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The State of the Art in Short-term Prediction of Wind Power Dr. Gregor Giebel DTU Wind Energy And numerous co-authors, not all knowingly… SANEDI, Sandton, South Africa, 19 Sept 2017

The State of the Art in Short-term Prediction of Wind Power...DTU Wind Energy, Technical University of Denmark. Time and space scale of atmospheric motion. Long waves. Mid latitudes

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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

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  • 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