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POWER DISTRIBUTION RELIABILITY AS A FUNCTION OF WEATHER By ROOP KISHORE R. MATAVALAM A THESIS PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE UNIVERSITY OF FLORIDA 2004

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POWER DISTRIBUTION RELIABILITY AS A FUNCTION OF WEATHER

By

ROOP KISHORE R. MATAVALAM

A THESIS PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT

OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE

UNIVERSITY OF FLORIDA

2004

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Copyright 2004

By

Roop Kishore R. Matavalam

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To my parents and my sister

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ACKNOWLEDGMENTS

First and foremost, I thank my advisor, Dr. Alexander Domijan, for having

confidence in me and allowing me to pursue this research. The work presented in this

thesis would not be possible without his consistent support. I am also very thankful to Dr.

Khai D.T. Ngo and Dr. Antonio A. Arroyo for serving as committee members in my

thesis.

I sincerely express my gratitude to my colleague and friend William S. Wilcox for

his thorough discussions in statistics and suggestions, without which the current thesis

would not have been exciting. I am also grateful to my colleague and friend Alejandro

Montenegro for his suggestions and answers to my questions without any hesitation.

I am also very grateful to my friend Raj Vignesh Thogulua for helping me in

understanding the neural networks. I am also thankful to Dr. Tao Lin for his helpful

suggestions. I also thank my fellow colleague and friend Ajay Karthik for being

enthusiastic about my work.

I would like to express my special thanks to all the personnel of FPL Distribution

Reliability group especially Mr. J. R. “Pepe” Diaz, Ms. Lee Davis and Ms. Jessica

D’Agostini for their valuable suggestions and financial support of this project, without

their consistent support the current project would not have been finished. I am also

thankful to FPL members including Mr. Val Miklausich, Mr. Santiageo Cocina, Mr. Luis

Delforn, Mr. Manny Miranda, and Ms. Martha Caneia for their assistance.

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I would like to express my gratitude to all the undergraduate students who worked

in FPL project and made it more lively and interesting. I also extend my gratitude to all

my great friends for their support and encouragement.

Finally, yet most importantly, I am indebted to my wonderful parents and sister for

believing in my goals, aspirations, for their love, encouragement, and constant support in

all my endeavors.

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TABLE OF CONTENTS page ACKNOWLEDGMENTS ................................................................................................. iv

LIST OF TABLES........................................................................................................... viii

LIST OF FIGURES ........................................................................................................... ix

ABSTRACT....................................................................................................................... xi

CHAPTER 1 INTRODUCTION ........................................................................................................1

1.1 Importance of Power Reliability.............................................................................2 1.2 Understanding Power Reliability Indices ...............................................................3 1.3 Purpose and Importance of this Thesis...................................................................5 1.4 Organization of Thesis............................................................................................6

2 UNDERSTANDING FLORIDA WEATHER .............................................................8

2.1 Air Density, Temperature and Pressure..................................................................8 2.2 Humidity .................................................................................................................8 2.3 Rain.........................................................................................................................8 2.4 Dew or Condensation of the Humidity...................................................................9 2.5 Pollution..................................................................................................................9 2.6 Wind .....................................................................................................................10 2.7 Lightning...............................................................................................................12

3 SYSTEM UNDER STUDY – FPL.............................................................................15

3.1 Description of the FPL distribution system..........................................................15 3.2 Interruption Data from FPL ..................................................................................17 3.3 Meteorological Weather Data from NCDC..........................................................22 3.4 Weather Parameters of interest .............................................................................23

4 CORRELATION OF WEATHER AND INTERRUPTIONS ...................................25

4.1 Importance of Statistical Tools.............................................................................26 4.2 Probabilistic Characteristics of Data Distributions...............................................27 4.3 Correlation Analysis between Weather Parameters and Interruptions .................29

4.3.1 Impact of Temperature on N ......................................................................29 4.3.2 Impact of Wind on N..................................................................................34 4.3.3 Impact of Rain on N ...................................................................................35 4.3.4 Effect of Rain and Wind Together on N ....................................................37

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5 PREDICTION OF INTERRUPTIONS USING ARTIFICIAL NEURAL NETWORKS ..............................................................................................................40

5.1 Introduction to Artificial Neural Networks ..........................................................40 5.1.1 Benefits of ANNS over statistical methods................................................41 5.1.2 Architecture of ANN ..................................................................................41 5.1.3 Functioning of ANN...................................................................................43 5.1.4 Back Propagation Learning Rule................................................................44

5.2 Steps to Enhance the performance of ANN..........................................................45 5.3 ANN Simulation Output .......................................................................................47

5.3.1 Detailed Observation ..................................................................................48 5.3.2 Dominant Weather Parameters - Preliminary Observations ......................51

5.4 Analysis of ANN Simulation Output....................................................................51 5.5 Pitfalls and Suggestions to FPL............................................................................53

5.5.1 Weather Data ..............................................................................................53 5.5.2 Interruption Data ........................................................................................53

5.6 Proving Localization of Weather Improves the Accuracy in Prediction..............56 Case 1: Localized Weather Data .........................................................................56 Case 2: Scattered Weather Data ..........................................................................57

5.7 Comparison of Statistical Model and ANN Model ..............................................57 5.8 Possible Software Development to Predict Power Interruptions Using ANNs....58

6 LIMITATIONS, CONCLUSIONS AND FUTURE WORK .....................................62

6.1 Limitations of Approach.......................................................................................62 6.1.1 Weather Data ..............................................................................................62 6.1.2 Unknown Variables ....................................................................................63 6.1.3 Outliers .......................................................................................................64 6.1.4 Hourly Data ................................................................................................64

6.2 Conclusions...........................................................................................................64 6.3 Future Work..........................................................................................................65

6.3.1 Data Collection and Creating New Variables ............................................66 6.3.2 Improving the Accuracy and Developing New ANN Models ...................66

LIST OF REFERENCES...................................................................................................67

BIOGRAPHICAL SKETCH .............................................................................................69

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LIST OF TABLES

Table page 2-1 Type of Contaminant and Atmospheric Conditions at the Time of

Contamination Flashover (UHV Project).................................................................10

3-1 FPL Power Sales by Sectors.....................................................................................15

3-2 FPL Distribution Management Areas along with Their Dispatch Centers ..............16

3-3 FPL Cause Codes (102) Table .................................................................................18

4-1 The Frequency of Interruptions due to Tree Limbs (Cause Codes 20 & 21)...........27

4-2 Prediction of N Using Maximum Temperature of All the MAs ..............................33

5-1 Summary Table of Covariance for All the Input Variables Considered in the Principle Component Analysis.................................................................................46

5-2 Performance Comparison Between Statistical Model and ANN Model..................57

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LIST OF FIGURES

Figure page 2-1 Regions with strong contamination (UHV project) ...................................................9

2-2 Swing angle as a function of instantaneous wind speed at tower ............................11

2-3 Vegetation effects on power interruptions ...............................................................12

2-4 Number of days with thunderstorms in Florida (US Weather Bureau)....................13

2-5 Cumulative frequency distribution of peak current amplitudes in downward negative flashes ..................................................................................14

3-1 Snap shot of Florida map .........................................................................................17

3-2 FPL’s historical SAIFI performance ........................................................................20

3-3 Frequency charts of interruptions and customers affected by interruptions .............................................................................................................21

4-1 N for all management areas from 1998 to 2001 using the previous filters.........................................................................................................................28

4-2 Rain (inches) for all management areas from 1998 to 2001 ....................................28

4-3 Wind-2 minutes maximum speed (mph) for all management areas from 1998 to 2001 ....................................................................................................29

4-4 Variation of average N due to transformer failures vs. maximum temperature...............................................................................................................30

4-5 Variation of average N due to transformer failures vs. maximum temperature (averaged per month per year) .............................................................31

4-6 Variation of average N due to transformer failures vs. max temperature (averaged per month) ...........................................................................32

4-7 Variation of N vs. wind ............................................................................................34

4-8 Mean of 2 minutes wind speed vs. average number of interruptions.......................35

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4-9 Variation of N vs. rain..............................................................................................36

4-10 Variation of N vs. rain in the interval [0 2] ..............................................................37

4-11 Impact of rain and wind together on N.....................................................................38

5-1 ANN structures.........................................................................................................42

5-2 A back propagation ANN model ............................................................................45

5-3 Prediction patterns of N overlaid on actual patterns of N of 3 MAs for year 2002..........................................................................................................................48

5-4 Predicted N and the actual N for a few of the cases in North Dade MA for 2002...49

5-5 Numerical values of weather and interruption data under consideration.................50

5-6 Histogram plot of predicted interruptions ................................................................52

5-7 Prediction results of ANN using the original N (not shift adjusted) ........................54

5-8 Prediction results of ANN using the adjusted N (shift adjusted) .............................55

5-9 Mean and standard deviation of actual N.................................................................55

5-10 Mean and standard deviation of adjusted N .............................................................55

5-11 Mean squared error vs. training epochs ...................................................................58

5-12 Graphical user interface developed to predicted interruptions................................59

5-13 Predicted interruptions vs. actual interruptions for Central Dade ............................61

6-1 Average precipitation difference ..............................................................................63

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Abstract of Thesis Presented to the Graduate School of the University of Florida in Partial Fulfillment of the

Requirements for the Degree of Master of Science

POWER DISTRIBUTION RELIABILITY AS A FUNCTION OF WEATHER

By

Roop Kishore R Matavalam

August 2004

Chair: Alexander Domijan, Jr. Major Department: Electrical and Computer Engineering

The system principles that are used to design and maintain electric power

distribution grids (distinct from transmission grids) are intended to minimize the number

and duration of power disturbances, including interruptions. Many of these principles,

such as load flow and load prediction are well understood and have been refined over

many years. However, the impact of local weather conditions on power distribution grids

has not been well researched. The current thesis is intended to improve our understanding

of the effects of weather on power distribution systems and to develop tools for the

prediction of weather related interruptions. Developing and disseminating this

information will allow electric power engineers to ultimately improve our nation’s power

distribution capabilities.

The current research also presents the novel concept of predicting the number of

power interruptions in a distribution system using weather parameters. Preliminary

results show that it is possible to define and build a model, using artificial neural

networks (ANNs), which can use weather parameters as inputs and predict the number of

xi

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interruptions with reasonable accuracy. The accuracy of the prediction depends, in part,

on the accuracy of the weather data that are used in the model and, in part, on the

precision of the model. It is expected that the use of real-time surface weather data, such

as can be collected from well-sited weather stations, will eliminate the uncertainty

inherent in weather data collected from geographically distant sources.

xii

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CHAPTER 1 INTRODUCTION

For any power company, providing reliable electric service is the number-one

priority. But unfortunately, sometimes, power interruptions are simply unavoidable. The

contribution of weather towards these power interruptions is significant, as it is going to

be shown in this thesis. Often times the terms – power outages and power interruptions

are exchanged each other to mean the same -- loss of power supply, even by many people

in power industry. But there is a fine difference between these two terms as stated by the

IEEE 1366 standard [1]:

An outage is defined in IEEE 1366-2001 as:

The state of a component when it is not available to perform its intended function due to some event directly associated with that component. Notes: (1) An outage may or may not cause an interruption of service to customers, depending on system configuration. (2) This definition derives from transmission and distribution applications and does not apply to generation outages.

An interruption is defined in IEEE 1366-2001 as: The loss of service to one or more customers connected to the distribution portion of the system. Note: It is the result of one or more component outages, depending on system configuration.

From FPL standards, the loss of power supply is defined in two ways based on the

duration of the power disturbance to the customer:

• Momentary Interruption: Single operation (Open – Close) of an

interrupting device which results in zero voltage for a period of time of 59

seconds or less.

1

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• Sustained Interruption: Power loss to the customer that has lasted at least

for one minute.

Note: In the current thesis, when we say interruptions we mean sustained interruptions.

Also we use N to represent the total number of sustained interruption per day.

1.1 Importance of Power Reliability

Because of the huge financial losses, besides customer satisfaction loss, associated

with power interruptions to our economy, power reliability is one of the most important

concerns for electric utilities. Power reliability modeling and indexing are among the

tools used by utilities to manage costs and monitor equipment performance, and

ultimately improvements in the flexibility of reliability assessment models will result in

increased savings. According to Contingency Planning Research Company’s annual

study [2], downtime caused by power disturbances result in major financial losses as

shown in Figure 1-1.

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Figure 1-1. Average hourly impact of downtime and data loss by business sector

Traditionally the reliability of an electric distribution system is measured in terms

of total number of power interruptions occurred.

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Currently there are a variety of indices available to measure the reliability of any

power utility. These indices are used as a yard stick within a utility to see how good they

are doing each year besides serving as a better tool to compare their relative performance

with the other utilities, of different sizes, in the country.

1.2 Understanding Power Reliability Indices

Among many power distribution reliability indices available [3], the following are

some of the widely used customer based indices:

SAIFI: System average interruption frequency index (sustained interruptions). This index

is designed to give information about the average of sustained interruptions per customer

over a predefined area. In words, the definition is

SAIFI = Total number of customer interruptonsTotal number of customers served

Mathematically it is represented as

SAIFI = i

T

NN∑

SAIDI: System average interruption duration index. This index is commonly referred to as

customer minutes of interruption or customer hours, and is designed to provide

information about the average time the customers are interrupted.

SAIDI = Customer interruption durationsTotal number of customers served∑

Mathematically it is represented as

SAIDI = i i

T

r NN

CAIDI: Customer average interruption duration index. CAIDI represents the average time required to restore service to the average customer per sustained interruption. In words, the definition is

CAIDI = Customer interruption durationsTotal number of customer interruptions∑

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Mathematically it is written as

CAIDI = i ir N SAIDINi SAIFI

=∑

ASAI: Average service availability index. This index represents the fraction of time( often

in percentage) that a customer has power provided during one year or the defined

reporting period. In words, the definition is

ASAI = Customer hours service availabilityCustomer hours service demand

To calculate the index, the following mathematical equation is used:

ASAI = .

.

( . / )( . / )

T i

T

N No of hours year r NN No of hours year

− i∑

Note that there are 8760 hours in a regular year, 8784 in a leap year.

Some of the other customer based reliability indices in use are CTAIDI, ASAI etc.

Load based sustained indices include ASIFI, ASIDI etc. Momentary indices include

CEMSMIn, AMAIFI and MAIFIE. The newest indices are CEMIn, Customers

experiencing multiple interruptions, and CEMSMIn, Customers experiencing multiple

sustained interruptions and momentary interruptions events. Usage of CEMIn as a basis

performance measure is under consideration [3] by many states in USA. In Florida, usage

of CEMI5 index is under consideration. If this value is exceeded, the commission is

considering fines that would be paid to the customers who experienced poor

performance.

The snapshot of the percentage usage of different reliability indices, by the IEEE

working group [1] on system design is as shown in Figure 1-2. It was analyzed through

surveys that the most commonly used indices are SAIFI, SAIDI, CAIDI, and ASAI.

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Figure 1-2. Percentage of companies using a given index reporting in 1990

1.3 Purpose and Importance of this Thesis

It was so obvious from previous discussed indices that one has to reduce the total

number of interruptions in order to improve the reliability of a distribution system.

Though there are lots of parameters/ conditions that are responsible for these

interruptions, weather is still a big player and has a significant contribution. Research

carried out by the Electric Power Research Institute [4] showed the effects of weather

components, such as lightning, rain and wind in transmission lines (345kV and above).

However, not significant similar work was done for distribution lines which brought our

attention to research in this new direction.

The purpose of the current thesis work was to study the impacts of normal weather

conditions on the distribution power interruptions and develop correlation models. Study

also includes how the correlation knowledge can be used to reduce the power

interruptions by incorporating Artificial Neural Networks (ANN). Using weather and

interruption data novel prediction tools and modeling methods were developed, in which

the similar kind of approach can be applied to any electric utility in the country. With the

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provision of novel tools developed in this thesis, any power utility would be able to

estimate/predict the total approximate number of interruptions that might happen in the

future due to weather. The accuracy of the prediction of interruptions depends, in part, on

the accuracy of the forecast weather data which serves as input to the model and, in part,

on the accuracy of the model. It is expected that the use of real-time surface weather data,

such as can be collected from well-sited weather stations, will eliminate the uncertainty

inherent in weather data collected from geographically distant sources.

Despite a thorough search of the available literature, examples of the use of surface

weather data in the construction of power reliability models have not been found. It is

expected that this project will contribute significantly to the existing literature by

providing predictive models, as well as background in a previously unexplored area.

Moreover, this research is valuable for the exploration of proper ANN structure, internal

parameters and feature pattern extraction methods for application to power systems.

1.4 Organization of Thesis

The current thesis work comprises six chapters. The current chapter gives the

motivation, literature survey and the importance of the project. The second chapter

explains about the behavioral model of weather conditions prevalent in Florida State. It

will also give a broad knowledge of different weather parameters. The third chapter deals

with the Florida Power & Light (FPL) system and also the information on weather and

interruption data considered in the analysis. The fourth chapter presents the approach

followed towards developing correlation models between weather parameters and power

interruptions using statistical tools. The fifth chapter reveals a novel model using Neural

Networks that can be used to predict the power interruptions based on the forecasted

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weather parameters. The last chapter concludes with the limitations of the research

results, and conclusions of the current thesis followed by future work.

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CHAPTER 2 UNDERSTANDING FLORIDA WEATHER

As weather in Florida is very varying, different weather parameters in Florida that

are more common are explained and their impact on power distribution lines is explained

in this chapter. Florida is also known as the lightning capital of the world.

The natural phenomena of the weather that can reduce the strength [4] of the

insulators in the state of Florida are air-density, temperature, pressure, humidity, rain,

dew or condensation of humidity, pollution, wind and lightening.

2.1 Air Density, Temperature and Pressure

The variation of the temperature in the state of Florida is between 20oF and 100oF

and the pressure doesn’t change significantly. The influence of this on the strength of the

insulators, without abnormal condition like fire, is around of 5%.

2.2 Humidity

The humidity in Florida changes significantly throughout the year and throughout

the day. Usually, the humidity can be very high between Midnight and 6 /7 A.M and after

that it starts to decrease. It again starts to increases at night. The influence of the humidity

without condensation can affect the strength of the insulator to around 16%.

2.3 Rain

The rain can be classified into weak rain (mist or drizzle) or strong rain

(rainfall).The influence of the rain on the insulator strength varies and depends on the

intensity and its direction. The maximum influence of rain [4] on clean insulators is

around 30% .

8

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The mist or drizzle along with pollution, can have a stronger impact on flashover

when it combines together with pollution on the insulators strings.

2.4 Dew or Condensation of the Humidity

When temperature decreases to the dew point, the condensation starts taking place

on the surface of the insulators and then a thin layer of water appears. The condensation

can have same effect as that of mist on insulator.

2.5 Pollution

Pollution can reduce the strength of an insulator. Its influence on flashover depends

on the type of contamination and its concentration on the surface of the insulators.

We are here concerned about two types of the contamination, the spot

contamination and the area contamination. In Florida the distribution of contamination

[4] is as shown in Figure 2-1. Black dots refer to spot contaminations and shaded refer to

area contaminations.

Figure 2-1. Regions with strong contamination (UHV project)

Table 2-1 shows the types of contamination that causes flashover. In dry conditions

most of them are not good conductors, however, in wet conditions due to condensation,

drizzle, mist or rain the conductivity increases substantially.

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Table 2-1. Type of Contaminant and Atmospheric Conditions at the Time of Contamination Flashover (UHV Project)

Pollution combined with condensation and rain can be considered as the worst

condition behind reduction of insulator strength. Moreover, dew, drizzle and mist are

considered the most important weather components at the time of flashover, for 72 % of

the cases [4].

Rain can have two different aspects. On one hand, it reduces insulators’

withstanding values. On the other hand, cleans the surface of the insulators thereby

preventing the system from new flashover due to dew (condensation), mist and pollution.

2.6 Wind

Special weather conditions, such as storms, thunderstorms, hurricanes and tornados

have a direct effect on power interruptions. However, these events are a combination of

rain, wind and lightning. Therefore, the individual analysis of each one of these weather

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components is required in order to study the real cause behind the flashover. An

evaluation of the influence of wind-speed on swing angle and therefore the minimum

clearance required to avoid possible flashover can be carried out. Wind can provoke

catastrophic mechanical damages due to asynchronous movements of the cables and/or

insulators. These damages are more significant in transmission lines where the span is

larger. Figure 2-2 shows the swing angle of a single conductor vs. wind-speed [4].

Figure 2-2. Swing angle as a function of instantaneous wind speed at tower

Distribution lines have small span, so the asynchronous movement of the

conductors, most of the times, gives insignificant disturbance except when there is high

speed. The most significant disturbance due to wind can come due to movement of the

trees and its branches. Trees, which are untrimmed, can touch the lines and can result in a

flash over leading to an outage.

The Figure 2-3 below shows the uncut trees and branches touching the distribution lines in Gainesville, Florida.

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. (a) (b)

(c) (d) Figure 2-3. Vegetation effects on power interruptions

2.7 Lightning

The number of days with thunderstorm in the Florida is between 80 and 100 as

shown in the Figure 2-4 (isokeraunic level). As we can see in Figure 2-4, Florida is a

state strongly affected with atmospheric discharges. The number of strokes to the earth

per square mile per year (lightning) can be found through the expression:

N= 0.25 I

where I is the local isokeraunic level.

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If a line has shadow width of W, the number of lightning expected to hit it per year is NL= 0.25 ILW/5280 where W=b+4h, L is the length of the line in miles, h is the height of the shield (ground)

wires and b is distance between shield wires. If the line doesn’t have shield wires, h is the

height of the conductors and b the distance between external conductors.

Due to strokes on transmission or distribution lines with shield wires a back

flashover is expected. The voltage across the insulator string in this case depends on

tower foot resistance, current through the tower and of the coefficient of coupling

between shield wire and phase conductor.

Figure 2-4. Number of days with thunderstorms in Florida (US Weather Bureau)

Thus, flashover or interruptions due to lightning depends on the tower foot

resistance and also on the intensity of the current. It is not possible to control the current

so all the control should be done through tower foot resistance. Distribution lines without

shield wires are directly affected by the lightning. The level of the voltage across the

string or insulator depends on intensity of the current and the magnitude of the surge

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impedance of the line. Figure 2-5 shows the amplitude of the crest of the strokes with the

probability of the occurrence. It is possible to see that the probability of a stroke, which

has a current up to 5 kA, is almost 1. This current while passing through the conductor

will be divided into two. Thus, the voltage across the insulators or string of distribution

lines with surge impedance between 150 Ω and 250 Ω will be more or less between 375

kV and 625 kV. Thus, in most of the cases distribution lines up to 69 kV (BIL up to 350

kV) will be practically submitted to a flashover for every stroke on it.

Figure 2-5. Cumulative frequency distribution of peak current amplitudes in downward negative flashes

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CHAPTER 3 SYSTEM UNDER STUDY – FLORIDA POWER & LIGHT

The preliminary results cited in this thesis are the research results obtained while

working on the project sponsored by Florida Power & Light (FPL). But the concept and

idea can be further applied to any system and can be enhanced as explained in the current

thesis. The power distribution interruption data of FPL was considered to study the

effects of weather on the occurrence of interruption patterns of FPL.

3.1 Description of the FPL distribution system

FPL is among the largest and fastest growing electric utilities in the United States.

As of December 2002, FPL had 9,612 employees serving nearly 8 million people, or

about half the state of Florida. Power is delivered (Table 3-1) safely and reliably from 86

generating units with a Total generation capability =26203MW, through more than 500

substations and over more than 69,000 miles of transmission and distribution lines [5].

Table 3.1. FPL Power Sales by Sectors Sector Number of Accounts* Total Sales (kwh)

Residential 3,521,146 50.9% Commercial 430,471 40.6% Industrial 15,248 4.4% Other** 2,746 4.1%

* Monthly average as of December 2001 ** Includes public authorities, railway, wholesale and interchange.

FPL Distribution system is divided in 16 management areas grouped under two

regions; urban and suburban (Table 3-2). Figure 3-1 shows the location and area covered

by each of the FPL distribution management areas (MA).

15

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Table 3-2. FPL Distribution Management Areas along with Their Dispatch Centers REGION URBAN SUBURBAN DISPATCH West Pam

Breach Dispatch Center

South Florida Dispatch Center

Daytona Dispatch Center

Sarasota Dispatch Center

TC-Treasure Coast

PM- Pompano NF-North Florida

MS- Manasota

WB- West Palm WG- Wingate CF-Central Florida

TB-Toledo Blade

BR- Boca Raton GS- Gulfsteam BV- Brevard GC- Gulf CoastND-North DadeWD-West DadeCE- Central

AREAS

SD-South Dade

(a)

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(b)

Figure 3-1. Snap shot of Florida map (a) FPL distribution management areas. (b) Weather stations chosen within the FPL area

3.2 Interruption Data from FPL

Power interruption data is primarily obtained from Florida Power & Light (FPL).

FPL has divided its power supplying territory into 16 sections called Management Areas

(MAs). An interruption data file was created for each of these 16 MAs. Interruption data

was made available to us in a data storage program known as “Power-Play.” To make the

things more clearly, interruptions are classified in to different groups, Figure 3-4, based

on the type of causes that are responsible for these interruptions, for example –

interruptions occurred due to squirrel are represented under the category of squirrel cause

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code (007). Basically a cause code indicates the principle cause of an interruption. With

this kind of facility, we will be able to see interruptions happened due to a any specific

cause as shown in Table 3-3.

Table 3-3. FPL Cause Codes (102) Table REV - 6 /16 /98 SC C A U S E C O D E S Eq u ip m e n t Co d e s

(Re q u ire d fo r a l l in te rru p tio n s) O ve rh e a d U n d e rg ro u n d1 8 7 -E Equ ipt. Fa ile d, Ca us e Unk 0 8 0 Dow n Guy or Anc hor 1 1 0 Te r m ina tor1 9 0 Unk now n 0 8 1 P o le 1 1 1 Ca ble

O th e r C a u se s 0 8 2 Cros s Ar m 1 1 3 Elbow1 7 0 W r ong s iz e fus e 0 8 3 Ins ula tor 1 1 4 Tx Fus e S w itc h1 7 1 O ve r loa de d De vic e 0 8 4 P o le Top P in 1 1 5 Tx B la de S w itc h1 7 8 Non-s ta nda rd Cons tr uc tion 0 8 7 T ie W ir e 1 1 6 Ba yone t S w itc h1 8 3 Im pr ope r Ins ta lla tion 0 8 8 J u m pe r 1 2 1 P a dm ount S w itc h1 9 1 -E V a nda lis m 0 8 9 S tir r up 1 2 2 O il Fu s e Cutout1 9 3 Cus tom e r Re qu e s t 0 9 0 Hot L ine C la m p 1 2 3 RA S w itc h1 9 5 Cr e w Re qu e s t (P la nne d) 0 9 2 Dis c onne c t S w itc h 1 2 4 M e c h for T hrow ove r S w .1 9 6 S la c k Conduc tors 0 9 3 Fus e S w itc h 1 2 5 P T Fu s e1 9 7 O the r (e x pla in) 0 9 6 L in e O CR 1 2 6 Conduc t CKT Fu s e2 0 2 -E Loo s e Con ne c tion 0 9 7 L in e Ca pa c itor 1 2 7 Contr o l Ca b le

A ccid e n ta l C a u se s 0 9 8 L in e Re gu la tor 1 3 2 Ha ndhole0 4 0 V e h ic le 1 0 4 Conduc tor Dow n 1 3 4 Bus h ing0 4 1 Ac c ide nta l Conta c t 1 0 5 Conduc tor Da m a ge d 1 3 5 P othe a d0 4 6 S w itc h in g Err or 2 1 1 In je c te d Ca b le0 7 9 Dig-In (P r ope r De pth ) O ve rh e a d o r U n d e rg ro u n d

S u p p o rt a n d F o llo w -U p C o d e s 0 8 5 Ar r e s te r 1 0 2 O the r Equipm e nt(C o d e s to b e u s e d as Su p p o r t o r Fo llo w -u p On ly ) 0 9 1 Conne c tor 1 0 3 S plic e

0 1 2 No Anim a l Gua r d 2 4 1 In je c tion Elb ow (Not Ins ta lle d ) 0 9 4 Tr a ns form e r 1 0 6 Autom a te d S w itc h (DA) 0 2 2 P a lm Tr e e 2 4 2 Flow (P os itive ) 0 9 5 S te p Dow n Tr a ns form e r S u b sta tio n 0 5 0 For e ign Cre w or Cus tom e r 2 4 3 Flow (Non e ) M e te r 1 4 0 O CB (Fe e de r Bre a k e r ) 0 6 6 FP L Cr e w 2 4 4 In je c tion Com p 1 6 0 M e te r 1 4 1 Re gula tor 0 6 7 FP L Dis tr ibution Contra c tor 2 4 5 In je c tion J ob P nd ng 1 6 1 M e te r B loc k s , Re pa ir a ble 1 4 2 Re a c to r 0 6 8 FP L L ine Cle a r ing Contr a c tor 2 5 0 Ca ble Re pla c e J ob P e nding 1 6 2 CT 's 1 4 3 Re la y 0 6 9 Tr a ns m is s ion Contr a c tor 2 5 1 Ca ble Re pla c e J ob Co m p 1 6 3 P T 's 1 4 7 S te p Dow n Tr a ns fo rm e r 0 7 5 Im prope r De pth 2 6 0 Fa ult Loc a tor Us e d 1 6 4 O the r M e te r Equ ipm e nt 1 4 8 O the r S ubs ta t ion Equip .1 0 0 Ina de qua te /No Groun d 2 6 5 Cle a r e d by P hone 1 6 5 M e te r Bloc k s -Not Re pa r a ble 1 5 0 S CADA1 9 2 Cre w Re que s t (For c e d O uta ge ) 2 7 1 In je c te d (8 /9 6 on) 2 0 0 Tra ns m is s ion r e la te d 1 5 1 T e le c om m unic a tions1 9 9 De fe c tive M a te r ia l - UP R 2 7 2 Re pla c e d (8 /9 6 o n) 2 2 2 P ow e r Te m p Us e d 2 9 9 Da ta Cor re c te d 2 4 0 In je c tion Elbow (Ins ta lle d) 9 9 9 Na m e d S torm Ex c lus ion s

No te : T h e s u f f ix "E" d e n o te s th at an Eq u ip m e n t C o d e is r e q u ir e d .Do No t En te r "E" o n T C M S .

Na tu ra l C a u se s 0 0 1 -E L ightning, w ith e qu ip .da m a ge 0 0 2 S torm w /no e quip . d a m a ge 0 0 3 -E Fir e 0 0 4 -E S a lt S pr a y Cor ros io n 0 0 7 S quir r e l 0 0 9 B ir d 0 1 1 O the r Anim a l 0 1 3 Tor na do 0 1 4 Hurr ic a ne 0 1 5 Ic e on L ine s 0 2 0 T r e e /L im b P r e ve nta ble 0 2 1 T r e e /L im b Unpr e ve nta ble 0 2 3 -E De c a y/De te r ior a tion 0 2 4 -E Cor ros ion (Non S a lt S pr a y) 0 2 5 V ine s /Gr a s s 0 2 6 -E Conta m ina t ion (Non S / S )

W e a th e r R e la te d C o d e s LIGHTNING NO LIGHTNINGP RES ENT P RES ENT

EQ UIP DAM AGE 0 0 1 - E 1 8 7 - E NO EQ UIP DAM AGE 0 0 2 1 9 0

The interruption data will be daily totals broken down by cause code. For example, a

specific substation may experience three interruptions on September 29, 1998, due to

cause code 093 - fuse switch. Each data point will be small, but the compilation of many

years and many areas will provide a statistically significant sampling.

The interruptions of interest to us were further defined by the use of the following

filters:

• With Exclusions - This filter suppresses interruption data that is defined as exclusionary by FPL, including hurricane and tornado damage. We use this filter because we are interested in the effects of normal weather conditions.

• Overhead - This filter includes only those interruptions that are caused by faults in overhead equipment or lines. Underground lines were considered immune to most weather conditions.

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• Internal Distribution - Interruptions located at the distribution system only were taken into account.

• Primary - Only primary systems (feeders, laterals and oil circuit breakers) are within the scope of this research.

• Substation - Each substation reports all the interruptions occurring in the secondary distribution system it supplies

• Cause code - FPL uses numeric cause codes to specify the causes of interruption. General categories include natural causes, equipment and accident.

• Dates - All relevant days from January 1, 1998 through December 31 2001 were considered. It is possible to get up to date interruption data by requesting FPL.

Assumptions about FPL system: An important consideration in choosing FPL is

that they have assured us that we can make the assumption that their equipment is

homogenous throughout their area of operations (AO).Homogeneity of equipment is a

necessary condition for statistically significant results

Scope of current Thesis: As FPL personnel have already done correlation analysis

between lightning strikes and the power interruptions, they are interested in knowing the

indirect effects of weather including wind, temperature, rain etc on the total number of

power interruptions. So the scope of the current research work is limited to these

parameters only.

Although interruptions represent between 3% to 5% [6-8] of the frequency of

disturbances, a common method for measuring the reliability of an electric distribution

system is based on the number of customers interrupted, which is proportional to the

number of interruptions, as explained in chapter 1. Let us revisit the definition of SAIFI,

a reliability index which the FPL uses more often. IEEE Standard 1366 defines the

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System Average Interruption Frequency Index (SAIFI) with the following formula:

b

N

i

C

CSAIFI

i

∑= 1

where

Ni = Number of interruptions (sustained interruptions lasting over 1 minute)

Ci = Customers interrupted for each interruption

Cb = Customer base or customers served

Years (J-January, D-December)

SAIF

I

Figure 3-2. FPL’s historical SAIFI performance

SAIFI indicates how often the average customer experiences a sustained

interruption (>1min.) over a predetermined period of time, and it has a special importance

in decision making for engineers working in distribution reliability. A typical breakdown

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by significance of the major causes for customer interruption and number of interruptions

of FPL distribution system under study for a period of 12 months is shown in Figure 3-3.

Customer Interrupted-2001

0

400000

800000

1200000

1600000

2000000

Wea

ther

(Sto

rm+L

ight

ning

)

Equi

pmen

t Fai

lure

Vege

tatio

n

Unk

now

n

Req

uest

Cor

rosi

on/D

ecay

Anim

al

Impr

oper

Pro

cess

Oth

er

Acci

dent

Major cause

Cus

tom

er In

terr

upte

d

0.00%3.00%6.00%9.00%12.00%15.00%18.00%21.00%24.00%27.00%30.00%

(a)

Number of Interruptions-2001

0

5000

10000

15000

20000

25000

Wea

ther

(Sto

rm+L

ight

ning

)

Equi

pmen

t Fai

lure

Vege

tatio

n

Unk

now

n

Req

uest

Cor

rosi

on/D

ecay

Anim

al

Impr

oper

Pro

cess

Oth

er

Acci

dent

Major cause

Num

ber o

f Int

erru

ptio

ns

0.00%2.00%4.00%6.00%8.00%10.00%12.00%14.00%16.00%18.00%20.00%

(b)

Figure 3-3. Frequency charts of interruptions and customers affected by interruptions. (a) number of customers interrupted vs. causes and, (b) number of interruptions a

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The previous graphs show the relative importance of the direct effects of weather

(storms and lightning) on the interruptions, but not the indirect effects i.e. temperature,

rain, wind etc. From this chart it is not possible to determine if interruptions associated

with, for example, vegetation or equipment are indirectly affected by weather conditions

such as temperature, rain or wind.

The current thesis shows that normal weather conditions do have effects on

interruptions and that those effects can be quantified. The benefits of this type of study

are the ability to explain trends in the SAIFI due to weather conditions and as an aid in

the development of indicators for possible use in anticipating interruptions.

3.3 Meteorological Weather Data from NCDC

We collected daily average weather data for rain, temperature, wind speed and

other parameters from Automated Surface Observation Stations (ASOSs) located at

airports throughout the area of operations (AO). Construction of these stations has begun

in 1981 as an aid to air navigation and they have since become the most comprehensive

source of weather data in the United States. For the stations we are interested in, we will

be using data from 1996 through 2002. As we are an educational institution, the National

Climatic Data Center (NCDC), a department of the National Oceanic and Atmospheric

Administration [9], is making this data available to us free of charge.

The greatest difficulty in collecting these data is its sheer volume. Six years of data

from one ASOS will generate a file containing 24 columns and 2190 lines. Stacking files

from all the ASOSs in the AO will generate a composite file with more than 20,000 lines.

To add to this problem, there are missing days, missing data points and formatting that is

not importable to the statistical program of our choice. A final editing of the data was

done by brushing (taking out) those points of data which doesn’t make sense : data points

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with zero barometric sea pressure, zero average temperature, 100 mph of 2 minutes

maximum wind gust etc.

To address this, we wrote programs in C/C++ that will correct the omissions and

convert the NCDC files to a generic text file that can be imported by any commercial

spreadsheet program presently in use. Since we anticipate the use of ASOS data by any

power engineer using our methods, file conversion is required by our objective.

3.4 Weather Parameters of interest

Though there are a lot of weather parameters available in weather file downloaded

from NCDC website, we used only those parameters which are of interest. A weather

data file was created for each of the 15 ASOSs (one particular ASOS covered two

regions). The following daily weather parameters were downloaded from the NCDC

database:

• Average temperature • Maximum temperature • Minimum temperature • Average dew point • Significant observations • Total rainfall • Barometric pressure (sea level and station) • Average wind speed • Two-minute maximum sustained wind gust • Five-second maximum sustained wind gust Weather is a complex combination of lot of parameters including, but not limited to,

wind, lightening, condensation, temperature, rain, pressure, humidity, cosmic dust, solar

storms, hurricanes, storms etc and the list goes on if all the meteorological terms are

included, some of which we are not even aware of. But if the daily prevailing weather

conditions are considered, fortunately lot of parameters can be neglected by throwing

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them under the category of extreme weather conditions i.e. not-a-common daily weather

parameter, e.g. Hurricanes, Storms, lightening etc. Therefore, the major focus was given

on the weather parameters like wind, temperature, rain, pressure, humidity etc which are

not extreme weather conditions. Also among all these common weather parameters, only

wind, rain and temperature are investigated, because of their dominant role [10] on the

power distribution interruptions.

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CHAPTER 4 CORRELATION OF WEATHER AND INTERRUPTIONS

Consequences of power interruptions can range from mild to severe inconvenience

such as missing your favorite TV show or losing critical data, to life threatening, such as

the failure of traffic signals. Less obvious consequences include increased cost to the

customer due to increased maintenance and repair costs for the provider. Because of these

consequences, power engineers are always researching methods to reduce the number of

interruptions.

The first step to reducing interruptions is to define the causes, and quantify their

effects. Accident, human error and aging equipment contribute a great deal, but weather

is still the largest single cause, although the effects are not as well understood as we

would like to think. We can all agree that adverse weather conditions cause power

interruptions. The evidence is apparent. When a bad thunderstorm storm hits, or a

hurricane arrives, many people experience power interruptions, and those who don’t, hear

about it on the news.

Lightning strikes, especially common in Florida, create transients that overload

transformers and trip fused circuit breakers, both conditions requiring a repair crew to

restore power. High winds blow down trees, damaging conductors.

Less apparent is the effect of normal weather on the frequency of power

interruptions. Several days of moderate rain can saturate the ground, invading buried

lines and causing short circuits (FPL study).An unexpectedly warm season can promote

25

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vegetation growth, causing interruptions due to tree limb/conductor contact. These and

other effects of normal weather are not easily defined because there is not a one-to-one

relationship such as ‘lightning hit the line so the transformer blew.’ In fact, many

preventable interruptions occur that are not properly attributed to weather because of that

lack of one-to one relationships.

4.1 Importance of Statistical Tools

Part of the interest of this project is to find the relationship between the number of

interruptions and normal weather conditions. Both interruptions and weather conditions

in the future are random. To gain a complete prediction of the number of interruptions in

the future, we need to predict future weather conditions and predict the number of

interruptions based on the predicted weather conditions.

However, because of limited resources and the difficulty of weather predictions, we

will process the conditional prediction for the number of interruptions assuming that the

weather condition is known. In this subsection, we will describe the probabilistic

characteristics of daily interruption frequencies and the sums of daily interruption

frequencies, i.e., monthly interruptions or sums of interruptions when it rains and when it

does not. Then the explanation on plausible statistical data analysis techniques for each

case follows.

The daily outage frequencies have only nonnegative integer values and are strongly

skewed to the right. For example, the daily interruptions caused by tree limbs (Cause

Code 20 and 21) has the range from 0 to 58, but 99.5% of frequencies are less than or

equal to 5 (Table 4-1). Therefore, statistical techniques based on the normal distribution,

such as t-Test, normal linear regression, and ANOVA, generate big biases in calculating

the confidence intervals of estimates and provide wrong conclusions in the search of

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significant weather effects. As a reminder, the normal distribution is symmetric and has

the range, (-∞, +∞).

Table 4-1. The Frequency of Interruptions due to Tree Limbs (Cause Codes 20 & 21) The Number of Outage

Frequency Percent Cumulative Percent

0 15890 81.16 81.16 1 2582 13.19 94.35 2 632 3.23 97.57 3 223 1.14 98.71 4 102 0.52 99.23 5 53 0.27 99.50 6 38 0.19 99.70 >6 59 0.30 100.00

The nature of the weather data sets is first evaluated to know the behavioral

patterns of weather parameters. Some of the parameters of our interest are wind,

temperature and rain.

4.2 Probabilistic Characteristics of Data Distributions

As a prelude to presenting results, I will describe the probabilistic characteristics of the

data set we are dealing with; to determine what statistical data analysis techniques and

models should be used to correlate weather parameters with power interruptions.

Daily interruption frequencies (for all cause codes) have only nonnegative integer

values, from 0 to 200, and are skewed to the right, as can be seen in Figure 4-1. Rain data

shows a stronger displacement to the right (Figure 4-2), while wind speed histogram

(Figure 4-3) gets close to a normal distribution.

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0 10 20 30 40 50 60 70 80

0

1000

2000

3000

4000

5000

6000

7000

8000

9000

N

Freq

uenc

y

Figure 4-1. N for all management areas from 1998 to 2001 using the previous filters

1 2 3 4 5 6 7 8 9 10

0

1000

2000

Rain

Freq

uenc

y

Figure 4-2. Rain (inches) for all management areas from 1998 to 2001

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0 10 20 30 40 50 60 70

0

1000

2000

2MMaxS

Freq

uenc

y

Figure 4-3. Wind-2 minutes maximum speed (mph) for all management areas from 1998 to 2001

Because a normal distribution is symmetric and the normal random variable is

continuous within the range (-∞,∞), these probabilistic characteristics must be explained

using Poisson distribution.

4.3 Correlation Analysis between Weather Parameters and Interruptions

The statistical correlation models between weather parameters of interest – wind,

temperature and rain, and the total daily number of power interruptions (N) were studied.

4.3.1 Impact of Temperature on N

In this section, the impact of daily temperature variations on the Power

interruptions due to transformer failures was studied.

The monthly averages (means) of the maximum temperatures were taken on the X-

axis and the monthly means of the total number of interruptions due to transformer

failures were taken on the Y- axis for 4 years (1998-2001) of all the MAs. Under these

conditions, the total number of monthly data points came to be around 567.

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Regression

95% CI

95% PI

65 75 85 95an of Max. Temperature (F)

Y= 202.803 - 5.09S = 2.62145 R-

Regression Pl380X + 0.0328080 X**2Sq = 42.0 % R-Sq(adj) = 41.8 %

ot of N Vs. Max. Temp

0

10

20

Me

Mea

n of

N

Figure 4-4. Variation of average N due to transformer failu

It can be observed from Figure 4-4 that the plot has p

X-axis. The reason can be attributed due to the heavy load

the maximum usage of power during these temperatures. P

customers try to switch on their air-conditioning at once w

temperature or minimum temperature. It looks like around

much increase in the transformer failure interruptions and h

temperature. Approximately after 800F, the curve increase

right skewness of the graph indicates that the higher tempe

predominant than the lower ones; this is true for Florida, es

most of the year it is sunny.

PI – Prediction Interval limits CI – Confidence Interval limits

res vs. maximum temperature

eaks over the two edges of the

on the transformers because of

art of the reason being, all the

hen there is either maximum

750F to 800F, there will not be

ence is an optimal

s in an exponential way. The

rature effects are more

pecially southern part, where

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908070

15

10

5

Mean of Max. Temperature (F)

Mea

n of

N

S = 1.11736 R-Sq = 80.9 % R-Sq(adj) = 80.1 % + 0.0335747 X**2Y = 208.210 - 5.22174 X

Regression Plot of N Vs. Max. Temperature

Figure 4-5. Variation of average N due to transformer failures vs. maximum temperature (averaged per month per year)

Figure 4-5 was plotted with the same exact information used to plot Figure 4-4, but

the data of the corresponding months of the 4 years for all the MAs was averaged giving

a total of 48 points. Similarly in Figure 4-6 the data of the corresponding months of all

the 4 years was averaged to give 12 data points. The important thing that we should

observe is that as the number of data points is getting lesser and lesser, the plot is getting

smoother with the increase in R2 value but at the cost of losing the finest details of the

data points because we are averaging out all the variations for each month. This method

of averaging out the data points provides us an opportunity to see the hidden pattern

between the variables by suppressing the disturbances/noise in the data set.

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75 80 85 90

3

4

5

6

7

8

9

10

11

12

13

Mean of Max. Temperature (F)

Mea

n of

N

Y = 273.490 - 6.81286 X + 0.0432362 X**2S = 0.597484 R-Sq = 95.1 % R-Sq(adj) = 94.0 %

Regression Plot for N Vs. Max.Temp

Figure 4-6. Variation of average N due to transformer failures vs. max temperature (averaged per month)

The correlation equation for the X and Y variables considered is given on the top of

each of the plots; R2 represents the proportion of variability in the Y variable accounted

for by the X variable.

Based on the correlation model developed between the transformer interruptions

and maximum temperature, it is possible to predict the total number of interruptions due

to transformer for any day/MA if the maximum temperature of that day/MA is know /

given. The following Table 4-2 shows the prediction of Transformer interruptions and the

error associated with it for each of the MAs of FPL.

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Table 4-2. Prediction of N Using Maximum Temperature of All the MAs MA Airport Tmax

(Avg.) N Tx (Avg.) actual

N Tx prediction ALL FPL EQUATION

Error ALL FPL EQUATION

N Tx prediction INDIVIDUAL MA’s EQU

Error MA’s EQU

Central Florida DAB 66.5000 7.36364 9.31668 26.523 8.170 10.951 Wingate FLL 74.4091 3.45455 5.40181 56.368 4.898 41.784 Gulf Coast FMY 72.5909 6.13636 5.91181 3.659 * * Treasure Coast FPR 71.3182 6.86364 6.40587 6.669 * * Wingate FXE 74.6364 3.45455 5.35414 54.988 4.850 40.395 Gulf Stream HWO 75.3636 4.04545 5.22544 29.168 * * Central Dade MIA 75.2727 3.50000 5.23954 49.701 5.020 43.429 Brevard MLB 69.8182 7.22727 7.13454 1.283 * * North Dade OPF 75.4545 4.81818 5.21190 8.172 * * West Palm PBI 74.0000 4.90909 5.49660 11.968 * * Toledo PGD 71.3182 4.18182 6.40587 53.184 5.429 29.824 Pompano PMP 73.8636 2.31818 5.53076 138.582 3.720 60.471 Cetral Florida SFB 68.3636 7.36364 7.99378 8.558 * * Manasota SRQ 68.0000 6.95455 8.23225 18.372 7.360 5.830 South Dade TMB 76.3636 5.40909 5.10758 5.574 * * ALL FPL 72.485 5.2 5.9 13.4%

Description:

• MA – Management Area considered

• Airport – The nearest airport to the MA considered in getting the weather data

• Tmax (Avg.) – The average value of the maximum temperatures occurred in January 2002

• N Tx (Avg.) – Average number of interruptions (N) happened due to Transformer failures

• N Tx prediction All FPL equation – Predicted N Tx (Avg.) using the common equation of all MAs

• N Tx prediction Individual equation – Predicted N Tx (Avg.) using local equation of individual MAs

It can be observed from table 4-2 that the prediction error varied over a wide range

from 1.28 % to 138 %. There were only 5 cases where the error exceeded 50%, with

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others within the satisfactory limits. The huge error is due to the incorporation of

common equation developed from the data of all the MAs. But using the individual MA’s

equations, which were developed from the local MA’s data, those huge errors were

drastically reduced. There were cases where the common equation gave better results

than the local equations of the MAs; hence local equations are used only for those MAs

where common equation gave a huge error.

4.3.2 Impact of Wind on N

The role of wind is very significant among all the weather parameters. There is a

very good correlation between wind and total number of interruptions (N).

When the plot is drawn between the daily 2 minute maximum wind gust (TMMG)

and N, it was a big mess and chaotic where no pattern can be seen. Because, for a given

value of the TMMG speed there were different levels of N occurred. So the averages of

different levels of N occurred at each of the speeds of TMMG were taken and then

plotted, the plot can be seen in Figure 4-7.

605040302010 0

15

10

5

0

Mean of 2minutes Wind Gust speed (mph)

Mea

n of

N

S = 2.76351 R-Sq = 39.8 % R-Sq(adj) = 35.2 %

+ 0.0355799 X**2 - 0.0004352 X**3Y = 4.57617 - 0.692087 XRegression Plot of N Vs. Wind

Figure 4-7. Variation of N vs. wind

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It seems that there is a pattern until 40 mph, but after that the pattern gets distorted.

If at least 30 points were considered while calculating averages then the correlation

obtained by this process is very high, R2 = 99.3% and reveals the existence of strong

cubic relationship, Figure 4-8, between N and TMMG. By doing so, only 1.5% of the

data points were neglected still keeping 98.5% of the whole data.

302010

4

3

2

1

Mean of 2minutes W ind guest speed (mph)

Mea

n of

N

S = 0.0900810 R-Sq = 99.3 % R-Sq(adj) = 99.2 % - 0.0065040 X**2 + 0.0002598 X**3Y = 0.613754 + 0.0647258 X

Regression Plot of N Vs. W ind

Figure 4-8. Mean of 2 minutes wind speed vs. average number of interruptions

It can be observed from Figure 4-8 that the total average number of interruptions

increases exponentially after around 20 mph. So power distribution poles and overhead

equipment must be designed in such a way that there won’t be any breakdown for wind

gusts of more than 20 mph. Also care has to be taken that the distribution line’s

neighborhood vegetation and others near by to it are at a proper distance and will not lean

on the power distribution lines during these wind gusts.

4.3.3 Impact of Rain on N

The impact of rain on the mean number of N can be observed in the following

figures.

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0 1 2 3 4 5

0

1

2

3

4

5

6

7

8

9

Mean of Rain(inch)

Mea

n of

N

Y = 1.43350 + 3.04671 X - 1.09160 X**2 + 0.137744 X**3S = 1.24028 R-Sq = 42.8 % R-Sq(adj) = 37.2 %

Regression Plot of N Vs. Rain

Figure 4-9. Variation of N vs. rain

The number of days that didn’t rain is more than the days that rain. As the impact

of rain on N is under consideration, the non-rainy days have been excluded from the data

set. The data points of N were averaged similar to the approach followed in analyzing

wind impacts on N; different occurrences of N for each level of rain were averaged and

then plotted in Figure 4-9.

The whole graph can be divided into 3 piecewise linear segments; 0.1 to 1 inch, 1

to 3 inch and more than 3 inch. In the first segment there looks a linear relationship,

Figure 4-10, between N and Rain, and hence initial small amount of rain play a vital role

in the amount of interruptions.

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0 1 2

1.0

1.5

2.0

2.5

3.0

3.5

4.0

4.5

5.0

5.5

Mean of Rain(Inch)

Mea

n of

N

Y= 1.47309 + 2.11652 X + 0.662153 X**2 - 0.498268 X**3S = 0.568862 R-Sq = 78.9 % R-Sq(adj) = 75.0 %

Regression Plot of N Vs. Rain

Figure 4-10. Variation of N vs. rain in the interval [0 2]

N remains pretty much constant in the second segment showing constant effect of

rain, but in the third segment N increases drastically as rain increases over 3 inch. The

small amount of rain, little showers, settles down on the insulators. This droplets of water

helps as a solvent for the salts and the atmospheric dust deposited on the insulators and

forms a conducting layer for the current, thereby causing a flashover which leads to

power interruptions, as explained in chapter 2.

On the other hand, rain from 1 to 3 inch is large enough to clean the insulator, as

they drop off from it instead of getting deposited. Finally, rain over 3 inches is

accompanied with extreme weather conditions leading to again huge amount of N.

4.3.4 Effect of Rain and Wind Together on N

The following three-dimensional Figure 4-11 gives the relationship between the

combined effect of wind and rain on the average number of N. It can be seen that the

predicted (calculated) Navg tracks very well the actual N happened for lower values of N.

The regression equation is given by

Navg = 1.05 – 0.04*Wwind speed + 6.82*Rrain average

The correlation coefficient, R2, is = 85.6%

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510

1520

2530

35

0

0.2

0.4

0.6

0.80

1

2

3

4

5

6

7

Wind (mph)Rain (inch)

N a

vg

Field dataPrediction

Figure 4-11. Impact of rain and wind together on N

Usual methods of statistical analysis rely, in part, on knowing in advance what the

researcher is looking for. An example is a study done by FPL that provides a linear

equation describing the number of interruptions caused by lightning as a function of the

number of lightning strikes. In this case, the cause of the outage is known (one-to-one

relationship) and the result is expected. The data required for this type of analysis is also

proscribed by the limited scope of the question. Also, there are limited strategies for

dealing with the problem, since lightning is a random and unpredictable event. Analyzing

the effects of normal weather requires a different approach. We need to be open to

unexpected results rather than expected ones. We need to consider a body of data much,

much larger than that required to investigate a single phenomena. We need to consider

non-linear relationships and relationships that imply a confluence of conditions. We need

to apply every statistical tool we can think of, and then learn some more. Most of these

features are available in a tool called Artificial Neural Networks (ANNs). Hence the

application of ANNs to our current problem is discussed in next chapter.

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4.3.5 Effect of Lightning Strikes on N

FPL has already done correlation analysis between cause codes 01(Lightening, with

equipment damage) and 02(Storm with no equipment damage) and lightning strikes for

all the MAs considering the years 1998-2001. Cause codes 01 and 02 represent the direct

weather effect on service interruptions. The following plot, copied from the FPL

information slides during their visit to University of Florida, explains the impact of

lightning strikes on the storm interruptions with a very high correlation with a linear

relation meaning the higher the lightning strikes the higher the storm interruptions.

Figure 4-12. Lightning strikes vs. storm interruptions during 1998-2001 for all MAs

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CHAPTER 5 PREDICTION OF INTERRUPTIONS USING ARTIFICIAL NEURAL NETWORKS

Though it gives the impression, from the previous chapter, that the effect of all the

weather parameters on power interruptions can be quantified using standard mathematical

functions/ statistical techniques, it is not always true. It may neither practical nor feasible,

always, to find a function for certain complex correlations between weather and

interruptions. This is where the need for the neural networks arises to analyze and

generalize the hidden relationship.

We need a tool which is powerful when applied to problems whose solutions

require knowledge which is difficult to specify, but for which there is an abundance of

examples – artificial neural networks is one of the best tools for this kind of problems.

5.1 Introduction to Artificial Neural Networks

Neural networks, or artificial neural networks (ANN) to be more precise, represent

a technology that is rooted in many disciplines: neurosciences, mathematics, statistics,

physics, computer science, and engineering. ANNs find applications in such diverse

fields as modeling, time series analysis, pattern recognition, signal processing, and

control by virtue of an important property: the ability to learn from input data

with(supervised) or without a teacher (unsupervised).The most common training

scenarios use supervised learning.

ANN is a very useful tool for predicting the interruptions of a power distribution

system to a decent accurate value. The accuracy of prediction is directly proportional to

the accuracy of the historical power interruption and weather data used to train the ANN.

40

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This project provides the methodology for predicting the interruptions beforehand for the

forecast weather conditions using ANNs.

5.1.1 Benefits of ANNS over statistical methods

ANN is an alternative to conventional methods [11]. ANN is an approach that

combines the time series and regression approaches; it learns from the previous

interruption and weather patterns and predicts one for the current conditions, it also

performs a non-linear regression between interruptions and weather patterns. It shows

superior performance in terms of accuracy when compared to statistical methods [12].

ANN derives its computing power through, first, its massively parallel distributed

structure and, second, its ability to learn and therefore generalize. Generalization refers to

the neural network producing reasonable outputs for inputs not encountered during

training (learning). These two information-processing capabilities make it possible for

neural networks to solve complex (large-scale) problems that are currently intractable.

The main reasons for using neural networks, for prediction, rather than statistical

techniques/ classical time series analysis are [13]

• They are self-monitoring (i.e., they learn how to make accurate predictions. • They are able to cope with nonlinearity and nonstationarity of input processes. • They are adaptive, non-linear and highly parallel. • They can generalize. • They are computationally at least as fast, if not faster than most available Statistical

techniques.

Multi-layered ANNs are capable of performing just about any linear or nonlinear

computation, and can approximate any reasonable function arbitrarily well.

5.1.2 Architecture of ANN

Figure 5-1(a) shows the basic model of a single neuron while Figure 5-1(b) shows a

one-layer network with R input elements and S neurons. In this network, each element of

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the input vector p is connected to each neuron input through the weight matrix W. The ith

neuron has a summer that gathers its weighted inputs and bias to form its own scalar

output n(i), Figure 5-1 (b). The various n(i) taken together form an S-element net input

vector N. Finally, the neuron layer outputs form a column vector a, where a = f (Wp+b).

(a) (b)

(c)

Figure 5-1. ANN structures: (a) basic nonlinear model of a neuron, (b) one layer network of neurons, and (c) 3 layer feed forward back propagation network

Figure 5-1 (c) shows the ANN model used in the current project. IW represents

Input Weight matrix having a source 1(second index) and a destination 1(first index).

Also, elements of layer one, such as its bias, net input, and output have a superscript 1 to

say that they are associated with the first layer. LW represents layer weights [14].

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The data is presented to the input nodes. Each input node is connected to several

nodes in the second layer. The second layer is called the hidden layer, since they are not

accessible to the outer environment. The hidden layer acts as a layer of abstraction,

pulling features from inputs. Determining the proper number of nodes for the hidden

layer is difficult and often determined through hit and trial. Generally, network

performance increases with the number of hidden nodes and then reaches a saturation

level [15]. The addition of more hidden nodes may actually degrade performance due to

increased difficulty of training data. The implementation of this commonly accepted rule

will help train the ANN efficiently and will also help convergence of the solution. The

last layer is referred to as the output layer, since the network’s output is the response of

nodes on this layer. The number of output nodes of an ANN is determined by the

requirement.

5.1.3 Functioning of ANN

In general, the operation of this feed forward network consists of passing weighted

and summed input signals through a chosen nonlinearity. It presumes knowledge of the

network’s bias functions and weighted links. Once activation and output functions are

chosen, an ANN is completely described by its weights and biases. Since a given ANN

solves a specific problem, or function, finding weights and biases for the network is

equivalent to finding the input/output relationship that describes the function. In the

current ANN model, Figure 5-1(c), the activation functions chosen in the hidden layer

and the output layer are “tansig” and “purelin” respectively. The two layer sigmoid/linear

network can represent any functional relationship between inputs and outputs if the

sigmoid layer has enough neurons.

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There were a lot of training algorithms and performance functions that we can

chose from to train the network model. For the present problem BPN algorithm has been

chosen, as it was the famous algorithm for multi-layer perceptron (MLP) networks and

‘trainbfg’ training function was used to train BPN. The term back propagation refers to

the manner in which the gradient is computed for nonlinear MLP networks. Properly

trained back propagation networks tend to give reasonable answers when presented with

inputs that they have never seen. Typically, a new input leads to an output similar to the

correct output for input vectors used in training that are similar to the new input being

presented. This generalization makes it possible to train a network on a representative set

of input/target pairs and get good results without training the network on all possible

input/output pairs.

5.1.4 Back Propagation Learning Rule

The back propagation learning rule [16] is an iterative gradient algorithm designed

to minimize the mean square error between the actual output of a multilayer feed forward

network and the desired output. An essential component of the rule is the iterative

method that propagates error terms required to adapt weights back from nodes in the

output layer to nodes in lower layers.

At beginning, we set all weights and node offsets to small random values. The

input values are presented and the desired outputs are specified. Then the network, Figure

5-2, is used to calculate actual outputs. A recursive algorithm, starting at the output nodes

and working back to the hidden layer, adjusts weights until weights converge and the cost

function is reduced to an acceptable value. The training process is repeated by presenting

different sets of input data to the ANN.

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Figure 5-2. A back propagation ANN model

5.2 Steps to Enhance the performance of ANN

There is a wrong notion that one can dump all the available variables as input to the

ANN to predict the solution. The more the number of input variables to ANN the

complex the problem to track in studying the correlation between these input variables.

To enhance the performance of ANN, the input data has to be pre-processed. ANN

toolbox of MATLAB 6.0 has some of the functions which can perform these operations.

The following are some of the techniques that could be helpful to enhance the quality of

the input datasets before giving it to ANN:

• Eliminate the unnecessary variables which don’t have significant contribution to the output.

• Scale the inputs and targets so that they always fall with in a specified range.

• Reduce the dimensions of the input data, without much loss in the variance, e.g. Principle Component Analysis, as explained below.

As weather is a combination of many parameters like wind, temperature, rain,

pressure, dew, lightening etc, the next question that comes to our mind is what are the

predominant ones among all these parameters that have significant contribution towards

the daily interruptions? One way to figure out solution for this problem is to see the

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variance of all the weather parameters with respect to each other. The ones which have

more variance are more responsible towards N than the ones with less variance. Less

variance in a variable means fewer changes in its value, which means this variable has

less effect on the changes of N. For investigations involving a large number of observed

variables, it is often useful by considering a smaller number of linear combinations of

original variables.

Principle Component Analysis (PCA)

PCA is one of the friendly tools used popularly to reduce the dimensions of input

variables. Principle component analysis [13] finds a set of standardized linear

combinations called the principal components, which are orthogonal and taken together

explain all the variance of the original data. The following analysis shows the variance of

the 8 input considered in the ANN model:

Table 5-1. Summary Table of Covariance for All the Input Variables Considered in the Principle Component Analysis

In the above table 5-1, if component 1(comp.1) alone is considered, it explains 54.9% of

the total variance in the data set by using the following linear combination of only 4

weather variables:

Comp.1 = 0.515(MaxTemp) + 0.738(MinTemp) – 0.107(HeatDays) + 0.415(CoolDays)

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Similarly, comp.2 alone explains 22.9% of the total variance in the data set with the

following linear combination:

Comp.2 = -0.197(MaxTemp) + 0.313(AvgwindS) + 0.727(5SecWindS) + 0.585(2MinWindS)

But when comp.1 and comp.2 are considered together, 77.8% of the total variance of the

data set can be explained. From above table, it can be observed that by considering up to

comp.3, around 91.7% of the total variance can be explained and by considering up to

comp.4, around 96.5% of the total variance can be explained. The choice of how many

number of components to be considered depends on the amount of variance that is of our

interest. Hence in this case, the total number of dimensions, 8, has been reduced to 4 if

we want to retain 96.5% of the total variance by considering up to comp.4. To our

interest, rain in above table has no contribution at all towards variance, if we consider

until comp.4, hence this variable can be eliminated. Hence the 8 variables can be reduced

to 4 components by preserving 96.56% of the total variance in the data set. Each

component is like a new variable but a linear combination of the actual weather variables.

5.3 ANN Simulation Output

Three management areas--Wingate, North Dade, and Gulf Stream were chosen as

pilot areas in the current artificial neural network (ANN) project. These 3 MAs are

adjacent to each other and small enough to make the assumption that the variation in

weather due to geographical differences is slight. Also, they are all urban MAs and

appear to have a similar distribution of customer types.

Two years, 2000 and 2001, of weather and interruption data were chosen to train

the ANN while 2002 weather and interruption data was used to evaluate the performance

of the trained ANN model. One entry in either the training or evaluation datasets is

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composed of one day’s weather and interruptions for one MA, so the one year evaluation

dataset had 1060 entries (allowing for missing data).

The output of the ANN is two columns of data; a prediction for each entry in the

evaluation dataset and the actual number of interruptions for each entry in the evaluation

dataset. Figure 5-3 is a graph of the predicted values superimposed over the actual values

for the evaluation year 2002. The MAs are in sequence and it can be seen that the

predicted values follow the seasonal trends for interruptions.

2002-Gulfstream 2002-North Dade 2002-Wingate Figure 5-3. Prediction patterns of N overlaid on actual patterns of N of 3 MAs for year

2002

5.3.1 Detailed Observation

Figure 5-4 is an expanded segment (North Dade) of the above graph to highlight

the details. It can be seen that where the actual number of interruptions are large, the

predictions matches the pattern of Max’s and Min’s, but are not always close in

magnitude. Where the actual number of interruptions is small, the pattern matching

breaks down, but large spikes in the predictions do not occur.

The following is a segment of a time series plot of predicted values and actual

values of total daily number of interruptions (N) for North Dade MA. It can be clearly

seen that during some periods (rectangles) the predicted values match the pattern of the

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actual values, if not the magnitude, while other periods (ovals) do not show any such

pattern matching although the magnitudes are small.

Figure 5-4. Predicted N and the actual N for a few of the cases in North Dade MA for

2002

Some of the interesting observations from the above plot, Figure 5-4 are explained below.

Case 1: Predicted N less than actual N. The actual value of N at points 529 and

530, in Figure 5-4, correspond to 6/17/2002 and 6/19/2002 in the North Dade MA. The

interruption data for 6/17/2002 indicates that up to 18 among 28 interruptions that

occurred in 6/17/2002 may not be related to daily common weather (Corrosion/Decay =

10, Improper Process = 6, Request = 2) which suggests that as few as 12 may be weather

related interruptions, which is just the same as the predicted value. Similarly 15 out of 29

interruptions that occurred on 6/19/2002 may not be related to daily weather, which is

close to our predicted value of 12.

Though the weather conditions for these days were relatively mild, we have a

significant increase in the number of interruptions, as shown in Figure 5-5 in the green

box.

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Case 2: Predicted N more than actual N. If we look into the details of the points

549, 550, 551 and 552, these points correspond to 7/8/2002, 7/9/2002, 7/10/2002,

7/11/2002 days of North Dade MA, outlined in red in Figure 5-5. The number of

interruptions for these days was pretty much same though their weather conditions vary

over a wide range. This large change in weather conditions forces the ANN model to

predict N proportional to the weather. So it is really a question one should ask that why

we have small changes in N though we have significant differences in their weather

conditions? Were some precautionary measures, e.g. tree trimming been taken few days

before the happening of these interruptions??

Figure 5-5. Numerical values of weather and interruption data under consideration

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Case 3: In some of the cases there was a very small increase in N though there

were large variations in the weather conditions.

5.3.2 Dominant Weather Parameters - Preliminary Observations

A series of ANN simulations with different weather parameters removed has been

done, and the relative accuracy of each simulation has been compared to determine which

weather parameters are the most significant.

The preliminary results show that only a few of the many weather parameters

account for most of the variation in the number of interruptions. It is expected that the

importance of individual weather parameters will vary with location.

The following list gives the weather variables in accordance with their importance

for the pilot area:

1. Two Minute Sustained Wind Gust (mph) 2. Rain (inches) 3. Lightning Strikes (# of strikes/day) 4. Temperature – Average or Max. & Min.(K)

On the other hand, the following list of parameters which account for the least

variation in the number of interruptions.

1. Pressure 2. Heat Days 3. Cool Days 4. Dew Point 5. Population (of MA)

5.4 Analysis of ANN Simulation Output

Based on the actual number of interruptions and the predictions during the

evaluation year, probability graphs (PGs) have been created to represent the range of

interruptions that actually occurred in the evaluation dataset for each predicted value. For

example, if every number between 1 and 40 interruptions were predicted at some point in

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the evaluation year, there would be 40 PGs. This is done by sub-setting the evaluation

dataset into 40 sets and creating a histogram of actual values for each predicted value in

the evaluation set. By dividing each frequency column by the sum of the interruptions

that comprise the histogram, a probability graph such as the one for a prediction of 11

shown below can be created.

1 2 3 4 5 6 7 8 9 1011121314151617181920212223

0

5

10

15

N Actual

Freq

uenc

y

Histogram

2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22

0

5

10

N ActualP

erce

nt P

roba

bilit

y

1.5267

3.8168 3.8168

5.3435

9.9237

8.3969

9.1603

12.2137

5.3435

7.6336

6.8702 6.8702

3.0534

1.5267

3.8168

3.0534

3.8168

1.5267

0.7634 0.7634 0.7634

Probability Graph

(a) (b)

Figure 5-6. Histogram plot of predicted interruptions

From the histograms, it can be seen that the actual values for each predicted value

follow a generally normal distribution, so it is justified to apply normally calculated mean

and standard deviation to gauge the accuracy and precision of a prediction. The accuracy

would be determined by the closeness of prediction to the mean actual number of

interruptions. The precision would be determined by the magnitude of the percent

standard deviation. Percent standard deviation was chosen to equalize the standard

deviations for lower to higher predictions. Outliers provide clues to elements of the

model that either are missing or should not be there.

Test data is just a single day's weather data; a real-time updated weather parameter

max, min or total from a weather station, a known day's values or a theoretical set of

weather data. The former is used in real-time prediction but the latter can only be used

after the fact and does not provide any predictive benefits, aside from inclusion in the

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historical data set. However, the latter can be used for research, such as modeling a

system's robustness to weather. Test data that shows a very low prediction can be used as

a base and the parameter values can be varied either individually or in groups to model

the response to those parameters.

5.5 Pitfalls and Suggestions to FPL

GIGO is an acronym from the predawn of computing- garbage in, garbage out. The

accuracy and precision of the ANN is limited by the accuracy and precision of the input.

Although there will always be error inherent in the data collected, significant

improvements may be possible.

5.5.1 Weather Data

The error inherent in the ASOS weather data may be geographical and ASOS data

is only available for historic and not real-time use. The installation of dedicated weather

stations that is now occurring at FPL service centers will reduce that inherent error and

allow real-time forecasting.

5.5.2 Interruption Data

Although the FPL data cubes are thorough, the reporting procedures are not

designed for a detailed, time-dependent study such as this, nor are they always sensitive

to the role of weather. Because of this, the accuracy and precision of the prediction

suffers.

An example is that a day on which an interruption may be reported runs three shifts

from 7 AM to 7AM. In the last random sample made, the last shift, from 11 PM to 7AM,

reported about 12% of the day's interruptions; meaning that from midnight to 7AM the

interruptions were being reported on the previous day. This can be largely accounted for

by taking data from the cube by shifts and summing, however that still leaves 11PM to

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midnight, or maybe 1-2% of the interruptions, reported on the wrong day. Because the

data was only shifted in time, the average difference after adjustment was only 0.05

interruptions; however, because of many instances where a large number of interruptions

were reported on the previous day, the average percent difference was 14%.

To determine the effect on the output of this error, two sets of data were taken from

the same time period and location, an original one with 24 hours of interruption data

taken from the cube on the day it was reported and an adjusted one with 24 hours of

interruption data taken from the beginning of the third shift on the day before it was

reported. Both were run through the ANN and the results compared. The following

detailed graphs of the same time period in the same MA show an improvement in the

pattern and magnitude matching after the interruption data were adjusted for the shift

differences.

Figure 5-7. Prediction results of ANN using the original N (not shift adjusted)

Mean and Standard deviation plots for the actual N vs predicted N and adjusted N

vs predicted N were plotted as shown in Figure 5-9 and Figure 5-10. It can be observed

that adjusting the data to include the correct shifts on the correct days improves the fit of

the prediction to the mean actual number of interruptions. It also shows that the fit

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Figure 5-8. Prediction results of ANN using the adjusted N (shift adjusted)

deteriorates as the prediction increases, indicating unknown factors. The graphs of the

original, Figure 5-9, and shift-adjusted percent standard deviation, Figure 5-10, show a

reduction in the adjusted %Standard Deviation at lower predictions while the higher

predictions are not much improved, similar to the graphs of the means.

5 15 25 35

10

20

30

40

prediction

Mea

n A

ctua

l

5 15 25 35

10

20

30

40

50

60

70

80

90

100

Prediction

Act

ual %

StD

ev

(a) (b)

Figure 5-9. Mean and standard deviation of actual N

5 15 25 35

10

20

30

40

prediction

Adj

Mea

n A

ctua

l

5 15 25 35

30

40

50

60

70

80

90

100

Prediction

Adj

uste

d %

StD

ev

(b) (d)

Figure 5-10. Mean and standard deviation of adjusted N

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These results suggest that there are other improvements that can be made in the

data reporting. Not one change would have as visible an effect, perhaps, but taken

together they could alter the results significantly. Some possibilities suggest themselves:

• Report interruption requests due to weather related damage repair on the day the causative weather condition occurred.

• Maintain an hourly database for interruptions since hourly weather is available. This would be especially useful if dedicated weather stations existed.

• Update cause codes to be more sensitive to the possible role of weather.

• Report Age of equipment

Simulations that have been run with different cause codes subtracted from the

interruption data, such as accident, animal, improper process and crew request (planned)

have shown similar improvements in differing regions of the graphs.

5.6 Proving Localization of Weather Improves the Accuracy in Prediction

Case 1: Localized Weather Data

Three areas Wingate, North Dade, and Gulf Stream were chosen for study as pilot

areas, which are adjacent to each other. Weather and Interruption data for each of the

MAs were considered for years 2000 and 2001 and were used to train the ANN model.

While Year 2002 weather data of the North Dade area was chosen to predict using the

built trained ANN.

The mean percentage error (MPE) of the predicted value is 25% (approximately)

The mean percentage error (MPE) is calculated using the following formula:

MPE = ∑ −Nactual

NpredictedNactualModM

)(1

Where M = Total number of cases considered Nactual = Actual number of N happened Npredicted = Predicted number of N

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Case 2: Scattered Weather Data

Contrary to taking weather data from each of the weather stations, only one weather

station was chosen for weather data while the interruption data was taken from all the 3

management areas.

The mean percentage error of the predicted value is 35% (>25%)

This shows that with the increase in the accuracy of weather, by considering the

smaller areas, there are chances to enhance the performance of the model.

5.7 Comparison of Statistical Model and ANN Model

A comparison of the prediction performance between statistical and ANN model

was done using the 2000 and 2001 weather and interruption data of Gulf Stream (GS),

North Dade (ND), and Wingate (WG) of FPL . In the process, three variables – Rain,

2Minutes Maximum Wind Gust and Average Temperature were considered in building

the above two models. A multiple regression equation was developed for the above three

variables as given below:

N = -16.6 + 0.174 *AvgTemp + 4.71* Rain + 0.852 *2MMaxS

The 2002 weather data of ND is used to predict N using the above equation. On the

similar lines, ANN model was developed with 3 input variables, 5 hidden nodes and 1

output node. The same data set which is used for the statistical model is used in

evaluating the ANN model. The results of both the models are tabulated in Table 5-1.

Table 5-2. Performance Comparison Between Statistical Model and ANN Model Statistical Model ANN Model

Mean % Error 67 45 Prediction with 30% Error 46 54

The above results show that the prediction accuracy of the ANN model is better

than the statistical model. Though the actual predicted figures of accuracy from both the

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models are less, as we considered only few variables to make the problem easy, the point

here is to show that the ANN model is better.

Figure 5-11. Mean squared error vs. training epochs

Figure 5-11 shows that the mean square error is gradually getting decreased with

the training of ANN for each epoch (a complete set of training data). The progress of

training is diagnosed by looking into the training, validation and test errors. The training

stopped after 40 epochs because the validation error increased. The result here is

reasonable, since the test set error and the validation set error have similar characteristics,

and it doesn’t appear that any significant over fitting has occurred.

5.8 Possible Software Development to Predict Power Interruptions Using ANNs

The following Figure 5-12, is a snap shot of the graphical user interface (GUI)

development of the ANN that had been trained to predict the interruptions.

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Figure 5-12. Graphical user interface developed to predicted interruptions

Using above interface model, Figure 5-12, is simple: We have to first load the training

and testing data files (ASCII format) using the options buttons provided and then click on

the “Run Simulation” button to see the above plots.

Currently, the development of custom software to predict the power distribution

interruptions, based on the idea provided in the current thesis, is in progress. The

proposed prediction model is under test at FPL management areas. The custom software

can be easily installed just like any other software on the user desktop and is just a click

away to know the power interruptions in advance. In the future, the software will be

distributed to other power utilities in USA.

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Using the model shown in Figure 5-12, it can also be possible to get similar kind of

predictions as shown in Figure 5-13.Central Dade management area (MA) has been

chosen as one of the pilot areas to see how well our developed model can predict the

interruptions. It can be seen that the correlation coefficient R2 is around 90 which means

the model is doing pretty good job in predicting the interruptions close to the actual

number of interruptions. The X-axis of figure 5-13(a) shows the predicted sum of

monthly interruptions while the Y-axis shows the actual sum of monthly interruptions

happened. This estimate of predicted interruptions will help the utilities to know in

advance how much personnel they need to deploy to manage the interruptions.

Sum Predicted

Sum

Act

ual

550500450400350300250200150

600

500

400

300

200

100

S 32.3396R-Sq 90.2%R-Sq(adj) 89.9%

Central Dade 2001-2003 Monthly Total NSum Actual = - 1.84 + 1.060 Sum Predicted

(a)

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Month

Y-D

ata

129630

600

500

400

300

200

129630

600

500

400

300

200

2001 2002

2003

VariableSum ActualSum Predicted

Panel variable: Year

Scatterplot of Sum Actual, Sum Predicted vs Month for Central Dade

(b)

Figure 5-13. Predicted interruptions vs. actual interruptions for Central Dade (a) 3 years plotted together (b) each year plotted separately

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CHAPTER 6 LIMITATIONS, CONCLUSIONS AND FUTURE WORK

The research results presented in this thesis are not with their own limitations.

Some of the hurdles that need to be overcome to get better results were discussed in this

chapter. The conclusions of the current thesis are followed by the future work explaining

about the steps that are to be followed from the current state of the project.

6.1 Limitations of Approach

6.1.1 Weather Data

There are two types of weather parameter measurement errors. First, we found that

the weather parameter measurement in an airport is not accurate as expected. Second, the

distance between the location of outages and the airport, where weather parameters are

measured, is up to 10 miles. The weather conditions in two locations for certain weather

parameters can be significantly different (Figure 6-1). However the rain difference

presents a normal distribution with mean close to zero. Therefore, rain data can be used

for nearby locations without changing the results.

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0

0.2

0.4

0.6

0.8

1

1.2

1.4

1.6

1.8

2

11/20/2000 1/9/2001 2/28/2001 4/19/2001 6/8/2001 7/28/2001 9/16/2001 11/5/2001 12/25/2001 2/13/2002

Time

Avg

diff

=(|R

1-R2

|+|R

1-R

3|+|

R2-R

3|)/3

(a)

(b)

Figure 6-1. Average precipitation difference (a)for 3 weather stations in Fort Lauderdale (b) showing less than 9 miles distance between each weather station

6.1.2 Unknown Variables

There are many explanatory variables that would contribute to the response. Some

of these are different weather parameters, but other variables are most likely specific to a

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system and would best be identified by utility employees who are familiar with the

system.

6.1.3 Outliers

It is possible to find aberrant observations among the data set, without any clear

explanation of the cause. These sort of outliers must me study independently.

6.1.4 Hourly Data

From the number of interruption database FPL provided, the lowest reachable level

is “daily basis”. However, for any interruption studied it is necessary to know the exact

time, at the hour level or even at the minute level as shown in [10-11].This is needed to

study different weather parameters at the given outage time since the weather varies for

each and every hour.

6.2 Conclusions

The ANN and statistical analysis of the ANN output has the potential to provide

powerful modeling tools, and can be used to provide limited real-time prediction. The

accuracy and precision of the model is dependent as much on the input as the ANN

model.

The graphical output of the ANN can be used by itself or in conjunction with the

statistical analysis to compare the accuracy and precision of the ANN model with

different variable selections, principal components, study areas or times. In some cases,

the graphical representation can provide better clues to the performance of the ANN than

the graphs of means and percent standard deviations.

With the ever increasing demand for more and more electricity every year, the need to

look for the better ways in preventing the interruptions due to over loading of the power

distribution equipment has drawn much attention.

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ANNs have been already applied in power systems in the areas of Economic Load

Dispatch, Optimization and Loss Reduction, Fault Detection and Diagnosis, Frequency

Control, Load Forecasting, Contingency analysis, static security assessment, Voltage and

Reactive Power Control etc. But, not much research work can be found either online or in

the IEEE publications regarding the application of ANNs for the prediction of power

distribution interruptions. This novel idea seems very promising in letting the utilities

know and alert them in advance about the number of interruptions that are going to

happen in future. This helps to optimize their crew by mobilizing them to the location of

interest and take proper action more effectively to avoid interruptions/ respond quickly in

restoring the power due to interruptions. This further helps in reducing the SAIFI value.

The utilities can predict SAIFI as they would be able to predict the total number of

interruptions and can use it in their internal calculations. The developed ANN model can

be further enhanced in predicting the extra information like time slot and location of the

occurrence of these interruptions besides revealing their approximate number, for which

all we need to do is to provide the extra information as input columns while training the

model. The accuracy of the predicted results is directly proportional to the accuracy of

the information provided in the training data which is used to train the model.

A basic methodology that is easily automated has been proposed. The methodology

promises to be easy to use and flexible enough to perform in both a real-time predictive

and a theoretical modeling mode.

6.3 Future Work

The following future steps will improve the accuracy of the current analysis.

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6.3.1 Data Collection and Creating New Variables

Additional data collection is necessary. It is suspected that a change in power usage

or equipment density might cause outage trends over time. To verify this idea, we need to

develop a scaling factor and collect usage data. This scaling factor would consist of

information such as equipment density and length of lines- daily power usage data would

be an additional explanatory variable. Also, this new data might be useful in comparing

management areas because the probability of interruptions occurring may be proportional

to the scaling factor. The more the new input variables of the system

6.3.2 Improving the Accuracy and Developing New ANN Models

• Other types of ANN such as RBF, LVQ, SOM or their combinations need to be

tested to see which of the model gives better prediction results.

• The dimension of input feature space/ input feature pattern needs to be reduced to

improve performance such as speed, prediction accuracy

• If the prediction variable(s) are more than one (multi-output rather than single

output), the architecture of whole system may be either a multi-input multi-output

ANN or the composition of several multi input-single output ANNs. The training

method as well as performance should be further investigated and compared.

• Develop an enhanced custom software model with Graphical User Interface,

where the user will have the options of selecting new input and output datasets to

train ANN and develop a model to predict the output. Hence, user can reuse this

tool every time he wishes to create new model / renovate the existing model.

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LIST OF REFERENCES

1. IEEE Trial-Use Guide for Electric Power Distribution Reliability Indices, IEEE Std 1366-2001, IEEE, New York, 1999.

2. 2001 Cost of Downtime, Contingency Planning Research (CPR) and Contingency Planning & Management Magazine (CPM). Website http://www.contingencyplanningresearch.com (accessed on December 2001).

3. C. A. Warren, Overview of 1366-2001 the Full Use Guide on Electric Power Distribution Reliability Indices, Power Engineering Society Summer Meeting, IEEE, Volume 2, 2002.

4. Transmission Line Reference Book, 345kV and Above/Second Edition. Electric Power Research Institute, Palo Alto, CA, 1982.

5. Florida Power and Light website http://www.fpl.com (accessed June 2004)

6. Thomas E. Grebe, D. Daniel Sabin, and Mark F. McGranaghan, An Assessment of Distribution System Power Quality: Volume 1: Executive Summary. EPRI Report TR-106294-V1, Electric Power Research Institute, Palo Alto, California, May 1996.

7. D. Daniel Sabin, An Assessment of Distribution System Power Quality, Volume 2: Statistical Summary Report. EPRI Report TR-106294-V2, Electric Power Research Institute, Palo Alto, CA, May 1996.

8. Daniel L. Brooks and D. Daniel Sabin, An Assessment of Distribution System Power Quality: Volume 3: The Library of Distribution System Power Quality Monitoring Case Studies. EPRI Report TR-106294-V3, Electric Power Research Institute, Palo Alto, California, May 1996.

9. National Climatic Data Center (accessed June 2004), Website http://nndc.noaa.gov/?http://ols.ncdc.noaa.gov/cgi-bin/nndc/buyOL-002.cgi.

10. A. Domijan, Jr., R. K. Matavalam, A. Montenegro, W. S. Willcox, Y. S. Joo, L. Delforn, J.R.Diaz, L.Davis, and J. D'Agostini, Effects of Normal Weather Conditions on Interruptions in Distribution Systems, International Journal of Power and Energy Systems, Publication No: 203-3453.

11. J. M. Zurada. Introduction to Artificial Neural Systems. West Publishing Company, St. Paul, MN, 1992.

67

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12. L. F. Garcia, and O.A Mohammed, Forecasting Peak Loads with Neural Networks, Southeast Conference. Creative Technology Transfer––A Global Affair, Proceedings of the 1994 IEEE, pp. 351 – 356, 10-13 April, 1994.

13. S. I. Wu, Mirroring our Thought Processes. IEEE Potentials 14, 36-41, 1995

14. Neuron Model & Network Architectures, Neural Networks Toolbox, MATLAB 6.0 Manual, Chapter 2.

15. W.M. Huang and R.P. Lippmann. Comparisons Between Neural Networks and Conventional Classifiers, Proc. IEEE Int. Conference on Neural Networks, pp. 485-493, 1987.

16. J.L Chen, and Chang, S.H, A Neural Network Approach to Evaluate Distribution Systems Engineering, IEEE International Conference on Neural Networks, pp. 487 – 490, 17-19 Sept. 1992.

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BIOGRAPHICAL SKETCH

Roop Kishore R. Matavalam was born in Tirupati city, Andhra Pradesh state, India.

He received his Bachelor of Technology (B.Tech) degree in 2001 specializing in

electrical and electronics engineering from Sri Venkateswara University, India. Since Fall

2001 he has been pursuing his Master of Science degree in electrical and computer

engineering at University of Florida, Gainesville. He has been working as a research

assistant, since 2001, in Florida Power Affiliates and Power Quality Laboratory,

University of Florida. His fields of interest include power reliability, power electronics,

analog circuit design and RF micro electronics.

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