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The State of the Art in Short-term Prediction of Wind Power
Dr. Gregor GiebelDTU Wind EnergyAnd numerous co-authors, not all knowingly…
SANEDI, Sandton, South Africa, 19 Sept 2017
DTU Wind Energy, Technical University of Denmark
Outline
•Why predictions? and for whom?
•Predictions: The general information flow
•Some actual implementations
•Some knowledge from research
•Best Practice
DTU Wind Energy, Technical University of Denmark
State-of-the-Art for Wind Power
DTU Wind Energy, Technical University of Denmark
State-of-the-Art in Short-term Prediction
DTU Wind Energy, Technical University of Denmark
State-of-the-Art in Short-term Prediction
111 pages>380 references>700 citationsDOI: 10.11581/DTU:00000017
DTU Wind Energy, Technical University of Denmark54 18 September
2017
Sou
rce:
Win
dEur
ope
Dai
lyW
ind
new
slet
ter,
val
id for
13
Sep
t20
17.
DTU Wind Energy, Technical University of Denmark
Record in DK: 140% wind power!Low demand and high wind production in a summer night.Here given for all of Denmark.
Source: www.emd.dk/el/
59 18 September
2017
DTU Wind Energy, Technical University of Denmark
Smoothing
DTU Wind Energy, Technical University of Denmark
All Europe is connected
The
imag
e is
of 1
997,
but
it’s
not m
uch
chan
ged
since
then
However, local or cross-border transmission can be a bottle-neck
DTU Wind Energy, Technical University of Denmark
Data from 60 meteorological stations
•One year of three-hourly wind speed data from (mostly) 10 m
•Also many inland sites
•Then spatially averaged over all time series at every time step
•=> Total generation profile is less variable!
DTU Wind Energy, Technical University of Denmark
Cross-correlation versus distance
• Calculate cross-correlation
coefficient between every
pair of stations
• Result: Cross-correlation
decreases with distance
• Exponential fit has shape
parameter of ca. 700 km
0 1000 2000 3000 4000 5000-0.4
-0.2
0.0
0.2
0.4
0.6
0.8
1.0
Cor
rela
tion
coef
ficie
nt (l
ag=0
hou
rs)
Distance [km]
DTU Wind Energy, Technical University of Denmark
Users
DTU Wind Energy, Technical University of Denmark
Users of forecasts
Who needs forecasts:
• Transmission companies in areas with high wind penetration (egEnerginet.dk, Tennet, 50Hertz, Red Electrica de España, CaISO, AEMO, ESKOM…)
• Wind power owners/operators with own market access (Iberdrola, DONG, Vattenfall, RWE Innogy, Vindkraft, DTEK, …)
• Electrical utilities (eg DONG Energy, Vattenfall, Acciona, Iberdrola, E.On, NUON, RWE, EnBW, ESKOM…)
• Everyone trading on markets with sizeable shares of wind power
DTU Wind Energy, Technical University of Denmark
Thomas Ackermann about TSOs
Source: 1st Workshop on Short-term Forecasting, Uni NSW, Sydney (AUS), December 2005
DTU Wind Energy, Technical University of Denmark
Level of users 2016
AU.SA
Slide source: Waldl: Operational wind & solar power forecasting - The Perfect Wind Power Prediction. Talk on the 1st Workshop on Large-scale Grid Integration of Renewables in India, Dehli, 6-8 Sept 2017
DTU Wind Energy, Technical University of Denmark
Timescales for wind forecasts
Source: The Future of Wind. White paper on Wind Power Monthly Expert reports, MetOffice, 2013
Min/sec
http://www.wpmexpertreports.com/Whitepaper/The-Future-of-Wind
DTU Wind Energy, Technical University of Denmark
Cost functionsDifferent users have different cost functionsEven within their organisationsMight not even be obvious for themUses:• trading wind power• definition of reserve requirements• unit commitment and economic dispatch• operation of combined wind-hydro• operation of wind associated with storage• design of optimal trading strategies• electricity market design• etc.
DTU Wind Energy, Technical University of Denmark
Strategic bidding vs TSO responsibilityREE showed first that aggregating the forecasts coming from the marketparticipants was worse than their in-house state-of-the-art tool
• Due to better information available at the TSO• Forecasts had variable quality (usually coming from the lowest bidder,
not necessarily the best)• Potential for strategic bidding of the market participants:
– E.g. allowing for a +- 20% corridor means that bidding the fullvolume increases the risk of error – safe bid is 80% max.
Requires online SCADA data at TSO, including active power, curtailment, maintenance information, …Often mandated in grid codes.
86 18 September
2017
DTU Wind Energy, Technical University of Denmark
PredictionsHowTo
DTU Wind Energy, Technical University of Denmark
Short-Term Prediction Overview
Numerical Weather Prediction Prediction model
Online data
Orography
Roughness
Wind farm layout
End user
GRID
TRADING
Image sources: DWD, WAsP, Joensen/Nielsen/Madsen EWEC’97, Pittsburgh Post-Gazette, Red Electrica de España.
DTU Wind Energy, Technical University of Denmark
Short-Term Prediction Overview
End user
Image sources: DWD, WAsP, Joensen/Nielsen/Madsen EWEC’97, Pittsburgh Post-Gazette, Red Electrica de España.
GRID
TRADING
Numerical Weather Prediction Prediction model
Online data
Orography
Roughness
Wind farm layout
DTU Wind Energy, Technical University of Denmark
End user
Image sources: DWD, WAsP, Joensen/Nielsen/Madsen EWEC’97, Red Electrica de España.
Numerical Weather Prediction Prediction model
Stakeholders
DTU Wind Energy, Technical University of Denmark
Statistical power curve estimation• Establish best connection between NWP wind speed and measured power• Often non-parametric and not a function• Often recursively adapted with new online data
DTU Wind Energy, Technical University of Denmark
Data with turbine availability and curtailment
Slide source: Waldl: Operational wind & solar power forecasting - The Perfect Wind Power Prediction. Talk on the 1st Workshop on Large-scale Grid Integration of Renewables in India, Dehli, 6-8 Sept 2017
15
20
25
30
35
40
45
50
4:30
5:30
6:30
7:30
8:30
9:30
10:30
11:30
12:30
13:30
14:30
15:30
16:30
17:30
18:30
19:30
20:30
21:30
Unconstrained wind farm production
Limited turbine
availability
Grid curtailment
Power [%]
Time [hours]
DTU Wind Energy, Technical University of Denmark
Performance
DTU Wind Energy, Technical University of DenmarkSource: Advanced Short Range Wind Energy Forecasting Technologies-- Challenges, Solutions, and ValidationKristin Larson and Tillman Gneiting, Global WINDPOWER 2004, March 31, 2004
DTU Wind Energy, Technical University of Denmark
Time and space scale of atmospheric motion
Long waves
Mid latitudes Hs & Lsfronts
TyphonesTropical Storms
days to a week or more
Land-sea breeze
Mountain-valley breeze
Thunder-storms tornadoes water-spouts
small turbulent eddies
hours to days
mins to hours
secs to mins
micro-scale
2 m
meso-scale 20 km
synoptic-scale 2000 km
global-scale 2000 km
Typical life span
Typical
sizes
Source: Jesper Nissen
DTU Wind Energy, Technical University of Denmark
Synoptic scale meteorology
(http://www.metoffice.gov.uk/weather/uk/surface_pressure.html#view)
High pressure system
Low pressure system
Cold front
Warm front
Source: Jesper Nissen
DTU Wind Energy, Technical University of Denmark
Mesoscale Meteorology
H
HL
L
SEA LAND
Sea breeze circulation
Coastal low level jets
Thunderstorm
Picture from http://www.news2.dk/pdf/20060224X008.pdf
Source: Jesper Nissen
DTU Wind Energy, Technical University of Denmark
There are always unresolved processes that cannot be represenby a numerical model.
These features are approximated through Parametrization!
Micro scales
Turbulent strees seen on the sea surface scales
1-500 m
Dust devils scale 25-50 m
Source: Jesper Nissen
DTU Wind Energy, Technical University of Denmark
NWP: DMI-HIRLAM
DTU Wind Energy, Technical University of Denmark
Level vs. Phase errors
• There are two error categories from the NWP: level errors and phase errors
– Level error means not to predict the intensity of a storm
– Phase errors are misjudging the timing of the storm
– Phase errors are more frequent these days (but how to report them?)
• Ca 80% of the error comes from the NWP!
DTU Wind Energy, Technical University of Denmark
Phase and Level errors• Errors can be phase (timing) or level errors
0
100
200
300
400
500
600
700
800
900
1000
09/0
1 00
:00
09/0
1 04
:48
09/0
1 09
:36
09/0
1 14
:24
09/0
1 19
:12
10/0
1 00
:00
10/0
1 04
:48
10/0
1 09
:36
10/0
1 14
:24
10/0
1 19
:12
11/0
1 00
:00
Time
MW
Actual Production Short Term Forecast
DTU Wind Energy, Technical University of Denmark
Common evaluation criteria
Since none were available, the ANEMOS project codified common criteria for performance measurements of short-term forecasting systems:
• Mean Error• Mean Absolute Error• Root Mean Square Error• R2 (coefficient of determination)• Histogram of errors
• Also, use separate training and validation datasets• Present the errors normalised with the installed capacity
• Madsen, H., P. Pinson, G. Kariniotakis, H.Aa. Nielsen, T.S. Nielsen: Standardizing the Performance Evaluation of Short-term Wind Power Prediction Models. Wind Engineering 29(6), pp. 475-489, 2005
http://www.ingentaconnect.com/content/mscp/wind/2005/00000029/00000006/art00002
DTU Wind Energy, Technical University of Denmark
Typical results (1996 – now more like 10%)
0 3 6 9 12 15 18 21 24 27 30 33 36-5
0
5
10
15
20
25
30
35
40
-251.5
0.0
251.5
503.0
754.5
1006.0
1257.5
1509.0
1760.5
2012.0
Peak capacity=5030 kWNøjsomhedsodde wind farm
Persistence HWP MeanRM
S Er
ror [
% o
f nam
epla
te c
apac
ity]
Forecast length [h]
RM
S Error [kW]
DTU Wind Energy, Technical University of Denmark
Typical results (1996 – now more like 10%)
0 3 6 9 12 15 18 21 24 27 30 33 36
0
5
10
15
20
25
30
35
40
0.0
251.5
503.0
754.5
1006.0
1257.5
1509.0
1760.5
2012.0
Peak capacity=5030 kWNøjsomhedsodde wind farm
Persistence HWP NewRef MeanRM
S Er
ror [
% o
f nam
epla
te c
apac
ity]
Forecast length [h]
RM
S Error [kW]
DTU Wind Energy, Technical University of Denmark
Typical results (1996 – now more like 10%)
0 3 6 9 12 15 18 21 24 27 30 33 36
0
5
10
15
20
25
30
35
40
0.0
251.5
503.0
754.5
1006.0
1257.5
1509.0
1760.5
2012.0
Peak capacity=5030 kWNøjsomhedsodde wind farm
Persistence HWP NewRef HWP / MOSRM
S Er
ror [
% o
f nam
epla
te c
apac
ity]
Forecast length [h]
RM
S Error [kW]
Typical forecast accuracy
of a modern system
DTU Wind Energy, Technical University of Denmark
Wind Speed Dependency• Wind speed errors from the NWP are quite similar across the whole range
of wind speeds• Folded through the power curve gives large errors for rising parts, small
errors for flat part
Source: M. Lange, D. Heinemann: Accuracy of Short Term Wind Power Predictions Depending on Meteorological Conditions. Proceedings of the Global Wind Power Conference, Paris 2002Central plot from Lange, M., and U. Focken: Physical Approach to Short-Term Wind Power Prediction. Berlin: Springer-Verlag, 2005
http://www.springer.com/engineering/power+engineering/book/978-3-540-25662-5
DTU Wind Energy, Technical University of Denmark
Forecast accuracy, historical (eg ISET)
• Forecasting got better during the last years
• Some of it piggybacks on improvements in meteorology
• Some is due to better interface to meteorological models (e.g., using 100m wind speed)
• Some is using multi-model approach
Graph shows error in E.Oncontrol zone over the years, with references from the paper
B. Lange et.al.: Wind Power Prediction in Germany - Recent advances and future challenges. Paper on the EWEC 2006 in Athens.
DTU Wind Energy, Technical University of Denmark
Smoothing of forecast errors
• Focken et al looked into the spatial smoothing of forecast errors – left is actual, right is derived model
• Therefore, predictions for a region always are better than predictions for a single wind farm
• Source: Lange, M., and U. Focken: Physical Approach to Short-Term Wind Power Prediction. Berlin: Springer-Verlag, 2005
http://www.springer.com/engineering/power+engineering/book/978-3-540-25662-5
DTU Wind Energy, Technical University of Denmark
History
DTU Wind Energy, Technical University of Denmark
Ed McCarthy 1985-87
• Predicted for the large wind farms in California (Altamont, San Gorgognio etc)
• Was run in the summers of 1985-87• On a HP 41CX programmable calculator
• Using meteorological observations and local upper air observations• The program was built around a climatological study of the site and
had a forecast horizon of 24 hours. • It forecast daily average wind speeds with better skill than either
persistence or climatology alone.
DTU Wind Energy, Technical University of Denmark
Prediktor
• Applied in Eastern Denmark between 1993 and 1999
• Similar: Previento
DTU Wind Energy, Technical University of Denmark
Previento
ω*
ω
Power
Prediction
Similar to Prediktor, but uses more stringent physical downscaling (incl stability) and specialised upscaling
Operational at EWE, E.On, RWE, Vattenfall, EnBWUniversity of Oldenburg / energy & meteo systems GmbH
DTU Wind Energy, Technical University of Denmark
Wind Power Prediction Tool• Developed at IMM/DTU• Operational in Western DK
1994• Operational for all of DK
1999• Statistical non-parametric
adaptive models for prediction of representative farms
• Upscaling statistically to installed capacity
• Employs data cleaning
• Similar: Sipreólico, WPMS, MORE-CARE
DTU Wind Energy, Technical University of Denmark
Fraunhofer IWES WPMS
• Wind Power Management System = Nowcasting + Forecasting
• In use at E.On Netz since 2001, RWE since 6/2003, Vattenfall Europe 2004
• E.On case: 50 representative wind farms (soon more) from WMEP -> ANN upscaling = Nowcast
• DWD Lokalmodell and others provide for forecast
• Accuracy: after 7 hours purely NWP dominated (5% RMS for E.On Netz total area)
DTU Wind Energy, Technical University of Denmark
New for WE: 100m winds
•100m wind forecasts and analysis (from ECMWF) publically available from August 2010...
•... Featured in the Weather Eye column of The Times (19th of August 2010)
Evaluation of 100m deterministic and ensemble forecastsFocus on sites with available observations (e.g. Fino)Potential benefit from getting more model-level wind forecasts
DTU Wind Energy, Technical University of Denmark
Evolution of the state of the art
1990
Deterministic approachesHybrid approaches
Probabilistic approaches1st BenchmarkingTowards standardisationCombined forecasts (multi model/NWPs)
2002 Anemos 2013
176
Next generation of toolsFocus on extremesDiversify predicted informationSpatio-tempRamp forecastingCut-off forecastingAlarming, risk indicesLink to meteorology etc
SafeWind2008
ANEMOS.plusdemos
End-users :• TSOs• DSOs• Island system
operators• Utilities• Traders
Functions considered:
Power system
scheduling
Reservesestimation
Congestion management
Wind/storage
coordination
Probabilisticforecasting
Optimal trading
38
ANEMOS./plus
Link forecasts to the applicationPower system management/tradingStochastic optimisationDemonstration
DTU Wind Energy, Technical University of Denmark
Research results
DTU Wind Energy, Technical University of Denmark
Doubling the number of NWP• Used DMI and DWD for six test cases in Denmark• Result: the combination of inputs is better
SyltholmFjaldene
MiddelgrundenKlim
Hagesholm
Tunø Knob
G. Giebel, A. Boone: A Comparison of DMI-Hirlam and DWD-Lokalmodell for Short-Term Forecasting. Poster on the EWEC, London, Nov 2004
DTU Wind Energy, Technical University of Denmark
Benefit of multiple NWPs• Combining two NWPs improves results• Alaiz data, Hirlam and MM5 (CENER) as NWP
H.Aa. Nielsen: Slides on project meeting, PSO project Intelligent Prognosis Systems, January 2006 at Risø
DTU Wind Energy, Technical University of Denmark
Spatio-temporal improvement of forecasts
Work done by DTU-IMM (now DTU-Compute) and ENFOR in the SafeWind project.
J. Tastu, P. Pinson, E. Kotwa, H.Aa. Nielsen, H. Madsen (2011). Spatio-temporal analysis and modeling of wind power forecast errors. Wind Energy 14(1), pp. 43-60
DTU Wind Energy, Technical University of Denmark
Anemos
DTU Wind Energy, Technical University of Denmark
Overview• 3 EU sponsored projects (20 M€ total, 15 M€ from EU)• Started 2002• Most important European institutes, many important end users, some
meteorological providers• Common shell for models developed… • … and installed at utilities / TSOs• Comparison of existing models• Advancing the state-of-the-art in statistical, physical and offshore
predictions
• Also commercial installations: AEMO, SONI
• Many slides in this section come from Georges Kariniotakis, Anemos project leader at Ecole des Mines / Armines.
DTU Wind Energy, Technical University of Denmark
The Consortium of Anemos
IASA
DTU Wind Energy, Technical University of Denmark
• Accuracy!• Uncertainty!
• 1990ies to 2005
Meteorology
Wind power forecasting technology
Operational decision making
Evolution
Graphics: George Kariniotakis
DTU Wind Energy, Technical University of Denmark
• Feedback to meteorology, dedicated wind powermeteorological forecasts
• 2000-
Meteorology
Wind power forecasting technology
Operational decision making
Evolution
Graphics: George Kariniotakis
DTU Wind Energy, Technical University of Denmark
Meteorology
Wind power forecasting technology
Operational decision making
• Specialised forecast products for power system issues:• Trading• Ramps / Variability• Medium-range forecasts• Congestion / Storage management• …
Evolution
Graphics: George Kariniotakis
DTU Wind Energy, Technical University of Denmark
Meteorology
Wind power forecasting technology
Operational decision making
Evolution
Graphics: George Kariniotakis
• Specialised forecast products for power system issues:• Trading• Ramps / Variability• Medium-range forecasts• Congestion / Storage management• …
DTU Wind Energy, Technical University of Denmark
Meteorology
Wind power forecasting technology
Operational decision making
Evolution
Graphics: George Kariniotakis
• Increased interaction between wind powerforecasting and meteorological community
DTU Wind Energy, Technical University of Denmark
Meteorology
Wind power forecasting technology
Operational decision making
Evolution
Graphics: George Kariniotakis
• Increased interaction between wind powerforecasting and meteorological community
DTU Wind Energy, Technical University of Denmark
The forecasting system
Generic architecture
An operational prediction platform is developed covering a wide range of end-user requirements: single wind farm forecasting up to regional/national forecasting.
DTU Wind Energy, Technical University of Denmark
Portfolio of models• Short-term (0-6 hours) statistical • Medium-term (0-48/72 hours) statistical & physical from the leading
model providers (choose some or all)• Combined approaches• Regional / National prediction • On-line uncertainty estimation • Probabilistic forecasts• Risk assessment• Numerical Weather Predictions by alternative models as input
DTU Wind Energy, Technical University of Denmark
Operational experience
Real-time operation & demonstration in 9 countries by 10 end-users.
France (utility)Germany (utility)Greece (utility)Ireland (TSO)Spain (TSO, developer)Portugal (TSO)UK (Northern Ireland TSO)
Denmark (utility)
Australia (TSO, commercial installation)
DTU Wind Energy, Technical University of Denmark
IEA Wind Task 36
DTU Wind Energy, Technical University of Denmark
IEA Wind Task 36 ForecastingInternational Energy Agency (IEA) has several Energy Technology Networks, e.g. Wind Power.Forecasting Task (36) runs 1/2016-12/2018 (and probably new phase afterthat). Some 200 people from weather services, operational forecasters, academiaand end users (TSOs, operators, traders, …).
Participation is open for IEA Wind member countries, but news aredistributed via a mailing list (send mail to [email protected]).
See details at www.ieawindforecasting.dk.
266 18 September
2017
mailto:[email protected]
DTU Wind Energy, Technical University of Denmark
Technical Results
Mainly: published 5 lists, useful for peers• Tall masts for NWP verification, and how to
access their data• Field experiments in wind power meteorology• Openly available benchmarks for power
forecasts• Research projects in the field• Future research issues
DTU Wind Energy, Technical University of Denmark
Use of probabilistic forecastingOpen Access journal paper48 pages on the use of uncertaintyforecasts in the power industry
Definition – Methods –Communication of Uncertainty – End User Cases – Pitfalls -Recommendations
Source: http://www.mdpi.com/1996-1073/10/9/1402/
272 18 September
2017
http://www.mdpi.com/1996-1073/10/9/1402/
DTU Wind Energy, Technical University of Denmark
Best Practice
DTU Wind Energy, Technical University of Denmark
Best Practice
• Get a model (24/7)• Get another model (NWP and / or short-term forecasting model)• Use online power data for first hours and power curve calibration• Work together with service provider / academia / weather
service to continuously improve model accuracy• Reduce error by predicting for a larger area (smoothing)• Balance all errors together, not just wind• Use the uncertainty / pdf
• Do forecasting on TSO level, not necessarily on wind farm / developer level
• Use intraday trading
• Use longer forecasts for maintenance planning• Meteorological training for the operators• Meteorological hotline for special cases
• Also in report on powwow.risoe.dk (Giebel and Kariniotakis: Best Practice in Short-term Forecasting. A User’s Guide. Project report for the POW’WOW project, 6 pages, 2009)
http://powwow.risoe.dk/publ/GGiebelGKariniotakis-STPBestPractice_POW'WOW.pdf
The State of the Art in Short-term Prediction of Wind PowerOutlineState-of-the-Art for Wind PowerState-of-the-Art in Short-term PredictionState-of-the-Art in Short-term PredictionSlide Number 54Record in DK: 140% wind power!SmoothingAll Europe is connectedData from 60 meteorological stationsCross-correlation versus distanceUsersUsers of forecastsThomas Ackermann about TSOsLevel of users 2016Timescales for wind forecastsCost functionsStrategic bidding vs TSO responsibilityPredictions�HowToShort-Term Prediction OverviewShort-Term Prediction OverviewStakeholdersStatistical power curve estimationData with turbine availability and curtailmentPerformanceSlide Number 110Slide Number 111Synoptic scale meteorologyMesoscale MeteorologySlide Number 114NWP: DMI-HIRLAMLevel vs. Phase errorsPhase and Level errorsCommon evaluation criteriaTypical results (1996 – now more like 10%)Typical results (1996 – now more like 10%)Typical results (1996 – now more like 10%)Wind Speed DependencyForecast accuracy, historical (eg ISET)Smoothing of forecast errorsHistoryEd McCarthy 1985-87Prediktor PrevientoWind Power Prediction ToolFraunhofer IWES WPMSNew for WE: 100m windsEvolution of the state of the artResearch resultsDoubling the number of NWPBenefit of multiple NWPsSpatio-temporal improvement of forecastsAnemosOverviewThe Consortium of AnemosEvolutionEvolutionEvolutionEvolutionEvolutionEvolutionSlide Number 258Portfolio of modelsSlide Number 264IEA Wind Task 36IEA Wind Task 36 ForecastingSlide Number 270Use of probabilistic forecastingBest PracticeBest Practice