River and Costal Floods 1- River Floods The basic cause of river flooding is the incidence of heavy rainfall.

Slides:



Advertisements
Similar presentations
Characteristics of High Gradient Streams
Advertisements

Thomas Kjeldsen, Michael Hilden, and many others Henk Wolters
A flood occurs... Any time a body of water rises to cover what is usually dry land.
Terrestrial Environments Around the World
 There are two types of Rainforest tropical and temperate. Tropical are found close to the equator. Temperate are found along coasts in the temperate.
Section 3: Stream Deposition
Ch  Know what design frequency means  Know how to delineate a drainage area on a topographic map 2.
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%
Chapter 6 Section 1 – Running Water
URBAN FLOODS IN GREECE Current situation and major research and development needs in Urban Flood Management Cost meeting, Warsaw, 29-31/5/2008 Vassilopoulos.
Use of Water resources Hydraulic Engineering Subjects in teaching.
WATERSHED MANAGEMENT IN JAMAICA. Background Location and Size The island is located in the north-western Caribbean Sea, it is the third largest of the.
The Hydrologic (Water) Cycle. Surface Water Oceans Rivers and streams Lakes and ponds Springs – groundwater becomes surface water.
Chapter 6.2 The Work of Streams.
Where is the WATER? By: Chelsy Bird & Kayla Melfi.
Bangladesh: Basic Facts Presented by: Syed Amdadul Huq Research Director (a.i.), FPMU 22/02/10 Presentation to Cambodian Food Security Team.
Floods Defined: any time a body of water rises to cover what is usually dry land Are one of most common hazards –75% of Federally declared disasters May.
Floods CERT Basic Training Hazards. When Floods Occur ●Any time a body of water rises to cover what is usually dry land ●One of most common hazards 
Floods.
FLOOD HYDROGRAPHS FOR GCSE GEOGRAPHY.
FNR 402 – Forest Watershed Management
CLIMATE CHANGE SILKE, VIKTORIA, JOSEFINE AND ANKE.
1 Flood Hazard Analysis Session 1 Dr. Heiko Apel Risk Analysis Flood Hazard Assessment.
CARIBBEAN STUDIES Hazards in the Caribbean. Earthquakes Earthquakes are caused by sudden release of slowly accumulated strain energy along a fault in.
Abstract Abstract. Flash-flood disasters are very rare in the Transylvanian Depression. During the last decade (i.e period), the occurrence.
Hydro-Electric Power Station Lecture No: 4. “”A generating station which utilizes the potential energy of water at a high level for the generation of.
Floods School: Abdallah Al-Alayly Teacher: Ms. Abeer Abdallah Prepared by: Grade 9 students.
FRESHWATER COULTER. RIVER SYSTEMS: TRIBUTARIES RIVERS OFTEN BEGIN IN THE MOUNTAINS, WHERE RUNOFFS FROM MELTING SNOW FORMS SMALL STREAMS. AS YOU FOLLOW.
A. Hydrologic cycle A. Hydrologic cycle o The hydrologic cycle is a summary of the circulation of Earth’s water supply o Processes involved in the hydrologic.
1/38 Urban Flood & Climate Change ----information from APWMF and SIWW Jinping LIU Hydrologist Typhoon Committee Secretariat.
Unit 3 – Gradational Processes.  Stability is determined by the relationship between the driving and resisting forces.  Driving forces – move earth.
Effect of Land Clearance or Land "Reclamation" Infrastructural project: build a air station WYS.
 This will occur when streams receive more water than their channels can hold,  i.e. when stream discharge is greater than stream capacity.  Streams.
Stream Erosion and Transport
Rick Cruse, Matt Helmers, Greg Brenneman, and John Laflen Iowa Water Center, and Iowa State University Extension.
Landform Geography Landforms of the Fluvial System.
A. Hydrologic cycle o The hydrologic cycle is a summary of the circulation of Earth’s water supply o Processes involved in the hydrologic cycle o Precipitation.
FLOODS.
Watershed Plan for Heredia, Costa Rica Whitney Thomas, Matthew O’Malley, William Brown Biological Systems Engineering, Virginia Tech Rio Tibas Watershed.
SEVERE FLOODING IN THE MIDDLE EAST LEBANON JANUARY 4, 2013 Walter Hays, Global Alliance for Disaster Reduction, Vienna, Virginia, USA.
Warmup How many river basins are in North Carolina? Which two river basins border Apex? Write two facts about your river basin from Friday.
Flooding How does flooding relate to weathering, erosion, and deposition?
Section 3: Stream Deposition
Assessment of Vulnerability on the Aral See Basin NATALYA AGALTSEVA Research Hydrometeorological institute (NIGMI) Uzhydromet Uzbekistan.
Journal #5 What is a flood? Why are floods harmful? What can humans do to prevent floods?
© 2007, John Wiley and Sons, Inc. Physical Geography by Alan Arbogast Chapter 16 Fluvial Systems and Landforms Lawrence McGlinn Department of Geography.
Land and Water in Your Area. The surface features of a place. geography.
Suwannee-Satilla Drainage Basin: Flood Control Issues and Requested Action Suwannee-Satilla Regional Water Planning Council Douglas, GA December 8, 2010.
FLOODS IN GHANA June 5, 2015 Walter Hays, Global Alliance for Disaster Reduction, Vienna, Virginia, USA Walter Hays, Global Alliance for Disaster Reduction,
FLOODS IN REPUBLIC OF GEORGIA June 13-15, 2015 Walter Hays, Global Alliance for Disaster Reduction, Vienna, Virginia, USA Walter Hays, Global Alliance.
SARDAR VALLABHBHAI PATEL INSTITUTE OF TECHNOLOGY, VASAD MADE BY:- AYUSHI R. DAVE ( ) BINAL S. PATEL( ) ANJALI H. RATHOD( )
CERT Basic Training Hazards Floods. Fl-1CERT Basic Training Unit 1: Floods ●Any time a body of water rises to cover what is usually dry land ●One of most.
BANGLADESH FLOOD 2K4. Causes of flood… 1.Monsoon climate brings very heavy rainfall and snow soils are leached and heavy runoff results in soil erosion.
Bhagwan Mahavir College of Engineering and technology Sub: HYDROLOGY AND WATER RESOURCE ENGINEERING Presentation On : Flood Subbmitted by: Trivedi Vinni.
Unit 3 - Hydrosphere Study Guide Answer Key.
FLOODS.
Highway Drainage-Hydrology
Ali Fares Associate Professor of Watershed Hydrology
2.3.2a Water Cycle, Surface Water, and Ground Water
15-3 Stream Deposition.
Severe Weather.
2.3.2a Water Cycle, Surface Water, and Ground Water
Any time a body of water rises to cover what is usually dry land.
Earth’s Fresh Water.
Earth and Space Science
CERT Basic Training Hazards
Warmup How many river basins are in North Carolina?
Hydrologic Engineering
Managing River Floods Natural Physical Causes of Floods
Presentation transcript:

River and Costal Floods 1- River Floods The basic cause of river flooding is the incidence of heavy rainfall.

Other factors are: -The promotion of hydraulic surcharge in water levels -The presence of natural or man-made obstructions in the flood path such as bridges piers, floating debris, weirs, etc. -Also included are the generally unforeseen river-surge events caused by sudden dam failure, land slip or mudflow.

The slow-developing characteristic of flood flows in many large rivers is in sharp contrast to flash floods more commonly but not exclusively associated with small catchments. There are so many small catchments within a given region, that efficient surveillance, warning and protection against the eventuality proves difficult. In other regions, flash floods occur each year on the same river. Warning in these cases is more a problem of timeliness.

Floods Hazards Information needed by Planers The dangers of flood water are associated with a number of different parameters:- -Depth of water -Duration -Velocity -Rate of rise -Frequency of occurrence -Seasonality

Flood Hazards Assessment Flood Maxima- “the regional flood” By far the most effective way of determining extreme flood levels (and discharges thereafter) is through exhaustive survey of riverside conditions and questioning of local inhabitants.

I Flood class Topographic situationFlood susceptibility 1Hilly zones and other high areas Above highest flood level 2Areas of medium heightSubject to exceptional flooding 3Medium height to low areasInfrequent flooding, in part seasonal shallow flooding 4Low-lying areasSubject to annual flooding. flooding, in part frequently and deeply flooded 5Local depressionsDeep flooding, often moist 6Local depressions, lowest parts Frequently very deeply flooded and in parts waterlogged throughout the year

II Flood classDischarge m³/sec Water level(m) Frequency in 100 yrs Flood/war ning Up to Up to – 100 Dangerous flood Up to Up to – 20 Emergent flood Up to Up to – 4 Exceptiona l flood Up to Up to

Floods and Forests -A key driving force in the yearly increase in flood disasters in the rapid rate of deforestation in the tropics.

-According to an FAO/UNEP study in 1981, tropical forests are disappearing at the rate of 7.3 million hectare (18 million acres)per year:.2 million hectares (10.4 million acres) a year in Latin America; 1.8 million hectares (4.4 million acres) a year in Asia; and 1.3 million hectares (3.2 million acres) a year in Africa.

The environmentalist Erik Eckholm wrote in Down to Earth (pluto Press;Norton, 1982): “Decades of research have proved that the deforestation of watersheds, especially around smaller rivers and streams, can increase the severity of flooding, reduce stream flows and dry up springs during dry seasons, and increase the load of sediment entering waterways.

Yet most efforts to combat such problems have entailed engineering measures –dams, embankments, dredging- that address symptoms and not causes. The exact contribution of deforestation to flood trends is probably impossible to pinpoint, but as flooding worsens in country after country, new attention is being given to watersheds”

Interventions: Reforestation and other soil conservation measures could decrease floods. The sponge effect of trees, grass and crops, whereby the land absorbs rainfall and then releases it slowly over a long period of time, reduces flooding