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Probabilistic Forecasts of Wind and Solar Power Generation Henrik Madsen 1 , Henrik Aalborg Nielsen 2 , Peder Bacher 1 , Pierre Pinson 1 , Torben Skov Nielsen 2 [email protected] (1) Tech. Univ. of Denmark (DTU) DK-2800 Lyngby www.imm.dtu.dk/ ˜ hm (2) ENFOR A/S Lyngsø All´ e3 DK-2970 Hørsholm www.enfor.dk Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 1

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Page 1: Probabilistic Forecasts of Wind and Solar Power Generationproyectotres.itccanarias.org/phocadownload/iib... · The methods have been used operationally for predicting wind power in

Probabilistic Forecasts ofWind and Solar Power GenerationHenrik Madsen1, Henrik Aalborg Nielsen2, Peder Bacher1,

Pierre Pinson1, Torben Skov Nielsen2

[email protected]

(1) Tech. Univ. of Denmark (DTU)

DK-2800 Lyngby

www.imm.dtu.dk/ ˜ hm

(2) ENFOR A/S

Lyngsø Alle 3

DK-2970 Hørsholm

www.enfor.dk

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 1

Page 2: Probabilistic Forecasts of Wind and Solar Power Generationproyectotres.itccanarias.org/phocadownload/iib... · The methods have been used operationally for predicting wind power in

Outline

Wind power forecasting

Configuration example

Use of several providers of MET forecasts

Uncertainty and confidence intervals

Scenario forecasting

Examples on the use of probabilistic forecasts

Value of probabilistic forecasts

Solar power forecasting

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 2

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Wind Power Forecasting - History

Our methods for probabilistic wind power forecasting have been implemented in theAnemos Wind Power Prediction SystemandWPPT

The methods have been continuously developed since 1993 - incollaboration withEnerginet.dk,Dong Energy,Vattenfall,Risø – DTU,The ANEMOS projects partners/consortium (since 2002),ENFOR (Denmark)

The methods have been used operationally for predicting wind power in Denmarksince 1996.

Anemos/WPPT is now used all over Europe, Australia, and North America.

Now in Denmark: Wind power coverson averageabout 27 pct of the system load.

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 3

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Prediction Performance

A typical performance measure. 13 large parks. Installed power: 1064 MW. Period: August2008 - March 2010. MET input is in all cases ECMWF. Criterion used: RMSE (notice:Power Curve model only)

Forecast horizon (hours)

Nor

mal

ized

pow

er

0.00

0.05

0.10

0.15

0 12 24 36 48

Nominal power: 1064 MW

RMSE

WPPT−PCSimple modelCommercial model 1Commercial model 2

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 4

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Uncertainty and adaptivity

Errors in MET forecasts will end up in errors in wind power forecasts, but other factors leadto a need for adaptation which however leads to some uncertainties.

The total system consisting of wind farms measured online, wind turbines not measuredonline and meteorological forecasts will inevitably change over time as:

the population of wind turbines changes,

changes in unmodelled or insufficiently modelled characteristics (importantexamples: roughness and dirty blades),

changes in the NWP models.

A wind power prediction system must be able to handle these time-variations in model andsystem. An adequate forecasting system may useadaptive and recursive model estimationto handle these issues.

We started (some 20 years ago) assuming Gaussianity; but this is a very serious (wrong)assumption !

Following the initial installation the software tool will automatically calibrate the models tothe actual situation.

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 5

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The power curve model

The wind turbine “power curve” model,ptur = f(wtur) is extended to a wind farmmodel, pwf = f(wwf , θwf ), by introducingwind direction dependency. By introducing arepresentative area wind speed and direction itcan be further extended to cover all turbines inan entire region,par = f(war, θar).

The power curve model is defined as:

pt+k|t = f( wt+k|t, θt+k|t, k )

wherewt+k|t is forecasted wind speed, andθt+k|t is forecasted wind direction.

The characteristics of the NWP change withthe prediction horizon.

k

Wind speedWind direction

P

k

Wind speedWind direction

P

k

Wind speedWind direction

P

k

Wind speedWind direction

P

HO - Estimated power curve

Plots of the estimated power curve forthe Hollandsbjerg wind farm.

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 6

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Configuration Example

This configuration of Anemos PredictionSystem/WPPT is used by a large TSO.Characteristics for the installation:

A large number of wind farms andstand-alone wind turbines.

Frequent changes in the windturbine population.

Offline production data with aresolution of 15 min. is availablefor more than 99% of the windturbines in the area.

Online data for a large numberof wind farms are available. Thenumber of online wind farms in-creases quite frequently.

ModelUpscaling

predictionTotal prod.

Dynamic

Power CurveModel

Model

Offline prod.data

predictionArea prod.

NWP data

Online prod.data

predictionOnline prod.

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 7

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Spatio-temporal forecasting

Predictive improvement (measured inRMSE) of forecasts errors by adding thespatio-temperal module in WPPT.

23 months (2006-2007)

15 onshore groups

Focus here on 1-hour forecast only

Larger improvements for eastern partof the region

Needed for reliable ramp forecasting.

The EU project NORSEWinD willextend the region

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 8

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Combined forecasting

A number of power forecasts areweighted together to form a newimproved power forecast.

These could come from parallelconfigurations of WPPT using NWPinputs fromdifferent METproviders or they could come fromother power prediction providers.

In addition to the improved perfor-mance also the robustness of the sys-tem is increased.

Met Office

DWD

DMI

WPPT

WPPT

WPPT

Comb Final

The example show results achieved for theTunø Knob wind farms using combinationsof up to 3 power forecasts.

Hours since 00Z

RM

S (

MW

)

5 10 15 20

5500

6000

6500

7000

7500

hir02.locmm5.24.loc

C.allC.hir02.loc.AND.mm5.24.loc

Typically an improvement on 10-15 pctin accuracy of the point prediction isseen by including more than one METprovider. Two or more MET providersimply information about uncertainty

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 9

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Uncertainty estimation

In many applications it is crucial that a pre-diction tool delivers reliable estimates (prob-abilistc forecasts) of the expected uncertaintyof the wind power prediction.

We consider the following methods for esti-mating the uncertainty of the forecasted windpower production:

Ensemble based - but corrected -quantiles.

Quantile regression.

Stochastic differential equations.

The plots show raw (top) and corrected (bot-tom) uncertainty intervales based on ECMEFensembles for Tunø Knob (offshore park),29/6, 8/10, 10/10 (2003). Shown are the25%, 50%, 75%, quantiles.

Tunø Knob: Nord Pool horizons (init. 29/06/2003 12:00 (GMT), first 12h not in plan)

kW

12:00 18:00 0:00 6:00 12:00 18:00 0:00Jun 30 2003 Jul 1 2003 Jul 2 2003

020

0040

00

Tunø Knob: Nord Pool horizons (init. 08/10/2003 12:00 (GMT), first 12h not in plan)

kW

12:00 18:00 0:00 6:00 12:00 18:00 0:00Oct 9 2003 Oct 10 2003 Oct 11 2003

020

0040

00

Tunø Knob: Nord Pool horizons (init. 10/10/2003 12:00 (GMT), first 12h not in plan)

kW

12:00 18:00 0:00 6:00 12:00 18:00 0:00Oct 11 2003 Oct 12 2003 Oct 13 2003

020

0040

00

Tunø Knob: Nord Pool horizons (init. 29/06/2003 12:00 (GMT), first 12h not in plan)

kW

12:00 18:00 0:00 6:00 12:00 18:00 0:00Jun 30 2003 Jul 1 2003 Jul 2 2003

020

0040

00

Tunø Knob: Nord Pool horizons (init. 08/10/2003 12:00 (GMT), first 12h not in plan)

kW

12:00 18:00 0:00 6:00 12:00 18:00 0:00Oct 9 2003 Oct 10 2003 Oct 11 2003

020

0040

00

Tunø Knob: Nord Pool horizons (init. 10/10/2003 12:00 (GMT), first 12h not in plan)

kW

12:00 18:00 0:00 6:00 12:00 18:00 0:00Oct 11 2003 Oct 12 2003 Oct 13 2003

020

0040

00

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 10

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Quantile regression

A (additive) model for each quantile:

Q(τ) = α(τ) + f1(x1; τ) + f2(x2; τ) + . . .+ fp(xp; τ)

Q(τ) Quantile offorecast error from anexisting system.

xj Variables which influence the quantiles, e.g. the wind direction.

α(τ) Intercept to be estimated from data.

fj(·; τ) Functions to be estimated from data.

Notes on quantile regression:

Parameter estimates found by minimizing a dedicated function of the

prediction errors.

The variation of the uncertainty is (partly) explained by the independent

variables.Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 11

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Quantile regression - An example

Effect of variables (- the functions are approximated by Spline basis

functions):

0 1000 3000 5000

−20

000

1000

2000

pow.fc

25%

(bl

ue)

and

75%

(re

d) q

uant

iles

20 25 30 35

−20

000

1000

2000

horizon

25%

(bl

ue)

and

75%

(re

d) q

uant

iles

0 50 150 250 350

−20

000

1000

2000

wd10m

25%

(bl

ue)

and

75%

(re

d) q

uant

iles

Forecasted power has a large influence.

The effect of horizon is of less importance.

Some increased uncertainty for Westerly winds.

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 12

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Example: Probabilistic forecasts

5 10 15 20 25 30 35 40 450

10

20

30

40

50

60

70

80

90

100

look−ahead time [hours]

pow

er [%

of P

n]

90%80%70%60%50%40%30%20%10%pred.meas.

Notice how the confidence intervals varies ...

But the correlation in forecasts errors is not described so far.

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 13

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Correlation structure of forecast errors

It is important to model theinterdependence structureof the prediction errors.

An example of interdependence covariance matrix:

5 10 15 20 25 30 35 40

5

10

15

20

25

30

35

40

horizon [h]

horiz

on[h

]

−0.2

0

0.2

0.4

0.6

0.8

1

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 14

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Correct (top) and naive (bottom) scenarios%

of in

stalle

d ca

pacit

y

0 24 48 72 96 120 144

020

4060

8010

0

hours

100% 90% 80% 70% 60% 50% 40% 30% 20% 10%100% 90% 80% 70% 60% 50% 40% 30% 20% 10%

% o

f insta

lled

capa

city

0 24 48 72 96 120 144

020

4060

8010

0

hours

100% 90% 80% 70% 60% 50% 40% 30% 20% 10%100% 90% 80% 70% 60% 50% 40% 30% 20% 10%

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 15

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Use of Stoch. Diff. Equations

The state equation describes the future wind power production

dxt =− θ(ut) · (xt − pt|0)dt+

2√

θ(ut)α(ut)pt|0(1− pt|0)xt · (1− xt)dwt,

with α(ut) ∈ (0, 1), and the observation equation

yh =xth|0 + eh,

whereh ∈ {1, 2, ..., 48}, th = k, eh ∼ N(0, s2), x0 = “observed power at t=0”, and

pt|0 point forecast byWPPT (Wind Power Prediction Tool)

ut input vector (heret andpt|0)

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 16

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Examples of using SDEs

Time

Pow

er

0.0

0.2

0.4

0.6

0.8

1.0

0 12 24 36 48

April 22. 2001, 12h May 19. 2001, 12h

May 5. 2003, 18h

0 12 24 36 48

0.0

0.2

0.4

0.6

0.8

1.0October 22. 2002, 00h

0.0

0.2

0.4

0.6

0.8

1.0

Obs. pt|0 pSDE

Use of SDEs provides a possibility for a joint description ofboth non-symmetricalconditional densities as well as the interdependence of theforecasts.

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 17

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SDE approach – Correlation structures

Time

Tim

e

12

24

36

48

12 24 36 48

April 22. 2001, 12h May 19. 2001, 12h

May 5. 2003, 18h

12 24 36 48

12

24

36

48October 22. 2002, 00h

0.0

0.2

0.4

0.6

0.8

1.0

Use of SDEs provides a possibility to model eg. time varying and wind power dependentcorrelation structures.SDEs provide a perfect framework forcombined wind and solar power forecasting.Today both theAnemos Prediction PlatformandWPPT provide operations forecasts ofboth wind and solar power production.

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 18

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Type of forecasts required

Point forecasts (normal forecasts); a single value for each time point in the future.Sometimes with simple error bands.

Probabilistic or quantile forecasts; the full conditional distribution for each timepoint in the future.

Scenarios; probabilistic correct scenarios of the future wind power production.

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 19

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Value of knowing the uncertainties

Case study: A 15 MW wind farm in the Dutch electricity market,prices andmeasurements from the entire year 2002.

From a phd thesis by Pierre Pinson (2006).

The costs are due to the imbalance penalties on the regulation market.

Value of an advanced method for point forecasting:The regulation costs arediminished by nearly 38 pct.compared to the costs of using the persistanceforecasts.

Added value of reliable uncertainties:A further decrease of regulation costs – up to39 pct.

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 20

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Stochastic Portfolio Optimization

Example on the use of quantiles for optimization (From Emil Sokoler)

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 21

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Wind power – asymmetrical penalties

The revenue from trading a specific hour on NordPool can be expressed as

PS × Bid +

{

PD × (Actual− Bid) if Actual > BidPU × (Actual− Bid) if Actual < Bid

PS is the spot price andPD/PU is the down/up reg. price.

The bid maximising the expected revenue is the followingquantile

E[PS ]− E[PD]

E[PU ]− E[PD]

in the conditional distribution of the future wind power production.

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 22

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Wind power – asymmetrical penalties

It is difficult to know the regulation prices at the day ahead level – research intoforecasting is ongoing.

The expression for the quantile is concerned with expected values of the prices – justgetting these somewhat right will increase the revenue.

A simple tracking ofCD andCU is a starting point.

The bids maximizing the revenue during the period September 2009 to March2010:

Qua

ntile

0.0

0.4

0.8

2009−09−01 2009−11−01 2010−01−01 2010−03−01

Monthly averages Operational tracking

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 23

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Balancing wind by varying other production

Correct

Storage (hours of full wind prod.)

Den

sity

−10 −5 0 5 10

0.00

0.10

0.20

0.30

Naive

Storage (hours of full wind prod.)

Den

sity

−10 −5 0 5 10

0.00

0.10

0.20

0.30

(Illustrative example based on 50 day ahead scenarios as in the situation considered before)

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 24

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Use of scenarios - Examples

Ramp forecasting; probabilities oframp events

Calculation of required storage asa function of horison (possibly ob-tained by varying hydro power pro-duction). Also show is the proba-bility that this storage will be suffi-cient.

Pro

babi

lity

of 1

0%, 2

h up

−re

gula

tion

even

t (%

)

h0 5 10 15 20 25 30 35

010

2030

0 5 10 15 20 25 30 35

−10

−5

05

Ene

rgy

stor

ed (

h of

full

prod

uctio

n)

100% 99%

98% 95%

90% 80%

70% 60%

50% 40%

30% 20%

10%100% 99%

98% 95%

90% 80%

70% 60%

50% 40%

30% 20%

10%

h

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 25

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Solar Power Forecasting

Same principles as for wind power ....

Developed for grid connected PV-systems mainly installed on rooftops

Average of output from 21 PV systems in small village (Brædstrup) in DK

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 26

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Method

Based on readings from the systems and weather forecasts

Two-step method

Step One: Transformation to atmospheric transmittanceτ with statistical clear skymodel (see below). Step Two: A dynamic model (see paper).

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 27

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Example of hourly forecasts

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 28

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Conclusions

The forecasting models must beadaptive (in order to taken changes of dust onblades, changes roughness, etc., into account).

Reliable estimates of theforecast accuracyis very important (check the reliability byeg. reliability diagrams).

Reliable probabilistic forecasts are important to gain thefull economical value.

Usemore than a single MET provider for delivering the input to the prediction tool– this improves the accuracy of wind power forecasts with 10-15 pct.

Estimates of thecorrelation in forecasts errors important.

Forecasts of ’cross dependencies’ between load, prices, wind and solar power areimportant.

Probabilistic forecasts are very important for asymmetric cost functions.

Probabilistic forecasts can provideanswersfor questions likeWhat is the probability that this storage is large enough forthe next 5 hours?What is the probability of an increase in wind power production of more that 50pct over the next two hours?What is the probability of a down-regulation due to wind power on more than xGW within the next 4 hours.

The same conclusions hold for our tools foreg. solar power forecasting.Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 29

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Some references

H. Madsen:Time Series Analysis, Chapman and Hall, 392 pp, 2008.

H. Madsen and P. Thyregod:Introduction to General and Generalized Linear Models, Chapman

and Hall, 320 pp., 2011.

P. Pinson and H. Madsen:Forecasting Wind Power Generation: From Statistical Framework to

Practical Aspects. New book in progress - will be available 2012.

T.S. Nielsen, A. Joensen, H. Madsen, L. Landberg, G. Giebel:A New Reference for Predicting

Wind Power, Wind Energy, Vol. 1, pp. 29-34, 1999.

H.Aa. Nielsen, H. Madsen:A generalization of some classical time series tools, Computational

Statistics and Data Analysis, Vol. 37, pp. 13-31, 2001.

H. Madsen, P. Pinson, G. Kariniotakis, H.Aa. Nielsen, T.S. Nilsen: Standardizing the performance

evaluation of short-term wind prediction models, Wind Engineering, Vol. 29, pp. 475-489, 2005.

H.A. Nielsen, T.S. Nielsen, H. Madsen, S.I. Pindado, M. Jesus, M. Ignacio:Optimal Combination

of Wind Power Forecasts, Wind Energy, Vol. 10, pp. 471-482, 2007.

A. Costa, A. Crespo, J. Navarro, G. Lizcano, H. Madsen, F. Feitosa,A review on the young history

of the wind power short-term prediction, Renew. Sustain. Energy Rev., Vol. 12, pp. 1725-1744,

2008.

J.K. Møller, H. Madsen, H.Aa. Nielsen:Time Adaptive Quantile Regression, Computational

Statistics and Data Analysis, Vol. 52, pp. 1292-1303, 2008.

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 30

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Some references (Cont.)

P. Bacher, H. Madsen, H.Aa. Nielsen:Online Short-term Solar Power Forecasting, Solar Energy,

Vol. 83(10), pp. 1772-1783, 2009.

P. Pinson, H. Madsen:Ensemble-based probabilistic forecasting at Horns Rev. Wind Energy, Vol.

12(2), pp. 137-155 (special issue on Offshore Wind Energy),2009.

P. Pinson, H. Madsen:Adaptive modeling and forecasting of wind power fluctuations with

Markov-switching autoregressive models. Journal of Forecasting, 2010.

C.L. Vincent, G. Giebel, P. Pinson, H. Madsen:Resolving non-stationary spectral signals in wind

speed time-series using the Hilbert-Huang transform. Journal of Applied Meteorology and

Climatology, Vol. 49(2), pp. 253-267, 2010.

P. Pinson, P. McSharry, H. Madsen.Reliability diagrams for nonparametric density forecastsof

continuous variables: accounting for serial correlation. Quarterly Journal of the Royal

Meteorological Society, Vol. 136(646), pp. 77-90, 2010.

G. Reikard, P. Pinson, J. Bidlot (2011).Forecasting ocean waves - A comparison of ECMWF wave

model with time-series methods. Ocean Engineering in press.

C. Gallego, P. Pinson, H. Madsen, A. Costa, A. Cuerva (2011).Influence of local wind speed and

direction on wind power dynamics - Application to offshore very short-term forecasting. Applied

Energy, in press

Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 – p. 31

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