FLOOD MAPPING FOR SUNGAI BUNUS
MOHD IRSYAM NOORFAWANA BIN MASRI
A project report submitted in fulfilment of the
requirements for the award of the degree of
Master of Engineering (Hydrology & Water Resources)
Faculty of Civil Engineering
Universiti Teknologi Malaysia
JUNE 2015
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ACKNOWLEDGEMENT
First of all, I am grateful to Allah S.W.T for the good health and wellbeing
that were necessary to complete this dissertation.
I was really appreciated to many people that contribute towards my
understanding and thoughts in order to finish this study. I wish to express my sincere
thanks to my supervisor, Dr. Zulhilmi Bin Ismail for his guidance and
encouragement. Also to Dr. Mohamad Hidayat B. Jamal for hiscritics, advice and
guidance. Also my sincere thank you to Perunding Azman, Ooi & Rao Sdn Bhd for
the education fees sponsorship.
Last but not least, to my beloved wife Mrs. Nurashikin Binti Zainal Abidin, I
am extremely thankful to her for sharing knowledge, and sincere encouragement
extended to me. To my lovely daughters, Nurin and Nadia, thank you for being such
a lovely and understanding.
My sincere appreciation to my colleagues Mrs. Nurashikin, Miss Farihan,
Mrs. Nurhaniza, Mrs. Norhayati and Mr. Aliff for their supportive, motivation, love,
advice and friendship.
I take this opportunity to express gratitude to all of the Hydrology and Water
Resources lecturers for their knowledge's and experiences. I also thank my parents
and parents in law for the unceasing Dua's, encouragement, support and attention.
I also place on record, my sense of gratitude to one and all, who directly or
indirectly, have lent their hand in this venture.
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ABSTRACT
Nowadays, the occurrence of flash flood in urban area in Malaysia has
become major problem. . Flood Mapping is one of the method that shows the flood
extent at the area that involve with flooding. There are a lot of beneficial on this
flood inundation map. This flood mapping for Sungai Bunus were modelled using a
HEC-GeoRAS two-dimensional hydraulic model to capture the hydraulic response
of the river and its floodplains in extreme flooding condition due to major storm
events. Digital terrain model (DTM) or LIDAR data are used for flood mapping
process. The model is capable to predict flood depth and velocity magnitude of flood
propagation. The flood mapping could assist local authorities to develop flood
warning system at the flood prone area and prepare proper mitigation measures to
prevent catastrophic damage and lost at the area where the flood frequently occur.
This flood mapping was develop with two scenario which is existing river without
flood pond and existing river with flood pond. The result shows significant reduction
in flood water level if a series of pond from upstream was use as a flood mitigation
measures.
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ABSTRAK
Pada masa kini, kejadian banjir kilat di beberapa kawasan bandar di Malaysia
telah menjadi masalah besar. Pemetaan banjir adalah salah satu kaedah yang
menunjukkan tahap banjir di kawasan yang terlibat dengan banjir. Terdapat banyak
yang kebaikan pada kaedah pemetaan banjir. Pemetaan banjir bagi Sungai Bunus
telah dimodelkan menggunakan model hidraulik dua dimensi HEC-GeoRAS untuk
manganalisis hidraulik sungai dan dataran banjir dalam keadaan banjir yang teruk
disebabkan oleh peristiwa hujan lebat. Model rupa bumi digital (DTM) atau LIDAR
data digunakan untuk proses pemetaan banjir. Model ini mampu untuk meramalkan
kedalaman banjir dan magnitud halaju air banjir. Pemetaan banjir boleh membantu
pihak berkuasa tempatan untuk membangunkan sistem amaran banjir di kawasan
yang sering dilanda banjir dan menyediakan langkah-langkah tebatan yang betul
untuk mengelakkan kerosakan dan kehilangan harta benda di kawasan yang sering
berlaku banjir. Pemetaan banjir ini dihasilkan berdasarkan dua senario yang berbeza
iaitu sungai sedia ada tanpa kolam banjir dan sungai sedia ada dengan kolam banjir.
Hasil kajian menunjukkan pengurangan yang ketara dalam paras air banjir jika
kaedah beberapa siri kolam takungan banjir bermula dari kawasan hulu digunakan
sebagai langkah pencegahan banjir.
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TABLE OF CONTENT
CHAPTER TITLE PAGE
DECLARATION ii
DEDICATION iii
ACKNOWLEDGEMENT iv
ABSTRACT v
ABSTRAK vi
TABLE OF CONTENTS vii
LIST OF TABLES x
LIST OF FIGURES xii
LIST OF SYMBOLS xv
LIST OF APPENDICES xvi
1 INTRODUCTION 1
1.1 Background of the Problem 1
1.2 Statement of the Problem 3
1.3 Objectives of the Study 4
1.4 Scope of the Study 4
1.5 Significance of the Study 5
2 LITERATURE REVIEW 6
2.1 Introduction 6
2.2 Flood 12
2.3 Risk and Hazard 12
2.4 Flood Frequency Analysis 14
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2.5 Flood hazard mapping 14
2.6 Flood modelling 18
3 RESEARCH METHODOLOGY 22
3.1 Introduction 21
3.2 Research Boundary 22
3.3 Design Methodology 23
3.4 Data Collection 26
3.4.1 LIDAR Data 26
3.4.2 River Data and Rainfall Data 26
3.4.3 Data Segmentation 27
3.4.3.1 Data Development 27
3.4.3.2 Data Validation 27
3.5 Data Analysis 28
3.5.1 LIDAR Data 28
3.6 HEC-GeoRAS Model 28
3.6.1 HEC-Geo RAS Development 29
3.6.2 Digitizing Process 30
3.6.3 HEC-RAS Model Development 43
3.6.4 Channel Data 43
3.6.5 Hydraulic Analysis in HEC-RAS 43
3.7 HEC-RAS Model 44
3.8 Advantages of HEC-GeoRAS 49
3.9 Disadvantages of HEC-GeoRAS 50
4 RESULT AND ANALYSIS 51
4.1 Introduction 51
4.2 Flood Mapping 51
4.3 Result 52
4.4 Calibration & Validation 61
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4.5 Design Rainfall 63
4.5.1 Development of IDF Curve 63
4.6 Calibration 68
4.6.1 Calibration Results 68
4.6.2 Discussion on Calibration Limitation 69
5 CONCLUSION AND RECOMMENDATION 70
5.1 Conclusion 70
5.2 Recommendations for future research: 71
5.3 Recommendations for Local Authorities
and communities 72
REFERENCES 73
APPENDICES 77
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LIST OF TABLES
TABLE NO. TITLE PAGE
2.1 Summary of Flood Events at Sungai Bunus 9
2.2 Destruction and Damage Caused by Flooding
Events at Sungai Bunus 9
4. 1 Flood Depth Colour Scheme 52
4. 2 Flood Inundation Area for Existing Condition
without Pond 53
4. 3 Flood Inundation Area for Existing Condition
with Pond 53
4.4 List of Rainfall Stations Use in Deriving IDF
Curve and Calibration 61
4.5 The Coefficients of the Fitted IDF Equation for
Stor JPS Ampang 64
4.6 Maximum Rainfall for Stor JPS Ampang
(Station No.: 3117070) – Previous study 64
4.7 Maximum Rainfall intensity for Stor JPS Ampang
(Station No: 3117070) – Previous study 65
4.8 Maximum Rainfall for Stor JPS Ampang
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(Station No: 3117070) - HP1 65
4.9 Maximum Rainfall Intensity for Stor JPS Ampang
(Station No: 3117070) - HP1 66
4.10 Comparison of Rainfall Intensity from the
Previous Study and New HP 1 66
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LIST OF FIGURES
FIGURE NO. TITLE PAGE
2. 1 Study Area of the Sg. Bunus 7
2.2 Sungai Bunus catchment. 8
2. 3 Flooding Occurs at 24 February 2011 10
2. 4 Flooding Occurs at 14 April 2011 10
2. 5 Flooding Occurs at 13 December 2011 11
2. 6 Flooding Occurs at 2 May 2012 11
2.7 Flood Inundation Map
(USGS Flood Inundation Mapping Science) 16
2.8 Flood Inundation Map (DID) 17
2.9 Shows an application of GIS in flood mapping
in United States. 20
3.1 Flowchart of the Process Flow 24
3.2 Steps In Digitizing Process 31
3.3 ArcGIS 10.1 32
3.4 New Map 32
3.5 Add Data 33
3.6 LIDAR Data 33
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3.7 RAS Geometry Layer Setup 34
3.8 Layer Setup for HEC RAS PreProcessing 35
3.9 Create RAS Layers 35
3.10 Create All Layers 36
3.11 RAS Layers Are Successfully Created 36
3.12 Editor Toolbar Figure 37
3.13 Digitizing the Stream 38
3.14 Create River Attribute 38
3.15 Complete Digitizing Process 39
3.16 Layer Setup- Required Surface 40
3.17 Layer Setup- Required Layers 41
3.18 Layer Setup- Optional Tables 41
3.19 Layer Setup- Optional Layers 42
3.20 Export GIS Data 42
3.21 Steps for HEC-RAS Model 44
3.22 HEC-RAS 4.1.0 45
3.23 Import GIS Data 45
3.24 Unit for import GIS Data 46
3.25 River Reach Streamlines 46
3.26 Cross Section and IB Nodes 47
3.27 Geometry Schematic Of The River System 47
3.28 Edit Geometric Data 48
3.29 Flow data 49
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3.30 Steady Flow Boundary Condition 49
3.31 Steady Flow Analysis 50
3.32 GIS Export 50
3.33 Convert RAS Output File to XML 51
3.34 Flood Inundation Map 52
4.1 Existing Drainage Model with 2D Flood Plain 54
4.2 Drainage model with Digital Terrain Model (DTM)
for Project Area. 55
4.3 Flood Mitigation Model (Without 2D Flood Plain) 56
4.4 Flood Map for Existing Condition (10 ARI) 57
4.3 Flood Map for Existing Condition (50 ARI) 58
4.4 Flood Map for Existing Condition (100 ARI) 59
4.5 Flood Map with Flood Pond Condition (50 ARI) 60
4.8 Rainfall Stations 62
4.9 IDF for Kuala Lumpur 63
4.10 Comparison of Rainfall from the Two Stations 67
4.11 Observed Water Level in Sg. Bunus at JalanTun Razak
on 24th Feb 2011 67
4.12 Comparison of Water Level between Observed and
Simulated for 24th Feb 2011 Flood 68
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LIST OF SYMBOLS
DID - Drainage and Irrigation Department
GIS - Geographic Information System
ARI - Average Recurrence Interval
HEC - Hydrologic Engineering Center
ESRI - Environmental System Research Institute
USACE - United States Army Corps of Engineers
1-D - One Dimensional
2-D - Two Dimensional
USGS - United States Geological Survey
FOTRAN - Formula Translating System
MS-DOS - Microsoft Disk Operating System
FEMA - Federal Emergency Management Agency
Ha - Hectare
Km 2 - Kilometre Square
m 3/s - Metre Cubic per Seconds
TIN - Triangular irregular networks
LiDAR - Light Detection and Ranging
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LIST OF APPENDICES
APPENDIX. TITLE PAGE
A Sungai Bunus Lower Profile 79
Sungai Bunus Middle Profile. 80
Sungai Bunus Upper Profile 81
B HEC-RAS Output Table 82
CHAPTER 1
INTRODUCTION
This chapter consist of background of the problem, statement of the problem,
objective of the study, scope of stdy and significant of study
1.1 Background of the Problem
In recent years there have been a number of significant riverine floods in the
rest of the world, which resulted in tragic loss of life and in enormous material
damage. In the past decades, thousands of lives have been lost, directly or indirectly,
by flooding. In fact, of all natural risks, floods pose the most widely distributed
natural risk to life today.
River flood risk management is the process under which different bodies try
to reduce the current and the future vulnerability of human society to natural risks.
Flood risk management measures can be structural where the risk is modified for
example dam and reservoir construction, channel improvements, bypass channels
and artificial levees. Non-structural where the flood damage and disruption is
modified for example setting up flood plain management regulations such as zoning,
building codes and measures where both the methods are applied. It is clear that no
protection work can offer a hundred percent security against floods. There is always
the possibility that a threshold is surpassed and that floodwater will enter into areas
where it should not go, e.g. by overtopping or breaching of dikes.
2 In the past, structural and non-structural measures have been adopted for the
flood control and flood management. Non-structural measures used to estimate the
floods and their proper management has been accelerated in the last couple of
decades throughout the globe in comparison to expensive structural measures. Non-
structural measure includes evaluation of impact of rainfall on runoff of a catchment,
return period of different magnitudes/frequency of floods and flood inundated areas,
and socio-economic aspects of floods
Starting in the year 2000s, extreme rainfall events with high intensity are no
longer a new issue in Malaysian urban cities, especially in the West Coast area This
phenomenon is formed mostly through convection process (Embi , 2004). The main
motivation of this research is an importance of river flood events in urban areas
which cause in large number loss of lives and properties damages. Knowledge on the
river basin response to rainfall events which is in the form of runoff is vital in
engineering practices for urban planning and management. River flood modelling is
a combination of hydrological modelling, hydraulic modelling and river flood
visualization using GIS.
Floods can also be very incremental to the primary effects, as the affected
region takes much time to recover where diseases and epidemics outbursts are
frequent. Floods are usually recurrent and have massive impacts on agriculture based
economies, which is the case of most small islands. Thus small countries and islands
suffer a heavy burden from such events on the economic aspect. Thus, flood studies
can be very useful in alleviating the already stressed economies of the insular
countries. The study of floods helps to understand the characteristics of the floods,
their cause and thus provide relevant data in assessment of these events.
A flash flood is characterized by a rapid stream rise with depths of water that
can reach well above the banks of the stream. Flash flood damage and most fatalities
tend to occur in areas immediately adjacent to a stream. Additionally, heavy rain
falling on steep terrain can weaken soil and cause mud slides, damaging homes,
roads and property.
3 Flooding is one of the major natural hazards affecting communities across
Malaysia and has caused damages worth millions of dollars every year. The required
allocation for flood mitigation projects has increased almost 600% (RM 6000
million) for the 8th Malaysian Plan compared to RM 1000 million during the 7th
Malaysian Plan (Abdullah, 2000).
Knowing the fact that the floods are part of human being life and that this
natural phenomena can’t be fully controlled, it’s important to focus and improve
knowledge about the prevention. In order to achieve this issue it is crucial that, more
specific and scientific work must be developed to a better understanding of the
flooding phenomena and their related geographical, hydrological and
geomorphologic causes. (Vaz (2000 and Jaarsma et. al. 2001) emphasized,
respectively, the need to define a strategy that includes a judicious combination of
structural and none structural measures, based on a careful analysis of the past floods
and improvements in floods forecasting.
The main objectives of flood mapping can be sorted as follows: to prevent
loss of life, to minimize property damage, to minimize social disruption and to
encourage coordinated approach for land/water use. The role of flood mapping in
river engineering is an important feature in planning and management: basis for
managing flood plains, engineering & planning tool, first step in flood plain
management, part of legislation for regulating development and basis for pursuing
structural and non-structural measures.
1.2 Statement of the Problem
A flash flood produced by a rainfall event which is due to flood mitigation
measures failure and poor drainage system. In a flash flood scenario, the subsequent
flood wave develops over a relatively short time and flows rapidly through the
downstream area as opposed to a rainfall event that would propagate more slowly
through the downstream area.
4 When a flash flood happened or is deliberately demolished, large quantities
of water are suddenly released, creating major flood waves capable of causing
disastrous damage to downstream valley. Major flood waves may seriously damage
or destroy power plants, industrial plants, roads and bridges and may cause loss of
life, adverse ecological and environment impact.
1.3 Objectives of the Study
Followings are the objectives proposed for this study:-
a) To determine water surface profiles at specific locations along the
stream network using the HEC River Analysis System (HEC-
GeoRAS).
b) To establish river flood delineation mapping in Sungai Bunus river
basin.
c) To predict river flood risk map in Sungai Bunus river basin.
1.4 Scope of the Study
The scope of this study is within this related area:-
a) Data collection and analysis
b) Flood hazard map analysis with HEC-RAS and HEC-GeoRAS
modeling
The flood hazard maps modelling will be conducted to determine the flood
inundation extents of a failure of the flood mitigation measures. Unsteady flows
HEC-GeoRAS Model are developed for a sunny day failure, raining day and during
maximum flood failure. The development of accurate flood hazard maps requires
high-resolution topographic data of known accuracy. More accurate topographic data
lead to more accurate flood-inundation maps (Horritt and Bates, 2001). Field
5 surveying produces the most accurate elevation data but can be time consuming and
expensive.
Light detection and ranging (lidar) is an airborne laser-profiling system that
produces location and elevation data to define the surface of the Earth and the
heights of aboveground features. Lidar can produce a digital elevation model (DEM)
with 1-foot (ft) contours that can be imported to a geographic information system
(GIS) in a relatively short amount of time.
The flood hazard maps indicate areas that would be flooded as a result of a
failure of flood mitigation measures. The inundated areas depicted on flood-
inundation maps are approximate, and accuracy of such maps is a function of the
accuracy of the topographic data, the hydraulic models on which the maps are based,
the assumptions made about the dam failure mode, and the initial flood wave. For
this report, lidar data with a vertical accuracy of about 3.3 inches (in) were used to
develop a 1-ft contour elevation map for the study area. The Hydrologic Engineering
Center’s River Analysis System (HEC-RAS) modeling software developed by the
U.S. Army Corps of Engineers, a standard for flood-inundation models, was used to
perform unsteady-flow simulations to model the dynamic nature of the flood wave
produced by a dam-breach scenario (Hydrologic Engineering Center, 2010).
1.5 Significance of the Study
The significant of the study is to develop the river hydraulics model, simulate
a flood mitigation measures failure and map the resulting flood wave. The proper
modeling of the hazards associated with flood mitigation measures will assist in land
use planning and developing emergency response plan to help mitigate catastrophic
loss to human life and property.
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