2003 Green: 1 declaration Yellow: 2 declarations Orange: 3 declarations Red: ≥4 declarations Map not to scale. Sources: FEMA, Michael Baker Jr., Inc., the National Atlas, and the USGS Floods are common and costly natural disasters

Hurricane Katrina - largely from flood [rain and storm surge] damage $$105 Billion Floods are common and costly natural disasters

Drainage Basin

Flood plains normally are dry Meandering river carve out the flood plain

Map of real-time streamflow compared to historical streamflow for the day of the year

Q = A X V Stream Discharge (Q) Hydrograph Lag time

Weather patterns can determine when floods occur

steep topography + intense rain = short lag time = “Upstream” (flash flood) flood 7.5 inches of rain in 70 minutes  flood water velocity of 23 ft/sec The Big Thompson Canyon flood killed 145 people, destroyed 418 houses and damaged another 138, destroyed 152 businesses and caused more than $40 million in damages. August 1,

Streamflow in Mercer Creek, an urban stream in western Washington, increases more quickly, reaches a higher peak discharge, and has a larger volume during a one-day storm on February 1, 2000, than streamflow in Newaukum Creek, a nearby rural stream. Streamflow during the following week, however, was greater in Newaukum Creek. Affect of Urbanization on Flooding What is it about urbanization that is problematic?

What parameters influence flooding? Weather patterns – precipitation, snow melt Topography (steep or flat) Properties of the soil (porous and permeable) Land use (impervious covers, channalization) All come down to: surface runoff >> infiltration  increase flood potential

The extrapolations of recurrence intervals are used to forecast the future probability of a flood of a given discharge. The probability (P) of an flood with recurrence interval T is P = 1/T “The 100 year flood” A flood discharge that has a 100-year recurrence interval has a 1% chance of occurring or being exceeded in a given year. Very large floods happen very seldom Flood Frequency Diagram

The stage of such a flood can be back-calculated using the rating curve for the river. Once the stage is known, a topographic map can be consulted to examine inundation

Wetlands (veg.) can reduce floods Retention ponds can reduce floods

Zoning restrictions limit flood damage Dams and levees can reduce the risk of floods Floodwalls along Willow Creek in Rosemont, Illinois. Source: Kevin D. Richards, U.S. Geological Survey.

A map from the U.S. Army Corps of Engineers sets out areas of flooding in New Orleans following Katrina, Sept. 2.

Levees (and channalization) can constrict a river, increasing flow velocities and causing flooding upstream and downstream