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A
Project on
"ANALYSIS OF MAXIMUM HOURLY RAINFALL FOR DESIGN OF STORM DRAIN
NETWORK OF SURAT CITY"
Prepared By: Supervisor
PINGUL JIGNESH K Dr. S.M. YADAV
(U12CE013) Professor
CED, SVNIT, Surat
Civil Engineering Department
SARDAR VALLABHBHAI NATIONAL INSTITUTE OF TECHNOLOGY
ICCHANATH, SURAT, GUJARAT - 395007
TableofContent 1. Basic Introduction
2. Objective
3. Scope of Study
4. Literature Review
5. Study Area
6. Need for Study
7. Rainfall Data Collection of Silvassa
8. Analysis of Rainfall Data for Silvassa
9. Rainfall Data Collection & Analysis for
Surat
10. Storm Drain Design for Illustrative
Region
11. Technical Visit
12. Conclusion
The circulation and conservation of earth’s water as it circulates from the land
to the sky and back again is called the ‘hydrological cycle’ or ‘water cycle’.
Hydrological cycle
BasicIntroduction
BasicIntroduction  Precipitation : It denotes all forms of
water that reach the earth from the
atmosphere.
The usual forms are rainfall , snowfall,
hail, frost, drizzle and dew.
 Evaporation : The process by which
water changes from a liquid to a gas & is
transferred from the surface to the
atmosphere.
 Interception : The process in which, the
part of precipitation, which may get
evaporated or flow down after
interception through trees and structures.
 Transpiration : Vegetation sends a part
of water from under ground surface back
to atmosphere.
 Infiltration : A process in which portion
of water that reaches the ground surface
and enters the earth surface.
 Runoff : The process in which the portion
of precipitation by different paths above
and below ground surface reaches the
stream channel.
BasicIntroduction
 This Runoff may cause flood in the city
areas and hence storm drain network are laid
to overcome this problem.
 A storm drain system is a network of pipes
used to convey runoff from a city to a
receiving water body.
 Their design involves determination of
diameters, slopes and crown elevation or
invert elevation of each pipe.
BasicIntroduction
 The selection of layout or network of pipe
location for a storm sewer system requires
a considerable amount of subjective
judgment.
 Gradually manholes/inlets are placed at
street intersections and at major changes
in grade or ground surface slope.
BasicIntroduction
Objective
Objective of the study:
 To find out the 1-hour maximum rainfall
depth for different return periods.
 To find out rainfall intensity duration
frequency relationship.
 Apart from these, to design storm drain
network for an illustrative region.
ScopeofStudy
 To carry out literature review for
analyzing rainfall intensity and frequency.
 To carry out data collection for compiling
rainfall intensity.
 To carry out analysis of collected data for
Silvassa and Surat city.
 To compute 1-hour maximum rainfall
Name Year Publication Description
Elsebaie I H
“Developing rainfall
intensity–duration–
frequency
relationship for two
regions in Saudi
Arabia”
2012 Elsevier
IDF relationship is a
mathematical relationship
between the rainfall intensity i,
the duration d, and the return
period T (or, equivalently, the
annual frequency of exceedance
‘f ‘referred to as ‘frequency’).
A
Ramchandra
Rao
“Statistical Analysis
of Indiana
Rainfall Data”
2006
Purdue
University
West
Lafayette
Several aspects of short time
interval rainfall data from
Indiana are investigated in this
study. The variability in rainfall
intensity estimates by different
procedures is quantified.
Dr. Lamia
Abdul Jaleel
“Developing Rainfall
Intensity-duration-
freqency
Relationship For
Basrah City”
2012
Kufa
Journal of
Engineering
(K.J.E)
The purpose of this paper is to
develop an empirical formula to
estimate design rainfall intensity
based on intensity–duration–
frequency (IDF) curves for
Basrah City.
LiteratureReview
Name Year Publication Description
Agnihotri et al
“Analysis of Rainfall
Data and Design of
storm Water Drainage
System in an Urban
Area”
2013
Global
Journal for
research
analysis
Rainfall data available from
1969 to 1983 are of duration 5,
10, 15, 30, 45, 60, 75, 90
minute. Analysis of rainfall data
is carried for year 1969 to 1983
and one year flood frequency is
calculated
Harshil H Gajjar
“Storm Water
Network Design of
Jodhpur Tekra
Area of City of
Ahmedabad “
2014
International
Journal of
Engineering
Development
and Research
In this paper, past 20 years
rainfall data is taken. The system
has been designed considering in
total of 65% of the impervious
area.
Rational method has been used
for estimation of storm water
runoff. .
S M Yadav
“A Case Study on
Remodelling of
Bambapada Khadi,
Silvassa “
2011
Present paper discusses the steps
involved in the design of storm
water drains.
LiteratureReview
Map of Surat City
StudyArea
StudyArea  Surat city is located on the western part
of India in Gujarat. It is also called as city
of flyovers.
 The city is located at 306 km south of the
state capital, Gandhinagar on the left bank
of the Tapti River (Tapi).
 Surat is Gujarat's second largest city with
a population of 2.1 million at the 2001
census and 4.6 million at the 2011 census.
 Surat city is divided into 7 zones by Surat
Municipal Corporation namely:
 North Zone
 South Zone
 East Zone
 West Zone
 South-West Zone
 South-East Zone
 Central Zone
StudyArea
 Surat is a port city situated on the banks of
the Tapti River. The city is located
at 21°10′N 72°50′E.
 The average annual rainfall of surat city
is about 1,200 millimetres (47 in) (IMD).
 The general slope is from north-east to
south-west.
 The city is 13m above mean sea level.
 The coastal line is along the villages of
Hazira, Mora, Limla, Dumas, Bhimpor,
Abhava, Gavier, Sarsana and Vesu.
StudyArea
NeedforStudy
 In Surat, life and property are frequently
under the threat of flooding due to heavy
rainfall. The average annual rainfall of
Surat is about 1200 millimetres.
 Such heavy rainfall, sometimes coupled
with high sea levels associated with storm
surges during the passage of tropical
cyclones, can cause flooding.
 Apart from natural causes, sometimes
human activities may also influence the
prevalence of flooding.
 Storm water drainage is an integral part of
the essential infrastructure of a modern
city. In Surat, separate systems are
provided for the collection and disposal of
storm water and sewage.
NeedforStudy
 For study of rainfall intensity, yearly rainfall data
and the 24-hour maximum rainfall data were
collected from Central Water Commission (CWC)
or Municipal corporation.
 Rainfall intensity and duration is calculated by
using India Meteorological Department (IMD)
Method.
 1-hour rainfall has been estimated by using 24-
hours maximum rainfall, using IMD empirical
reduction formula. 1-hour maximum rainfall is
denoted by:
Pt = P24 (t/24)1/3
where P24 = yearly 24-hour maximum rainfall
Rainfall Data of Silvassa for 29
years.
RainfallDatacollectionofSilvassa
 By using Gumbel frequency distribution
method, frequeny analysis of 1-hour
maximum rainfall is carried out.
 Graph is plotted between 1-hour maimum
rainfall and Gumbel frequency factor(K).
 1-hour maximum rainfall depth for
different return periods of 2, 5, 10, 20, 50
and 100 year is calculated.
Pt = Pm + K*s
where Pt = expected 1-hour T-year rainfall depth,
Pm = mean 1-hour maximum rainfall
s = standard deviation of 1-hour maximum rainfall
k = Gumbel frequency factor
AnalysisofRainfallDatafor
Silvassa
 1-hour maximum rainfall depth is used for
finding the t-minute rainfall depth for
different time period such as 5, 10, 15, 30
and 120 minute.
 1 hour T-year rainfall depth is multiplied
by factor (taken from Journal of Indian
Water Works Association, Vol-Octo-Dec-
2007 ) to obtain T minute Rainfall Depth.
Frequency Analysis Using Gumbel Distribution method
AnalysisofRainfallDatafor
Silvassa
 Rainfall data of different time period ranging from
previous 50 year, 100 year and 120 year are
obtained for Surat city.
 Similar calculations is executed on these data and 1-
hour maximum rainfall depth, maximum rainfall
intensity and intensity duration curve is obtained.
Estimation of Rainfall Intensity of Surat for 30 years.
Estimation of Rainfall Intensity of Surat for 50 years.
Estimation of Rainfall Intensity of Surat for 100 years.
Estimation of Rainfall Intensity of Surat for 120 years.
Datacollection&AnalysisforSura
StormDrainDesignforanIllustrat
Region
 Design of Storm Water Drainage Network
for a rectangular plot of area 180 X 250
square meter has been carried out.
 Reduced levels of all the nodes for the
illustrative region were available.
 The main line passes through the centre of
the catchment area.
 The runoff from other part of the
catchment area flows through the sub
branches which are connected to the main
line.
DesignofStormDrain
Network
 The frequency of storm selected was once
in 2 years.
 Usually, the storm drains are not designed
for peak discharges or extreme events
from economical point of view.
 The design of the drain should be
economical and at the same time it should
prevent frequent flooding and it should
drain out quickly.
DesignofStormDrain
Network
For designing the storm water network for
the given area the following data is
required:
1.Catchment area
2. Rainfall intensity and duration
3. Impervious factor
4. Design of Drainage system
 Rainfall Intensity and duration has been
estimated using India Meteorological
Department (IMD) method.
 For the paved area, the impervious factor
is taken as 0.7
DesignofStormDrain
Network
 Storm water runoff has been calculated by
using Rational Method suggested by
CPHEEO.
 The diameter of pipe is selected so as to
maintain the minimum velocity of 0.6 m/s
and to carry slightly more discharge
compared to the theoretical discharge.
 The diameter of the pipe was selected to
maintain a self cleansing velocity.
 Moreover, the velocity of flow should not
exceed more than scouring velocity.
Design of Storm drain network of an illustrative region
DesignofStormDrain
Network
 A site was visited at Godadara where
drainage pipes were being laid for the
removal of storm water.
 The storm water has been transported to
the pumping station, treated and than
disposed of in to the Khadi.
 Consultant : Mayur Shah, Assistant
Engineer Surat Municipal Corporation.
TechnicalVisit
 The pipes which were being laid were
spigot pipe of 500 mm diameter and the
length of each pipe was 265 mm.
 The pipes were being laid at the slope of
1:500. Generally the slope in the field is
set by two methods:
1. Boning method 2.Spirit level
TechnicalVisit
 Analysis of Rainfall Data of 29 years for
Silvassa region has been carried out. Maximum
hourly intensity with a recurrence interval of 2
year is estimated to be 78 mm/hr.
 The same analysis of rainfall data was carried
out for Surat region:
 The present study helps in computing rainfall
intensity which is used to estimate storm water
runoff.
 The storm water runoff thus computed is very
important for the design of storm drain network.
Conclusion
Years Intensity (mm/hr)
30 Years 56.5
50 Years 56.309
100 Years 52.87
120 Years 51.54
Referencesand
Bibliography
 https://www.suratmunicipal.gov.in/TheCity/weather_annual.h
tml
 Central Public Health and Environment Engineering
Organization manual on Sewerage and Sewage
Treatment(1993), Ministry of Urban Development, New
Delhi
 Subramanya K (1994), Engineering Hydrology, Tata-
McGraw-Hill Publishing Company Limited, New Delhi
 Garg Santoshkumar (1993), Irrigation Engineering and
Hydraulic Structures, Khanna Publications.
 A Case Study on ' Remodelling of Bambapada Khadi,
Silvassa '.
 http://www.pressseal.com/Downloads/EvolutionOfWatertight
StormDrainageSystemsFinal.pdf
 Madhur K. Rathi and Patil Dhananjay Rajiv, " Study Of
Problems and Corrective Actions of Urban Drainage
Network“.
 Dr. Lamia Abdul Jaleel and Maha Atta Farawn, " Developing
Rainfall Intensity-Duration-Frequency Relationship For
Basrah City "
 Dr. P. G. Agnihotri, R. B. Khasiya, Priyanka D. Harpalani, “
Analysis of Rainfall Data and Design of storm Water
Drainage System in an Urban Area.”
 Ibrahim H. Elsebaie, “ Developing Rainfall Intensity-
Duration-Frequency Realtionship For Two Regions In Saudi
Arabia.”
 John Argue, “ Storm Drainage Design In Small Urban
Catchments: A Handbook For Australian People.”
 City of Sheridan, Public Works Department, “Storm drainage
Design Criteria; City of Sheridan, Wyoming”
 Drainage Service Department, Government of Hong
Kong, “Storm Water Drainage Manual; Planning,
Design and Management.”
Referencesand
Bibliography
 William S. Springer, “ Storm Drain Design”
 Kwokwing Chau and C. S. Cheung, “ Knowledge
Representation on Design Of Storm Drainage system.”
 Minister of Urban Development, Government of India, “
Storm Water Drainage.“
 Zameer Ahmed, D. Rammohan Rao, K. Ram Mohan Reddy,
Ellam Raj, “Rainfall intensity Variation For Observed Data
And Derived Data – A Case Study of Imphal.”
 “Application of Methods For Analysis of Rainfall Intensity in
Areas of Israeli, Jordanian and Palestinia Interest.”
 Rezual Kabir, P. Das, “Short Duration Rainfall Estimation of
Sylhet, IMD and USWD Method(2007), Journal of Indian
Water Works Association.”
 Ram Babu, Tejwani, K. K. Agarwal, M. C. & Bhusan, L. S.
(1979) “Rainfall Intensity Period Equation and Nomograph of
India, CSWCRTI, ICAR, Dehradun India.”
Referencesand
Bibliography
Thank You

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Project ppt

  • 1. A Project on "ANALYSIS OF MAXIMUM HOURLY RAINFALL FOR DESIGN OF STORM DRAIN NETWORK OF SURAT CITY" Prepared By: Supervisor PINGUL JIGNESH K Dr. S.M. YADAV (U12CE013) Professor CED, SVNIT, Surat Civil Engineering Department SARDAR VALLABHBHAI NATIONAL INSTITUTE OF TECHNOLOGY ICCHANATH, SURAT, GUJARAT - 395007
  • 2. TableofContent 1. Basic Introduction 2. Objective 3. Scope of Study 4. Literature Review 5. Study Area 6. Need for Study 7. Rainfall Data Collection of Silvassa 8. Analysis of Rainfall Data for Silvassa 9. Rainfall Data Collection & Analysis for Surat 10. Storm Drain Design for Illustrative Region 11. Technical Visit 12. Conclusion
  • 3. The circulation and conservation of earth’s water as it circulates from the land to the sky and back again is called the ‘hydrological cycle’ or ‘water cycle’. Hydrological cycle BasicIntroduction
  • 4. BasicIntroduction  Precipitation : It denotes all forms of water that reach the earth from the atmosphere. The usual forms are rainfall , snowfall, hail, frost, drizzle and dew.  Evaporation : The process by which water changes from a liquid to a gas & is transferred from the surface to the atmosphere.  Interception : The process in which, the part of precipitation, which may get evaporated or flow down after interception through trees and structures.
  • 5.  Transpiration : Vegetation sends a part of water from under ground surface back to atmosphere.  Infiltration : A process in which portion of water that reaches the ground surface and enters the earth surface.  Runoff : The process in which the portion of precipitation by different paths above and below ground surface reaches the stream channel. BasicIntroduction
  • 6.  This Runoff may cause flood in the city areas and hence storm drain network are laid to overcome this problem.  A storm drain system is a network of pipes used to convey runoff from a city to a receiving water body.  Their design involves determination of diameters, slopes and crown elevation or invert elevation of each pipe. BasicIntroduction
  • 7.  The selection of layout or network of pipe location for a storm sewer system requires a considerable amount of subjective judgment.  Gradually manholes/inlets are placed at street intersections and at major changes in grade or ground surface slope. BasicIntroduction
  • 8. Objective Objective of the study:  To find out the 1-hour maximum rainfall depth for different return periods.  To find out rainfall intensity duration frequency relationship.  Apart from these, to design storm drain network for an illustrative region.
  • 9. ScopeofStudy  To carry out literature review for analyzing rainfall intensity and frequency.  To carry out data collection for compiling rainfall intensity.  To carry out analysis of collected data for Silvassa and Surat city.  To compute 1-hour maximum rainfall
  • 10. Name Year Publication Description Elsebaie I H “Developing rainfall intensity–duration– frequency relationship for two regions in Saudi Arabia” 2012 Elsevier IDF relationship is a mathematical relationship between the rainfall intensity i, the duration d, and the return period T (or, equivalently, the annual frequency of exceedance ‘f ‘referred to as ‘frequency’). A Ramchandra Rao “Statistical Analysis of Indiana Rainfall Data” 2006 Purdue University West Lafayette Several aspects of short time interval rainfall data from Indiana are investigated in this study. The variability in rainfall intensity estimates by different procedures is quantified. Dr. Lamia Abdul Jaleel “Developing Rainfall Intensity-duration- freqency Relationship For Basrah City” 2012 Kufa Journal of Engineering (K.J.E) The purpose of this paper is to develop an empirical formula to estimate design rainfall intensity based on intensity–duration– frequency (IDF) curves for Basrah City. LiteratureReview
  • 11. Name Year Publication Description Agnihotri et al “Analysis of Rainfall Data and Design of storm Water Drainage System in an Urban Area” 2013 Global Journal for research analysis Rainfall data available from 1969 to 1983 are of duration 5, 10, 15, 30, 45, 60, 75, 90 minute. Analysis of rainfall data is carried for year 1969 to 1983 and one year flood frequency is calculated Harshil H Gajjar “Storm Water Network Design of Jodhpur Tekra Area of City of Ahmedabad “ 2014 International Journal of Engineering Development and Research In this paper, past 20 years rainfall data is taken. The system has been designed considering in total of 65% of the impervious area. Rational method has been used for estimation of storm water runoff. . S M Yadav “A Case Study on Remodelling of Bambapada Khadi, Silvassa “ 2011 Present paper discusses the steps involved in the design of storm water drains. LiteratureReview
  • 12. Map of Surat City StudyArea
  • 13. StudyArea  Surat city is located on the western part of India in Gujarat. It is also called as city of flyovers.  The city is located at 306 km south of the state capital, Gandhinagar on the left bank of the Tapti River (Tapi).  Surat is Gujarat's second largest city with a population of 2.1 million at the 2001 census and 4.6 million at the 2011 census.
  • 14.  Surat city is divided into 7 zones by Surat Municipal Corporation namely:  North Zone  South Zone  East Zone  West Zone  South-West Zone  South-East Zone  Central Zone StudyArea
  • 15.  Surat is a port city situated on the banks of the Tapti River. The city is located at 21°10′N 72°50′E.  The average annual rainfall of surat city is about 1,200 millimetres (47 in) (IMD).  The general slope is from north-east to south-west.  The city is 13m above mean sea level.  The coastal line is along the villages of Hazira, Mora, Limla, Dumas, Bhimpor, Abhava, Gavier, Sarsana and Vesu. StudyArea
  • 16. NeedforStudy  In Surat, life and property are frequently under the threat of flooding due to heavy rainfall. The average annual rainfall of Surat is about 1200 millimetres.  Such heavy rainfall, sometimes coupled with high sea levels associated with storm surges during the passage of tropical cyclones, can cause flooding.
  • 17.  Apart from natural causes, sometimes human activities may also influence the prevalence of flooding.  Storm water drainage is an integral part of the essential infrastructure of a modern city. In Surat, separate systems are provided for the collection and disposal of storm water and sewage. NeedforStudy
  • 18.  For study of rainfall intensity, yearly rainfall data and the 24-hour maximum rainfall data were collected from Central Water Commission (CWC) or Municipal corporation.  Rainfall intensity and duration is calculated by using India Meteorological Department (IMD) Method.  1-hour rainfall has been estimated by using 24- hours maximum rainfall, using IMD empirical reduction formula. 1-hour maximum rainfall is denoted by: Pt = P24 (t/24)1/3 where P24 = yearly 24-hour maximum rainfall Rainfall Data of Silvassa for 29 years. RainfallDatacollectionofSilvassa
  • 19.  By using Gumbel frequency distribution method, frequeny analysis of 1-hour maximum rainfall is carried out.  Graph is plotted between 1-hour maimum rainfall and Gumbel frequency factor(K).  1-hour maximum rainfall depth for different return periods of 2, 5, 10, 20, 50 and 100 year is calculated. Pt = Pm + K*s where Pt = expected 1-hour T-year rainfall depth, Pm = mean 1-hour maximum rainfall s = standard deviation of 1-hour maximum rainfall k = Gumbel frequency factor AnalysisofRainfallDatafor Silvassa
  • 20.  1-hour maximum rainfall depth is used for finding the t-minute rainfall depth for different time period such as 5, 10, 15, 30 and 120 minute.  1 hour T-year rainfall depth is multiplied by factor (taken from Journal of Indian Water Works Association, Vol-Octo-Dec- 2007 ) to obtain T minute Rainfall Depth. Frequency Analysis Using Gumbel Distribution method AnalysisofRainfallDatafor Silvassa
  • 21.  Rainfall data of different time period ranging from previous 50 year, 100 year and 120 year are obtained for Surat city.  Similar calculations is executed on these data and 1- hour maximum rainfall depth, maximum rainfall intensity and intensity duration curve is obtained. Estimation of Rainfall Intensity of Surat for 30 years. Estimation of Rainfall Intensity of Surat for 50 years. Estimation of Rainfall Intensity of Surat for 100 years. Estimation of Rainfall Intensity of Surat for 120 years. Datacollection&AnalysisforSura
  • 23.  Design of Storm Water Drainage Network for a rectangular plot of area 180 X 250 square meter has been carried out.  Reduced levels of all the nodes for the illustrative region were available.  The main line passes through the centre of the catchment area.  The runoff from other part of the catchment area flows through the sub branches which are connected to the main line. DesignofStormDrain Network
  • 24.  The frequency of storm selected was once in 2 years.  Usually, the storm drains are not designed for peak discharges or extreme events from economical point of view.  The design of the drain should be economical and at the same time it should prevent frequent flooding and it should drain out quickly. DesignofStormDrain Network
  • 25. For designing the storm water network for the given area the following data is required: 1.Catchment area 2. Rainfall intensity and duration 3. Impervious factor 4. Design of Drainage system  Rainfall Intensity and duration has been estimated using India Meteorological Department (IMD) method.  For the paved area, the impervious factor is taken as 0.7 DesignofStormDrain Network
  • 26.  Storm water runoff has been calculated by using Rational Method suggested by CPHEEO.  The diameter of pipe is selected so as to maintain the minimum velocity of 0.6 m/s and to carry slightly more discharge compared to the theoretical discharge.  The diameter of the pipe was selected to maintain a self cleansing velocity.  Moreover, the velocity of flow should not exceed more than scouring velocity. Design of Storm drain network of an illustrative region DesignofStormDrain Network
  • 27.
  • 28.  A site was visited at Godadara where drainage pipes were being laid for the removal of storm water.  The storm water has been transported to the pumping station, treated and than disposed of in to the Khadi.  Consultant : Mayur Shah, Assistant Engineer Surat Municipal Corporation. TechnicalVisit
  • 29.  The pipes which were being laid were spigot pipe of 500 mm diameter and the length of each pipe was 265 mm.  The pipes were being laid at the slope of 1:500. Generally the slope in the field is set by two methods: 1. Boning method 2.Spirit level TechnicalVisit
  • 30.
  • 31.  Analysis of Rainfall Data of 29 years for Silvassa region has been carried out. Maximum hourly intensity with a recurrence interval of 2 year is estimated to be 78 mm/hr.  The same analysis of rainfall data was carried out for Surat region:  The present study helps in computing rainfall intensity which is used to estimate storm water runoff.  The storm water runoff thus computed is very important for the design of storm drain network. Conclusion Years Intensity (mm/hr) 30 Years 56.5 50 Years 56.309 100 Years 52.87 120 Years 51.54
  • 32. Referencesand Bibliography  https://www.suratmunicipal.gov.in/TheCity/weather_annual.h tml  Central Public Health and Environment Engineering Organization manual on Sewerage and Sewage Treatment(1993), Ministry of Urban Development, New Delhi  Subramanya K (1994), Engineering Hydrology, Tata- McGraw-Hill Publishing Company Limited, New Delhi  Garg Santoshkumar (1993), Irrigation Engineering and Hydraulic Structures, Khanna Publications.  A Case Study on ' Remodelling of Bambapada Khadi, Silvassa '.  http://www.pressseal.com/Downloads/EvolutionOfWatertight StormDrainageSystemsFinal.pdf  Madhur K. Rathi and Patil Dhananjay Rajiv, " Study Of Problems and Corrective Actions of Urban Drainage Network“.
  • 33.  Dr. Lamia Abdul Jaleel and Maha Atta Farawn, " Developing Rainfall Intensity-Duration-Frequency Relationship For Basrah City "  Dr. P. G. Agnihotri, R. B. Khasiya, Priyanka D. Harpalani, “ Analysis of Rainfall Data and Design of storm Water Drainage System in an Urban Area.”  Ibrahim H. Elsebaie, “ Developing Rainfall Intensity- Duration-Frequency Realtionship For Two Regions In Saudi Arabia.”  John Argue, “ Storm Drainage Design In Small Urban Catchments: A Handbook For Australian People.”  City of Sheridan, Public Works Department, “Storm drainage Design Criteria; City of Sheridan, Wyoming”  Drainage Service Department, Government of Hong Kong, “Storm Water Drainage Manual; Planning, Design and Management.” Referencesand Bibliography
  • 34.  William S. Springer, “ Storm Drain Design”  Kwokwing Chau and C. S. Cheung, “ Knowledge Representation on Design Of Storm Drainage system.”  Minister of Urban Development, Government of India, “ Storm Water Drainage.“  Zameer Ahmed, D. Rammohan Rao, K. Ram Mohan Reddy, Ellam Raj, “Rainfall intensity Variation For Observed Data And Derived Data – A Case Study of Imphal.”  “Application of Methods For Analysis of Rainfall Intensity in Areas of Israeli, Jordanian and Palestinia Interest.”  Rezual Kabir, P. Das, “Short Duration Rainfall Estimation of Sylhet, IMD and USWD Method(2007), Journal of Indian Water Works Association.”  Ram Babu, Tejwani, K. K. Agarwal, M. C. & Bhusan, L. S. (1979) “Rainfall Intensity Period Equation and Nomograph of India, CSWCRTI, ICAR, Dehradun India.” Referencesand Bibliography