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Terms of Reference
1. Focus on illustrating how statistical methods are used to solve business problems and how statisticians interact with colleagues and clients to achieve this.
2. Descriptions of past and on-going case studies
3. Short introductions to their organisations and to the diverse roles of the organisation’s statisticians,
Models
HistoricBasics
WEATHERfrom Met Office
(Actual and forecast)
Reading UniversityRSS 15th June 2005
Shanti Majithia
Forecasting Development Manager
Wokingham, Berks
UK Transmission
Agenda
My Background
Company Background
Application of Statistical techniques within the Company
University and Project work
Conclusion
My Background
Further education in London Maths Stats and Computing
Market Electricity Load research, Manpower planning
Operational Forecasting (Short Time Scale)
Liaison with students and Uni. to assist in data and direction
Presentations: Research paper and Forecasting conferences
Wind Energy, Climate Change, Heating and Cooling Load ( Air Con)
Risk management
Short term Gas Demand and Supply Forecasting
Translating data, analysis and information into decision making tools
Argentina:27.6% Transener
Zambia:38.6% CEC(Copperbelt transmission)
Australia:Basslink (Interconnector to Tasmania)
UK:E&W transmissionGB Gas TransportationLNGGridCom
USA: NEESCom
National Grid Transco - principal activities in regulated electricity and gas industries
Over 21,000 Transmission Towers
Over 13,000 circuit kmof 400 & 275kvtransmission lines and cables
Fibre optics
National Grid - UK : Electricity
300 substations
Electricity
Balance generation and demand efficiently
Ensure quality and security
Non stop process
Keeping the lights onKeeping the lights on
Electricity Transmission Elements
96/29355 ISSUE A SH. 1 OF 1 30-04-99
Power Station
GeneratorTransformer
Transformer
33 kV
To Small Factories, Farms,
Residential Areas and Schools
Large Factories,Heavy Industry
Medium Factories,
Light Industry
11 kV 240 V
132kV
23kV 400kV
}
40 % of Distribution
TRANSCO & IPGTS
TRANSCO
Suppliers
• Producers
• DFO’S
• Storage Operators
• Shippers
• Traders
The UK Gas Industry Model
Competitive Monopoly
Energy Companies Regulated Systems
Gas supply Independent transmission
6300 km Pipelines
CompressorsRegulators
St. Fergus
Teesside
Easington
Rough
TheddlethorpeBacton
Barrow
Terminals
Burton Point
Gas: National Transmission System (NTS)
• 6,600km 450-1220mm diameter pipeline• High strength steel X65-X80 • Operating pressure design
70-94bar• 7 Transco terminals• 24 compressor stations• 400 above ground installations (AGI)
Key Stats• Max demand 02/03 205 GW• Peak Demand (1/20) 240 GW• Energy Supplied 1150 TWh/yr
Compressor
Salt cavitystorage
LNGstorage
LDZ Offtake
Regulator Station
Governor
Meter
CUBIC FEET
0 0 1 2 6 5
High pressure storage
Low pressurestorage
Industry
Terminal
Power Station
Gas: From Beach To Meter
Balance supply and demand efficientlyBalance supply and demand efficiently
Facilitate the marketFacilitate the market
Ensure quality and securityEnsure quality and security
Maximise system capacityMaximise system capacity
Non stop processesNon stop processes
BUTBUT
Gas can be stored => daily balancingGas can be stored => daily balancing
Electricity can’t => real-time balancingElectricity can’t => real-time balancing
Real Time System Operation in Gas and Electricity…..
Application of Statistical Techniques within NGT
Data collection - live metering, market intelligence and field measurement
Data mining e.g. Kohonen SOMs, Genetic Algorithms.
Forecasting Methods
Regression, Box-Jenkins, Bayesian, Neural Network (MLP & ALN), Curve fitting and Holts-Winters, Arch and Garch
Probability and Risk Management
Liaison to keep abreast of modern methods e.g. Statistical methods
Management Information System
Area of Application of Statistical Techniques
Forecasting Energy Demand
Trading advice
Minimising of volatility
Management of probability and risk
Calculating and calibrating climate sensitivity
Health of the assets in terms of the return period
Simple use of statistical methods in plant reliability
Responses on the efficiency of the equipment
Electricity Forecasting Techniques
Multiple linear regression
Last 3 years of historic data
Summer (BST) and winter (GMT)
Weekdays / Sat / Sun
Special days excluded
‘Conventional’ and ‘Trend’ models
~ 120 models per annum
Interpolation between cardinal points for half hourly resolution
Forecasting Tools
Oracle database Weather and demand feeds StatGraphics EViews SAS PREDICT & Forecaster Clementine NN and ALN Genetic Algorithm Library (MIT)
Weather Input
Historical Demand Input
Mathematical& Statistical
Models
The Forecast
The Forecasting Process
Demand - Influences
Seasons/ Weather
“Exceptional events”
TV
00:00 02:00 04:00 06:00 08:00 10:00 12:00 14:00 16:00 18:00 20:00 22:00 24:00
15
20
25
30
35
40
45
50
55
Typical Summer Day
Minimum Summer Day
Typical Winter Day
Maximum Winter Day
GW
NGC System demand during 3 minute silence on 14 September 2001 in memory of the tragedy in America
35000
35500
36000
36500
37000
37500
38000
38500
Dem
and
200
1
33000
33500
34000
34500
35000
35500
36000
36500
Dem
and
199
9
3 minute silence
Remembranceday 1999Eclipse 11-08-99
Previous Drop on the 11 August 1999 - 2200MW The Solar Eclipse
The start of the Drop, just before 11:00
2700MW Highest ever drop in Demand.
Remembrance Day 1999 gave a 750 MW drop
13 minute duration
The Effect of Temperature on Demand
0
1000
2000
3000
4000
5000
6000
7000
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30Temperature
Dem
and
Eff
ect
(MW
)
COLDHigh Demand
Comfortable
HOTHigh Demand
Degrees Centigrade
The Effect of Illumination on Demand
0
500
1000
1500
2000
2500
3000
3500
4000
4500
0 5 10 15 20 25 30 35 40 45 50 55 60 65 70 75 80 85 90 95 100 105 110 115 120 125 130 135 140 145 150 155 160
Logarithmic Function of Illumination
De
ma
nd
Eff
ec
t (M
W)
DULLHigh Demand
BRIGHTLow Demand
Four Weather Variables
• Average Temperature [TO]: average of 4 spot hourly temperatures up to current hour
• Effective Temperature [TE]: TO lagged to 50% with TE from 24 hours previous
• Cooling Power of the Wind [CP]: empirical combination of temperature and wind speed
• Effective Illumination of the Sky [EI]: (EI=MI-ID), where ID is a function of visibility, numbers and types of cloud layers and amounts of precipitation and MI is maximum illumination. In the logarithmic domain.
Winter Week Day Peak Demand ModellingMultiple Regression Model Of Demand
Weekday Darkness Peak Demand =
+ Weather Dependant Demand
+ Day of Week
An econometric regression model of the weekday darkness peak is determined on the four previous winters demand & weather data
+ Seasonal trends
+ error terms
The days affected by Christmas & New Year holidays are excluded from the sample
Mean Darkness Peak Demand
Weather Dependant Demand
Weather Dependant
Demand functionTEt+2TEt
2+EIt+CPt
Example of a Weather forecast data
Example 1: MG3 file for receiving Forecast Data (Samplefile format for 0800 bulletin.)
‘A00’,’MG3’,’19082002’,’073030’,007‘D00’, ‘19082002’, ‘080000’‘D10’, 1,,
‘D01’, ‘LON’, ‘19082002’, ‘090000’, 15.0, 0,,,‘D01’, ‘LON’, ‘19082002’, ‘110000’, 15.0, 0, 04, 0, ‘SSW’‘D01’, ‘LON’, ‘19082002’, ‘130000’, 15.0, 0,,,‘D01’ ‘LON’, ‘19082002’, ‘150000’, 15.0, 0, 04, 0, ‘SSW’‘D01’, ‘LON’, ‘19082002’, ‘170000’, 15.0, 0,,,‘D01’, ‘LON’, ‘19082002’, ‘190000’, 15.0, 0, 04, 0, ‘SSW’‘D01’, ‘LON’, ‘19082002’, ‘210000’, 15.0, 0,,,‘D01’, ‘LON’, ‘19082002’, ‘230000’, 15.0, 0, 04, 0, ‘SSW’‘D01’, ‘LON’, ‘19082002’, ‘010000’, 15.0, 0,,,‘D01’, ‘LON’, ‘19082002’, ‘030000’, 15.0, 0, 04, 0, ‘SSW’‘D01’, ‘LON’, ‘20082002’, ‘050000’, 15.0, 0,,,‘D01’, ‘LON’, ‘20082002’, ‘070000’, 15.0, 0, 04, 0, ‘SSW’‘D01’, ‘LON’, ‘20082002’, ‘090000’, 15.0, 0,,,‘D01’, ‘LON’, ‘20082002’, ‘110000’, 15.0, 0, 04, 0, ‘SSW’‘D01’, ‘LON’, ‘20082002’, ‘130000’, 15.0, 0,,,‘D01’, ‘LON’, ‘20082002’, ‘150000’, 15.0, 0, 04, 0, ‘SSW’‘D01’, ‘LON’, ‘20082002’, ‘170000’, 15.0, 0,,,‘D01’, ‘LON’, ‘20082002’, ‘190000’, 15.0, 0, 04, 0, ‘SSW’‘D01’, ‘LON’, ‘20082002’, ‘210000’, 15.0, 0,,,‘D01’, ‘LON’, ‘20082002’, ‘230000’, 15.0, 0, 04, 0, ‘SSW’‘D01’, ‘LON’, ‘20082002’, ‘010000’, 15.0, 0,,,‘D01’, ‘LON’, ‘20082002’, ‘030000’, 15.0, 0, 04, 0, ‘SSW’‘D01’, ‘LON’, ‘19082002’, ‘050000’, 15.0, 0,,,
Gas Forecasting - suite of models using different techniques
Profile (ARIMA)
STF (Complex regression)
Neural network
ALN (Adaptive logic network)
Inday (Simple regression)
Bayes (Complex regression)
Box 1 (Box Jenkins)
Box 2 (Box Jenkins)
Sumest (Complex regression)
Wintest (Complex regression)
D-1
D-1
D-1
D-1
D-1
D-1
D-1
D-1
D-1
Averageweighted according to
performance over last 7 days (Combination). Further adjustment made based on
recent combination error (CAM)
D
D
D
D
D
What Does a Gas Model Look Like?
PROFILE – WITHIN DAY MODELPROFILE – WITHIN DAY MODEL
PROFILE model uses the Box Jenkins technique to forecast within day gas demand. There are two different models in the program. Model 1 is usually used for the 10am forecast and model 2 for the rest of the day. However, if the 9am temperature is greater than either the 1pm or 3pm temperature then model 1 is used for the 1pm and 4pm forecasts.
Model 1 (at hour k) (used for 10:00 forecast)
7Dt(h) = w07Tt
(3) + w17Tt(6) + w27Tt
(9) + w37Dt(k) + (1-1B) (1-7B
7) at
Model 2 (at hour k) (used for forecasts at other times)
7Dt(h) = w07Tt
(h-1) + w17Dt(6) + w21
k7Dt(j) + (1-1B) (1 - 7B
7)at
where Tt(h) is the temperature at hour h on day t,
Dt(h) is the corresponding hourly demand on day t,
at is the error in the forecast demand for hour h on day t,
B is the backward shift operator i.e. Byt = yt-1
w0, w1, w2, w3, 1, 7 are model parameters.
.
PROFILE model uses the Box Jenkins technique to forecast within day gas demand. There are two different models in the program. Model 1 is usually used for the 10am forecast and model 2 for the rest of the day. However, if the 9am temperature is greater than either the 1pm or 3pm temperature then model 1 is used for the 1pm and 4pm forecasts.
Model 1 (at hour k) (used for 10:00 forecast)
7Dt(h) = w07Tt
(3) + w17Tt(6) + w27Tt
(9) + w37Dt(k) + (1-1B) (1-7B
7) at
Model 2 (at hour k) (used for forecasts at other times)
7Dt(h) = w07Tt
(h-1) + w17Dt(6) + w21
k7Dt(j) + (1-1B) (1 - 7B
7)at
where Tt(h) is the temperature at hour h on day t,
Dt(h) is the corresponding hourly demand on day t,
at is the error in the forecast demand for hour h on day t,
B is the backward shift operator i.e. Byt = yt-1
w0, w1, w2, w3, 1, 7 are model parameters.
.
NTS Supply Forecasting Model types
Every supplypoint
End of
dayWithin
dayRegression of DFNs & AT-Link nomsEvery
hour
When For What Horizon How - Model type
Nat End of
dayWithin
dayRegression of DFNs & AT-Link nomsEvery
hour
Every supplypoint
End of
day
Day ahead Regression of change of supplyEvery
hour
Every supplypoint
Every hour
7 days ahead
Holts-Winters (Time series)Once per day
What is a Holts-Winters Model?
stt
tt
tttt
ttst
tt
SL
YS
bLLb
bLS
YL
1
1
1
11
11
where s is the length of the seasonality. L is the smoothed level of the series, bis the trend of the series and S is the seasonality component.
The Forecast uses the following equation;
stttt SbLF
Understanding Data Questions
What to look for in the data before preparing forecasts
How to treat data when “problems” are recognised
How to prepare forecasts using different models and techniques
When each forecasting model is appropriate
How to use forecasts effectively after they are prepared
Why is a forecast needed?
Who will use the forecast, and what are their specific requirements?
What level of detail or aggregation is required and what is the proper time horizon?
How accurate can we expect the forecast to be?
Will the forecast be made in time to help decision making process?
Does the forecaster clearly understand how the forecast will be used in the organisation?
Key Questions
Projects and Case Studies
The seasonal forecast of electricity demand: asimple Bayesian model with climatological
weather generator
Sergio Pezzulli, Patrizio Frederic, Shanti Majithia,
Coloured areas are clusters, each with a distinctive daily demand profile. Red text is their interpretation.
Data mining --- Clustering of Electricity Profiles
Clustering of Gas Profiles
Kohonen Network (SOM) Analysis
Yellow-ish areas indicate similar profiles, Red-ish areas indicate more varying profiles.
Jan & Dec
Jan Feb Mar & Nov
Apr May & Oct
June July Aug & Sept
Forecast DemandLondon
0.5
1
1.5
2
2.5
1 9 17
25
33
41
49
57
65
73
81
89
97
105
113
121
129
137
145
153
161
169
177
185
193
201
209
MC
M
1 Day Lag Forecast
Real Demand
-0.3
-0.2
-0.1
0
0.1
0.2
0.3
1 10 19 28 37 46 55 64 73 82 91 100 109 118 127 136 145 154 163 172 181 190 199 208
Error
North Thames LDZ, Early Jan 2003
New up coming Challenges
Windpower
Variable
Uncertain
Uncertain uncertainty
Danger: possibility of sudden loss
Weather differences can be at finer geographic resolution
Volatility and UncertaintyHow best to model? Ensemble forecasts?How to make operational decisions?
Site Clustering
Site clustering can be used to produce a more accurate national prediction by taking local conditions into account
The main way of achieving this is to have a ‘reference’ farm which is representative of the cluster
It is possible to then use cluster predictions as inputs to a national model or simply upscaled
One further thought is to forecast both a reference farm and a cluster separately and use them to create a more stable regional prediction
Daily Load Forecasting using ARIMA-GARCH and Extreme Value Theory
University of Loughborough EPSRC Project
Application
Climate Change Impacts on Electricity demand can be categorised into a long term (monthly) and short term (daily and hourly) load forecast.
Long term load forecast using the multiple regression approach completed. The results are satisfactory. 80 years projection requires the UKCIP scenario and BESEECH data (population, GDP, consumer spending).
Short term load forecast using Box Jenkins and Extreme Value Theory is also completed. Waiting for hourly climate data from BADC and CRU before we can extend our daily/hourly projections to 2080s.
ARIMA (p, d, q) Model
The AutoRegressive Integrated Moving Average (ARIMA) model is a broadening of the class of ARMA models to include differencing.
Reason: daily and hourly pattern are volatile and shows a strong seasonal pattern. p: no. of autoregressive terms, d: the number of non-seasonal differences and q = no of lagged forecast errors in the prediction equation.
q
j noisewhite
t
d
kregressor
k
ragemoving ave
jtj
p
iregressiveauto
i ktXityCty1 11
, ˆ
ARIMA(1,1,1) is used
Probability Distributions
nt is a standardized, independence, identically distributed (iid) random draw from some probability distributions.
3 distributions are used for this purpose:-
a) Normal
b) Student-t
c) Extreme Value Distribution
For quantiles > 0.95, extreme value distribution is used.
Example of Scenario Forecasting (with max and min scenarios)
17000
19000
21000
23000
25000
27000
29000
31000
33000
HALF-HOURLY
MW
Forecast issued on Friday 12:00hrs
Maximum risk scenario
Minimum risk scenario
Actual
Combination of Distribution-- ExampleLink between Annual Peak and Weekly Peak
The density traces shows how the median of the simulated winter peak distribution cuts off an area of about 12% on the corresponding distribution of simulated weekly peak demands.
VariablesSimulated Weekly Peak DemandSimulated Winter Peak Demand
Density Traces
dens
ity
47 48 49 50 51 52 53 54 55 56 57 58 59 60GW
0
0.5
1
1.5
2
2.5
3(X 0.0001)
Winter ACS Median
12% Area cut off
Weekly Peak
Distribution
Probability Distribution
51000
52000
53000
54000
55000
56000
57000
58000
59000
60000
61000
620000 5 10 15 20 25 30 35 40 45 50 55 60 64 69 74 79 84 89 94 99
%
MW
Conclusions
Various statistical applications demonstrated
Wide variety of Statistical method used in data rich Energy business
Opportunity for Statistician/Business Analysis