Advanced Statistical Hydrology Project: Flood Analysis in NSW
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Project
AI Summary
This project report focuses on advanced statistical hydrology, specifically analyzing flood discharge in NSW, Australia. The assignment involves analyzing annual maximum flow data from two stations using the R programming language. The core tasks include fitting four different probability distributions (Normal, EV1, P3, and GEV) to estimate the 1% AEP flood discharge, comparing these estimates with a non-parametric method, and recommending an appropriate flood discharge for the design of a bridge upstream. The report includes an introduction, literature review, methodology, results and discussion, and conclusion. The analysis involves converting data, generating graphs, and deriving equations within R. The project aims to determine the most reliable analytical or predictive model for flood discharge and recommend its use in infrastructure design, specifically bridge construction, considering the hydrological characteristics of the region. The literature review covers the impact of floods, emphasizing the need for accurate discharge predictions for effective water management and infrastructure planning.

HYDROLOGY 1
ADVANCED STATISTICAL HYDROLOGY
NAME OF STUDENT
NAME OF PROFESSOR
NAME OF CLASS
NAME OF SCHOOL
DATE
ADVANCED STATISTICAL HYDROLOGY
NAME OF STUDENT
NAME OF PROFESSOR
NAME OF CLASS
NAME OF SCHOOL
DATE
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HYDROLOGY 2
INTRODUCTION
The dealings and the focus of this report will be entirely on hydrology and the discharge
of hydrological water from the areas that are within peripheries of NSW state. Actually, the
discharge is measured in seconds and the rate of discharge is excessively high when summed up
in a year and this eventually causes floods that require frequent discharges from an area. This is
what leads to the interest in the development of this report. The assignment itself has two parts,
there will be the analysis part which will lead to the development of the report. The report is
bound to have the introductory part that is bound to have the explanations of what the whole
assignment will entail. The whole structure of the report is also bound to be explained at this
point as well.
Leaving the report structure out for a while, we will be focusing on the analysis part first.
In the analysis of the dataset that was provided for use during analysis, there is need to analyze R
over the discharge or flood flow of the hydrological water that is experienced in NSW state (a
state in Australia). There needs to predict the discharge probability of up to one per cent (1%) of
the total flood flow that is experienced. There will be a total of up to four (4) probability
distributions that are required to be explored. There will also be a no parametric method that will
surely give a probability prediction out of the probability distribution codes. After the analytical
predictions, then there will be the reported build-up. This report, therefore, will have the
introduction that carries everything that there is to be focused on but in a skeleton manner. After
the introduction, there will be a literature review of the whole methods that have been used on
analysis. There will be the methodology section that talks about methods developed in project
analysis. This will be followed by he realized results and the actual discussions of the same
results. There needs to be actual evidence and the visuals as well. After this section, what follows
INTRODUCTION
The dealings and the focus of this report will be entirely on hydrology and the discharge
of hydrological water from the areas that are within peripheries of NSW state. Actually, the
discharge is measured in seconds and the rate of discharge is excessively high when summed up
in a year and this eventually causes floods that require frequent discharges from an area. This is
what leads to the interest in the development of this report. The assignment itself has two parts,
there will be the analysis part which will lead to the development of the report. The report is
bound to have the introductory part that is bound to have the explanations of what the whole
assignment will entail. The whole structure of the report is also bound to be explained at this
point as well.
Leaving the report structure out for a while, we will be focusing on the analysis part first.
In the analysis of the dataset that was provided for use during analysis, there is need to analyze R
over the discharge or flood flow of the hydrological water that is experienced in NSW state (a
state in Australia). There needs to predict the discharge probability of up to one per cent (1%) of
the total flood flow that is experienced. There will be a total of up to four (4) probability
distributions that are required to be explored. There will also be a no parametric method that will
surely give a probability prediction out of the probability distribution codes. After the analytical
predictions, then there will be the reported build-up. This report, therefore, will have the
introduction that carries everything that there is to be focused on but in a skeleton manner. After
the introduction, there will be a literature review of the whole methods that have been used on
analysis. There will be the methodology section that talks about methods developed in project
analysis. This will be followed by he realized results and the actual discussions of the same
results. There needs to be actual evidence and the visuals as well. After this section, what follows

HYDROLOGY 3
is the conclusion which will serve as both the recommendation section as well. There will be the
recommendation made as to what analytical or predictive model should be used for being more
reliable and which ones as well do not actually do not give the best predictive results and
therefore should be dropped. The final bit will be the references section and the referencing
should be made in Harvard style and there should also be in-text citations as well. Deeply
indicated, there will also need to deeply do a heavy in-text citation on the literature review
section.
LITERATURE REVIEW
i. Hydrological Floods Overview
Flood in NSW state is something that has hit headlines of the newspapers produced by different
media houses in the state and the entire country altogether. It is a matter that has therefore proven
to be of great interest both nationally and state wise. Floods or so-called high amounts of
hydrological water discharged from the grounds in large numbers have been of great interest that
it requires the critical look in the sense that it is taken through intellectual analysis in different
levels (Clark and Hanson, 2017). Estimates can be looked into, and this can be done statistically
and after proper analysis of the hydrological related data appropriate steps can be taken. These
steps are no different from the steps that are usually being taken by the other many different
nations that do try to curb the effects of high amounts of floodwater when it pours (Hutton et al.
2016). Looking at the steps taken currently, both in Africa and the western countries at large in
order to curb flood effects, we realize that there is actually water reservoirs that are put up and
additionally proper drainage systems are also set up to help channel excess water out of the
is the conclusion which will serve as both the recommendation section as well. There will be the
recommendation made as to what analytical or predictive model should be used for being more
reliable and which ones as well do not actually do not give the best predictive results and
therefore should be dropped. The final bit will be the references section and the referencing
should be made in Harvard style and there should also be in-text citations as well. Deeply
indicated, there will also need to deeply do a heavy in-text citation on the literature review
section.
LITERATURE REVIEW
i. Hydrological Floods Overview
Flood in NSW state is something that has hit headlines of the newspapers produced by different
media houses in the state and the entire country altogether. It is a matter that has therefore proven
to be of great interest both nationally and state wise. Floods or so-called high amounts of
hydrological water discharged from the grounds in large numbers have been of great interest that
it requires the critical look in the sense that it is taken through intellectual analysis in different
levels (Clark and Hanson, 2017). Estimates can be looked into, and this can be done statistically
and after proper analysis of the hydrological related data appropriate steps can be taken. These
steps are no different from the steps that are usually being taken by the other many different
nations that do try to curb the effects of high amounts of floodwater when it pours (Hutton et al.
2016). Looking at the steps taken currently, both in Africa and the western countries at large in
order to curb flood effects, we realize that there is actually water reservoirs that are put up and
additionally proper drainage systems are also set up to help channel excess water out of the
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HYDROLOGY 4
whole area that if not checked would experience full dose effects of the actual downpour that
leads to flooding. Looking at the dataset that has been provided and taking the average which is
above 200 m3/s (Montanari, 2015). This is a very high amount of discharge of hydrological water
if now summed up into an hour's downpour of rain, if the same amount of discharge was almost
the same amount of pour with the little amount being absorbed by the soil, then there can be
adverse effects if matters are largely not taken into account. Imagine there were no proper
drainage systems, reservoirs were not raised to actually aid in the hold up of excess water, and
therefore water were to stagnate at the same point for a long time, this would definitely cause
very many effects to the lives and the comfort of those that actually live in the areas that
experience the actual flood flows due to high amount of waters that are supposed to be
discharged and yet are actually not discharged (Bolch, 2017).
Look for example, at other parts of the content and in other continents as well for
example in Asia, Africa and South America as well, some deaths are related to high amounts of
stagnation of the downpour that is meant to be discharged. We have to look at how high amounts
of hydrological water from the rains, if not discharged as fast as expected, actually affect the
lives of people in a space that this occurs (Liljedahl et al. 2016). To begin with, high amounts of
water expected to be discharged, if stagnated at one point for a longer time, may block paths and
there is no way an individual can know which part of the path that they are using is safe to use.
take for example a driver of a car driving along a road which was being rectified during the dry
sessions maybe during the da. If this person was not aware of the fact that there were sections of
the road that required slow spend, actual precision and change of lanes, then this individual is
bound to drive directly into an unsafe space and maybe to a fatal trap (Flowers, 2018). This is
whole area that if not checked would experience full dose effects of the actual downpour that
leads to flooding. Looking at the dataset that has been provided and taking the average which is
above 200 m3/s (Montanari, 2015). This is a very high amount of discharge of hydrological water
if now summed up into an hour's downpour of rain, if the same amount of discharge was almost
the same amount of pour with the little amount being absorbed by the soil, then there can be
adverse effects if matters are largely not taken into account. Imagine there were no proper
drainage systems, reservoirs were not raised to actually aid in the hold up of excess water, and
therefore water were to stagnate at the same point for a long time, this would definitely cause
very many effects to the lives and the comfort of those that actually live in the areas that
experience the actual flood flows due to high amount of waters that are supposed to be
discharged and yet are actually not discharged (Bolch, 2017).
Look for example, at other parts of the content and in other continents as well for
example in Asia, Africa and South America as well, some deaths are related to high amounts of
stagnation of the downpour that is meant to be discharged. We have to look at how high amounts
of hydrological water from the rains, if not discharged as fast as expected, actually affect the
lives of people in a space that this occurs (Liljedahl et al. 2016). To begin with, high amounts of
water expected to be discharged, if stagnated at one point for a longer time, may block paths and
there is no way an individual can know which part of the path that they are using is safe to use.
take for example a driver of a car driving along a road which was being rectified during the dry
sessions maybe during the da. If this person was not aware of the fact that there were sections of
the road that required slow spend, actual precision and change of lanes, then this individual is
bound to drive directly into an unsafe space and maybe to a fatal trap (Flowers, 2018). This is
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HYDROLOGY 5
why there is a need for proper drainage systems which help in getting read of excess
hydrological water that needs to be gotten rid of overtime.
A second case of how lives are affected when water is not precipitated or discharged off the
ground as fast as required is there can be causes of deceases. Stagnated water on the ground or
too much water that is not flowing forms breeding ground for; mosquitoes, snakes, snails and
along with that it makes the soil poorer for farming as soil only requires very little amounts of
water to aid with the growth of plants. Lack of discharge or precipitation will ensure venomous
snakes that survive in water the time to get the chance to and a breading space. This alone proves
to be detrimental to the lives of the locals as most snakes bite to kill (Loucks, 2015). The
mosquitoes without a doubt, have a real breeding ground when the large amounts of hydrological
water are not discharged as wished. Excess breeding grounds for the mosquitoes give an excess
of mosquitoes and this can cause deaths as mosquitoes spread malaria at a high rate. There can
actually be the spread of bilharzia from snails as well as snails love the feel of water and I if
there is in excess of that in stagnation then there can be a really conducive space for them to
bread and therefore lives, by extension can be affected in the ways mentioned above, among
others though, that actually can be discussed in details in a more elaborate literature (Eslamian,
2018).
ii. Discharge from the station
From the assignment's specifications, there is a need for us to offer a recommendation on
the appropriate flood discharge processes from the actual results that will be gotten from the
analysis. The station is a question here, from the assignment details is Station 204017 at
Bielsdown Creek at Dorrigo number 2 and number 3. This is an indication that there were two
stations to be taken into account during consideration. The stations are adjacent to one another
why there is a need for proper drainage systems which help in getting read of excess
hydrological water that needs to be gotten rid of overtime.
A second case of how lives are affected when water is not precipitated or discharged off the
ground as fast as required is there can be causes of deceases. Stagnated water on the ground or
too much water that is not flowing forms breeding ground for; mosquitoes, snakes, snails and
along with that it makes the soil poorer for farming as soil only requires very little amounts of
water to aid with the growth of plants. Lack of discharge or precipitation will ensure venomous
snakes that survive in water the time to get the chance to and a breading space. This alone proves
to be detrimental to the lives of the locals as most snakes bite to kill (Loucks, 2015). The
mosquitoes without a doubt, have a real breeding ground when the large amounts of hydrological
water are not discharged as wished. Excess breeding grounds for the mosquitoes give an excess
of mosquitoes and this can cause deaths as mosquitoes spread malaria at a high rate. There can
actually be the spread of bilharzia from snails as well as snails love the feel of water and I if
there is in excess of that in stagnation then there can be a really conducive space for them to
bread and therefore lives, by extension can be affected in the ways mentioned above, among
others though, that actually can be discussed in details in a more elaborate literature (Eslamian,
2018).
ii. Discharge from the station
From the assignment's specifications, there is a need for us to offer a recommendation on
the appropriate flood discharge processes from the actual results that will be gotten from the
analysis. The station is a question here, from the assignment details is Station 204017 at
Bielsdown Creek at Dorrigo number 2 and number 3. This is an indication that there were two
stations to be taken into account during consideration. The stations are adjacent to one another

HYDROLOGY 6
and therefore experience the same level of discharge problem as the level of hydrological
circulation that one station experiences are the same level as the other. this one translates into the
stations having one and only one mega drainage system that seeks to expel or discharge
floodwater out of both the stations, having been adjacent to one another. There are
recommendations on using the data that has been derived from the analysis to aid in the design of
a bridge up the stream. What this translates to is that these are the weather of electric supply
stations and requires something like a dam that can hold more water upstream. This conclusion
though cannot be reached until an actual analysis that is needed to be carried out is effected on R,
the required platform.
iii. Methods used
In this section, there will be a discussion on what analytical methods to use as given in all
the roman numbers of the requirements of the assignment. Since the analysis is to be done in R
software, there needs to be actual copying of the data dataset that has been provided into a CSV
file from the pdf file that contains the assignment as R does not accept files in pdf formats. So
initially, they will be taken in an excel format and then later changed into a CSV format, which is
comma-delimited and can be opened in notepad to get the fact that it is a comma-delimited file
format. The example of the vie of the dataset as a CSV format in notepad is as below;
and therefore experience the same level of discharge problem as the level of hydrological
circulation that one station experiences are the same level as the other. this one translates into the
stations having one and only one mega drainage system that seeks to expel or discharge
floodwater out of both the stations, having been adjacent to one another. There are
recommendations on using the data that has been derived from the analysis to aid in the design of
a bridge up the stream. What this translates to is that these are the weather of electric supply
stations and requires something like a dam that can hold more water upstream. This conclusion
though cannot be reached until an actual analysis that is needed to be carried out is effected on R,
the required platform.
iii. Methods used
In this section, there will be a discussion on what analytical methods to use as given in all
the roman numbers of the requirements of the assignment. Since the analysis is to be done in R
software, there needs to be actual copying of the data dataset that has been provided into a CSV
file from the pdf file that contains the assignment as R does not accept files in pdf formats. So
initially, they will be taken in an excel format and then later changed into a CSV format, which is
comma-delimited and can be opened in notepad to get the fact that it is a comma-delimited file
format. The example of the vie of the dataset as a CSV format in notepad is as below;
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HYDROLOGY 7
As can be seen from the above diagram it is evident that the dataset has commas in each and
case. It is only noted pad that brings out the ideal structure of the dataset that is to be used.
Notepad as well can be used to save codes from R for presentation to someone who does not
have R software to view and run the codes to get results (Giner and Smyth, 2016).
There will be graphs produced which must be displayed in the methodology section, there are
equations that will be derived, written as per the code rules o R and all that will be displayed in R
altogether. R studio is the best version of R for use as it contains four windows, the first window
is the code writing window where actually, the codes that give results are written under. What
this means is there a window called the console window that runs the codes that are written in
them. There is an additional window that contains all the history of the codes that are written in
R. There is the environment window that gives the return of what is run but in a skeleton aspect.
The final window is the plots, files, packages, help, viewer tabs window. Using the packages tab,
libraries can be installed. Using the plots tab one can view the plots generated by the developed
plot codes. Help tab allows for actual help on what most R documents mean (Riviello et al.
2016).
After knowing how R works, it is only important to have an actual discussion of what has been
asked to be the basis of analysis in the requirements of the assignment. There is a need to analyze
while predicting the occurrence of 1% of the total discharge. This is to be done through some
probability distribution. Before we look at the probability distributions, there will need to have a
look into each probability distribution and explain what they mean in words. The very first
probability distribution to be looked into will be the normal probability distribution ad this is the
simplest probability distribution to get to understand (McElreath, 2018).
As can be seen from the above diagram it is evident that the dataset has commas in each and
case. It is only noted pad that brings out the ideal structure of the dataset that is to be used.
Notepad as well can be used to save codes from R for presentation to someone who does not
have R software to view and run the codes to get results (Giner and Smyth, 2016).
There will be graphs produced which must be displayed in the methodology section, there are
equations that will be derived, written as per the code rules o R and all that will be displayed in R
altogether. R studio is the best version of R for use as it contains four windows, the first window
is the code writing window where actually, the codes that give results are written under. What
this means is there a window called the console window that runs the codes that are written in
them. There is an additional window that contains all the history of the codes that are written in
R. There is the environment window that gives the return of what is run but in a skeleton aspect.
The final window is the plots, files, packages, help, viewer tabs window. Using the packages tab,
libraries can be installed. Using the plots tab one can view the plots generated by the developed
plot codes. Help tab allows for actual help on what most R documents mean (Riviello et al.
2016).
After knowing how R works, it is only important to have an actual discussion of what has been
asked to be the basis of analysis in the requirements of the assignment. There is a need to analyze
while predicting the occurrence of 1% of the total discharge. This is to be done through some
probability distribution. Before we look at the probability distributions, there will need to have a
look into each probability distribution and explain what they mean in words. The very first
probability distribution to be looked into will be the normal probability distribution ad this is the
simplest probability distribution to get to understand (McElreath, 2018).
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HYDROLOGY 8
From the illustrative phone above, we have a normal curve, representing a normal distribution,
the distribution under the curve is continuous and moves from negative infinity to positive
infinity. The total area under the curve is supposed to be equal to 1 as this is a probability
distribution ranging from zero (0) to one (1). Z on the graph represents the independent values
that are fed in the actual function to get the probability results represented by f(Z) (Faraway,
2016).
Moving progressively, we get to the EV1 probability distribution which in full is Extreme
value type 1 distribution. Extreme value type 1 distribution is of two types actually, the smallest
extreme and the largest extreme and they are both referred to as minimum and the maximum
cases respectively. Another reference of the EV1 is Gumbel distribution. There are several
functions under this distribution and just in listings they will be; Cumulative Distribution
Function, Percent Point Function, Hazard Function, Cumulative Hazard Function, Survival
Function and Inverse Survival Function (Benson, Ransohoff and Huang, 2017).
The next distribution which we will be looking at will be the P3 distribution which is called the
is largely based on whether a variable is random or non-random. It depends on the type of
From the illustrative phone above, we have a normal curve, representing a normal distribution,
the distribution under the curve is continuous and moves from negative infinity to positive
infinity. The total area under the curve is supposed to be equal to 1 as this is a probability
distribution ranging from zero (0) to one (1). Z on the graph represents the independent values
that are fed in the actual function to get the probability results represented by f(Z) (Faraway,
2016).
Moving progressively, we get to the EV1 probability distribution which in full is Extreme
value type 1 distribution. Extreme value type 1 distribution is of two types actually, the smallest
extreme and the largest extreme and they are both referred to as minimum and the maximum
cases respectively. Another reference of the EV1 is Gumbel distribution. There are several
functions under this distribution and just in listings they will be; Cumulative Distribution
Function, Percent Point Function, Hazard Function, Cumulative Hazard Function, Survival
Function and Inverse Survival Function (Benson, Ransohoff and Huang, 2017).
The next distribution which we will be looking at will be the P3 distribution which is called the
is largely based on whether a variable is random or non-random. It depends on the type of

HYDROLOGY 9
variability of study. All the other illustrative instances will be looked at when running the actual
analysis in R studio itself.
GEV in full, goes by the name, General extreme value and is a family of a continuous
probability distribution. They are developed under extreme value theory to combine Gumbel,
Frechet, Weibull families also known as type I, II and III extreme value distributions. In other
cases, this distribution is known as Fisher-Tippet distribution. This is a naming derived from the
names Ronald Fisher and L. H. C Tippet. This distribution proves only to be the only possible
limit distribution of properly normalized maxima of a sequence where variables are distributed
randomly in an identical manner and are also independent. There is no need for any limit
distribution to existing at all (Garvey, Book and Covert, 2016).
In the second requirement of the assignment, there is a need to focus on a non-parametric
method of analyzing to help make a non-parametric prediction on the 1% of discharge that is
required to be made. The non-parametric method for use, in this case, will be the non-parametric
regression, which is a regression but can only make predictions when one numeric dependent
variable is applied. There should be no integer and no constants (Taylor et al. 2018).
Finally, there will be a recommendation on the actual recommendations made as per the
derivation that is made from the analysis itself, whether a bridge, a dam, a proper and elaborate
drainage system should be constructed. This will be looked at in different angle as the stations
geographical area must be taken into account. Different measures must be taken due to them that
there might be discrepancies in the geographical alignment of the areas that are surrounding the
stations that are under study (Delignette-Muller and Dutang, 2015).
variability of study. All the other illustrative instances will be looked at when running the actual
analysis in R studio itself.
GEV in full, goes by the name, General extreme value and is a family of a continuous
probability distribution. They are developed under extreme value theory to combine Gumbel,
Frechet, Weibull families also known as type I, II and III extreme value distributions. In other
cases, this distribution is known as Fisher-Tippet distribution. This is a naming derived from the
names Ronald Fisher and L. H. C Tippet. This distribution proves only to be the only possible
limit distribution of properly normalized maxima of a sequence where variables are distributed
randomly in an identical manner and are also independent. There is no need for any limit
distribution to existing at all (Garvey, Book and Covert, 2016).
In the second requirement of the assignment, there is a need to focus on a non-parametric
method of analyzing to help make a non-parametric prediction on the 1% of discharge that is
required to be made. The non-parametric method for use, in this case, will be the non-parametric
regression, which is a regression but can only make predictions when one numeric dependent
variable is applied. There should be no integer and no constants (Taylor et al. 2018).
Finally, there will be a recommendation on the actual recommendations made as per the
derivation that is made from the analysis itself, whether a bridge, a dam, a proper and elaborate
drainage system should be constructed. This will be looked at in different angle as the stations
geographical area must be taken into account. Different measures must be taken due to them that
there might be discrepancies in the geographical alignment of the areas that are surrounding the
stations that are under study (Delignette-Muller and Dutang, 2015).
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HYDROLOGY 10
METHODOLOGY
This is the methodology section where all the codes as required to be typed using the
equation editor. What is most important and that must be taken into consideration is that the
assignment that is to be carried out has its analysis in R. Therefore, the pen and paper way of
writing the required equations will not be applicable in this case at all. The kind of equations that
will be written will be based on the format that R provides (Kopp et al. 2017). To get a recap of
the methods used at an introductory level, please get a recap at the last sub-section (methods
used) of the second section (Literature review). In the second section, the last subsection all the
four probability sections that are required to be used including the final analytic level, the non-
parametric method, there needs to be a clear illustration on the results and the methods and how
they unroll out themselves (McElreath, 2018). There will be a clear comparison of the
probability estimates from the probability distribution methods that will be employed.
Taking a recap in this paragraph there will be consideration of these four probability
methods, we note that we will be starting with the binomial probability distribution, which has a
normal distribution graph that is plotted for the same. The area under the graph is totalling up to
1. Probability values range from zero (0) to one (1) and that is where the summation gets to 1.
The next is the EV1, the extreme value distribution of type 1 which is of two types. The
minimum and maximum extreme levels of distributions. The EV1 has several functions that are
tied up to it and depends on the functions that are run from time to time (Hsiang at al. 2017).
Therefore, a scientist is bound to make proper and informed decisions when it comes to the
choice of extreme value for type 1 distribution that is intended for use. Then there is the P3
distribution and then there is the GEV probability distribution, which is a General value extreme
value, that consists of a group of continuous probability distributions. In the final list of the
METHODOLOGY
This is the methodology section where all the codes as required to be typed using the
equation editor. What is most important and that must be taken into consideration is that the
assignment that is to be carried out has its analysis in R. Therefore, the pen and paper way of
writing the required equations will not be applicable in this case at all. The kind of equations that
will be written will be based on the format that R provides (Kopp et al. 2017). To get a recap of
the methods used at an introductory level, please get a recap at the last sub-section (methods
used) of the second section (Literature review). In the second section, the last subsection all the
four probability sections that are required to be used including the final analytic level, the non-
parametric method, there needs to be a clear illustration on the results and the methods and how
they unroll out themselves (McElreath, 2018). There will be a clear comparison of the
probability estimates from the probability distribution methods that will be employed.
Taking a recap in this paragraph there will be consideration of these four probability
methods, we note that we will be starting with the binomial probability distribution, which has a
normal distribution graph that is plotted for the same. The area under the graph is totalling up to
1. Probability values range from zero (0) to one (1) and that is where the summation gets to 1.
The next is the EV1, the extreme value distribution of type 1 which is of two types. The
minimum and maximum extreme levels of distributions. The EV1 has several functions that are
tied up to it and depends on the functions that are run from time to time (Hsiang at al. 2017).
Therefore, a scientist is bound to make proper and informed decisions when it comes to the
choice of extreme value for type 1 distribution that is intended for use. Then there is the P3
distribution and then there is the GEV probability distribution, which is a General value extreme
value, that consists of a group of continuous probability distributions. In the final list of the
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HYDROLOGY 11
algorithms that are run, will be the non-numeric list and this will have it R code equations written
at the last (Hensen et al. 2016).
i. Actual R Codes and Equations of the Probability Distributions
a. Normal Probability Distribution
The original equation as per the pen and paper without considering the part of the code;
y= ( 1
σ ❑
√2 π )e¿
)² )/2σ²)).
b. EV1 (Extreme Value Probability Distribution of Type 1
f ( x )= ( 1
β )e ( x−μ
β )e (−e ( x−μ
β ))
c. GEV (Greatest Extreme Value Probability Distribution)
y=¿σ)t(𝓍)^(έ+1)e(-t(x)).
From the above, there is an actual listing of the actual probability distribution equation and are
listed in number sequentially. The next section will now be focusing largely on the application of
these equations in R codes.
RESULTS AND DISCUSSION
This will be the most interesting part of the whole report at this forms the major part of
the whole of the report. This is the section where the estimates that are supposed to be made are
made. The software that we have chosen for use in making the estimates will be R and this is
where the probabilistic distribution predictions will be made. All the codes that do give the
algorithms that are run, will be the non-numeric list and this will have it R code equations written
at the last (Hensen et al. 2016).
i. Actual R Codes and Equations of the Probability Distributions
a. Normal Probability Distribution
The original equation as per the pen and paper without considering the part of the code;
y= ( 1
σ ❑
√2 π )e¿
)² )/2σ²)).
b. EV1 (Extreme Value Probability Distribution of Type 1
f ( x )= ( 1
β )e ( x−μ
β )e (−e ( x−μ
β ))
c. GEV (Greatest Extreme Value Probability Distribution)
y=¿σ)t(𝓍)^(έ+1)e(-t(x)).
From the above, there is an actual listing of the actual probability distribution equation and are
listed in number sequentially. The next section will now be focusing largely on the application of
these equations in R codes.
RESULTS AND DISCUSSION
This will be the most interesting part of the whole report at this forms the major part of
the whole of the report. This is the section where the estimates that are supposed to be made are
made. The software that we have chosen for use in making the estimates will be R and this is
where the probabilistic distribution predictions will be made. All the codes that do give the

HYDROLOGY 12
relevant estimates in terms of probability of the 1% of discharge that is required will all be
written here and the results will be gotten from the console or the results view. In the previous
section, there was the listing of the equations of the relative probabilistic distributions but in this
section, the actual case will be different as there will be no listing of the equations but the major
focus will be entirely on R software (Hoyos, Morales and Akhavan-Tabatabaei, 2015).
Critically turning back and looking at R, it was talking about in an earlier section but there will
need to dig deeper in this case as well. The twist of looking at it will be a bit different as
compared to the earlier section. R, as it is known, is a statistical software build by statisticians for
a statistician to aid them with their statistical analysis and purposes. This software has been in
the topnotch arena of statistical tools for a very long time. This was before other competitive
statistical software like python came up (Thisted, 2017). A python is multipurpose software that
allows app, website, different system development as well as statistical analysis. The tools that
are used for and statistical analysis and in statistical analysis using python are Spyders and
Jupiter notebook. Rubi as well offers some level of competition to R but because Rubi is not so
much known, this puts R ahead of Rubi as a statistical software for analysis. On the other hand,
though python as statistical analysis software, is still ahead of R. reason for this is because it was
realized that python had a better interface for users that R, a better outlook and more attractive
that R itself. Its interface as well is very easy to handle. The only reason as to why R still comes
on top is the fact that there is the fact that R has more libraries tied to its operation. There are
more elaborative languages that can aid in the development analytical codes that are more
elaborative as opposed to the ones that are found in the other platforms (Tüselmann, Sinkovics
and Pishchulov, 2016). The arrival is the analytical results being sorted for is always way faster
as opposed to like in the cases of other software. Libraries found and used for R, are bulkier and
relevant estimates in terms of probability of the 1% of discharge that is required will all be
written here and the results will be gotten from the console or the results view. In the previous
section, there was the listing of the equations of the relative probabilistic distributions but in this
section, the actual case will be different as there will be no listing of the equations but the major
focus will be entirely on R software (Hoyos, Morales and Akhavan-Tabatabaei, 2015).
Critically turning back and looking at R, it was talking about in an earlier section but there will
need to dig deeper in this case as well. The twist of looking at it will be a bit different as
compared to the earlier section. R, as it is known, is a statistical software build by statisticians for
a statistician to aid them with their statistical analysis and purposes. This software has been in
the topnotch arena of statistical tools for a very long time. This was before other competitive
statistical software like python came up (Thisted, 2017). A python is multipurpose software that
allows app, website, different system development as well as statistical analysis. The tools that
are used for and statistical analysis and in statistical analysis using python are Spyders and
Jupiter notebook. Rubi as well offers some level of competition to R but because Rubi is not so
much known, this puts R ahead of Rubi as a statistical software for analysis. On the other hand,
though python as statistical analysis software, is still ahead of R. reason for this is because it was
realized that python had a better interface for users that R, a better outlook and more attractive
that R itself. Its interface as well is very easy to handle. The only reason as to why R still comes
on top is the fact that there is the fact that R has more libraries tied to its operation. There are
more elaborative languages that can aid in the development analytical codes that are more
elaborative as opposed to the ones that are found in the other platforms (Tüselmann, Sinkovics
and Pishchulov, 2016). The arrival is the analytical results being sorted for is always way faster
as opposed to like in the cases of other software. Libraries found and used for R, are bulkier and
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