Introductions – Stream Ecology (NR 280) Welcome! The Syllabus Blackboard content Labs/Field Trips Hurricane Irene What next?

Slides:

Advertisements

Similar presentations

Dam Control of Flow Rates on the Scioto and Olentangy Rivers 1.

Advertisements

Flooding Case Study - Boscastle

Y A S O O B A L I b o r n o n 1 9 t h F e b r u a r y i n K a n p u r d i s t r i c t o f U t t a r P r a d e s h. H e s t a r t e d s i n g i.

Flash Floods 6 th Grade. FLASH FLOODS Flash Flood: #1 weather- related killer in the United States!

Hydrograph Interpretation.

Stephen Swan CE 394K 2 April 22,  Project Background  Dallas and the Trinity River  Flood of 1908  Current Flood Control Measures  Initial.

Start Audio Lecture! FOR462: Watershed Science & Management 1 Streamflow Analysis Module 8.7.

FLOODS, STREAMS AND MEANDERS. GAUGING STATION On all major streams Measures Stream Height Height vs. Discharge (volume) Flood Stage and height above Flood.

Geomorphic Effects of Dams on Rivers Gordon Grant.

The Damming of the Winooski River Watershed. An Historic Look at the Damming of the Winooski River Watershed. Winooski River Watershed. Waterbury Dam,

Reading: Applied Hydrology Sections 8.1, 8.2, 8.4

1 Water Quality: Temperature How is water quality affected by temperature?

FLOOD HYDROGRAPHS FOR GCSE GEOGRAPHY.

The three main courses of Yangtze river Facts about the Yangtze river Length 3,964 miles Source Qinghai-Tibet Plateau, China Mouth East China.

KINEROS (KINematic runoff and EROSion model) Michael Schaffner Senior Service Hydrologist NOAA National Weather Service WFO Binghamton, NY Eastern Region.

Ch. 21-1: North Africa and Southwest Asia

WFM 5201: Data Management and Statistical Analysis © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM 5201: Data Management and Statistical Analysis Akm Saiful.

Recent Storm Activity and its Effect on Turbidity Levels in Neversink Reservoir Rich Van Dreason Watershed Water Quality Science and Research New York.

Principles of Flash Flood Development: An Introduction to Hydrometeorology Anthony Phillips GEOG 490/590 Ball State University  Hazards associated with.

Climate: Outlook and Operational Planning Jayantha Obeysekera (’Obey’), Ph.D.,P.E.,D.WRE Department Director Hydrologic & Environmental Systems Modeling.

SITES SOFTWARE APPLICATION SEMINAR __________________________ SITES INTEGRATED DEVELOPMENT ENVIRONMENT for WATER RESOURCE SITE ANALYSIS 5 Point.

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.

Channel Flow Routing Reading: Applied Hydrology Sections 8.4, , 9.7.

Chapter 4: Weathering and Erosion

Stream Order 4.12.A. Physical Methods Stream order is a measure of the relative size of streams. Range from smallest, first- order, to the largest, the.

Libby Dam June 2006 Spill: Total Dissolved Gas Monitoring.

1.Look at the pieces of the picture. 2.Can you guess what is in the picture?

Fluvial Geomorphology GRG 338-C Streamflow (Discharge)

Rivers and Streams. What is the continental divide?

THE CATASTROPHE AFTER IRENE’S EXIT RECORD-TO-NEAR-RECORD FLOODING IN NEW ENGLAND AND CANADA IS STILL HAPPENING AUGUST 29---?, 2011 Dr. Walter Hays, Global.

Spokane River Basin Monitoring. Spokane Basin Monitoring.

Floods: “Rain Rain, go away”!! Brooke Porter Science 1st Mr. Shepard.

Lower Putah Creek Community Watershed Management.

Looking upstream from the Main Street Bridge: left to right, top: June 2004 (plant dominated reach following a dry winter), June 2005 (algal takeoff after.

Hydrology of Inland Flooding  Stream Gauges  Hydrologic Forecast Process  Forecast Considerations  Forecast Hydrographs 3-1.

BY RHIANNON AND RACHAEL. An eruption of hot volcanic ash rose 80,000 feet (24,400m) into the sky. At the same time, ice, snow and several glaciers which.

2008 FLOODS IN ARKANSAS 2008 FLOODS IN ARKANSAS August 13 – 14, 2009 Jaysson Funkhouser SEVERE.

Public Meeting April 2, 2015 Albany Park Stormwater Diversion Tunnel.

(b)Study Figure 2 which is an extract from a news website about the cause of floods in Pakistan in August With the help of Figure 2 explain why.

Hurricane Irene in Connecticut River Milena Spirova CE 394 K 2015.

Investigation 3 Go with the Flow. The Grand Canyon is one place where erosion has taken place on a grand scale. Geologists are still trying to figure.

A RIVER SYSTEM ACTS LIKE A SYSTEM OF DOWNPIPES AND GUTTERING ON A HOUSE - IT ALLOWS THE MOVEMENT OF RAINWATER INTO THE SEA.

Aquatic Biomes. Determined by Salt content Flow rate Size (sometimes) 2 major categories of aquatic biomes: Salt water system Freshwater.

Lesson 2 – page 1.  To learn what is a flood hydrograph  To learn how to read a flood hydrograph  To learn what is:  Lag time  Peak discharge  Rising.

Chs : Africa Chs : SW Asia. Chs : SW Asia and North Africa.

Massachusetts Bay Physical Processes 2011 compared to 2012

Hurricane Matthew Anatomy of a Flood

Parvathy Sankara Raman

Storm Hydrographs Storm hydrographs are used to measure a river’s flow and show the change in river discharge over a short period of time after a storm.

Walker River Irrigation District

River Conwy - hydrographs

The issue: A Damming report – why are some strategies for flood management more sustainable than others?

Elizabeth Stanley Mann Meghan Kirsch

Flash Flood Video arizona-desert/

Highland Lake Reservoir System

Comparing NFIE RAPID models with measured river flood hydrographs.

Welcome to an Introduction to Technology at Illinois State University!

Hydrographs River Discharge = cross sectional area X

Hydrologic Engineering

The Flow of Water.

ES Waterfall Bridge.

Carlisle Flood: 2005 Why has this area flooded? List all the reasons you can think of.

Introduction to settlements

Presentation transcript:

Introductions – Stream Ecology (NR 280) Welcome! The Syllabus Blackboard content Labs/Field Trips Hurricane Irene What next?

Last 7 Days Winooski River at Essex Junction

Last 120 Days Winooski River at Essex Junction

Peak flow 08/29/ :15 EDT 38,900 cfs Peak flow for Winooski River at Montpelier 08/28/ :30 EDT 14,600 cfs Annual Peak Flows from 1927

Last 7 Days Little River near Waterbury

VTrans Traveler Warnings – Critical Issues

NBC story on flooding in Vemont Flow over IBM dam Videos from 29 August 2011 (~12-18h after peak rainfall from Hurricane Irene but only a few hours before peak discharge. Flow below Rt 15 bridge east of Essex Junction Flow at Cascades in Winooski Flow at Winooski River mouth – scan from bank to bank Eddy at Winooski River mouth – true left bank Floating tree at Winooski River mouth Effects of Hurricane Irene Images for Winooski River tour, mid-day 29 August 2011

Introductions – Stream Ecology (NR 280) Welcome! The Syllabus Blackboard content Labs/Field Trips Hurricane Irene What next?