Probabilistic Forecasts of Wind and Solar Power Generation



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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 hm@imm.dtu.dk (1) Tech. Univ. of Denmark (DTU) DK-2800 Lyngby www.imm.dtu.dk/ hm (2) ENFOR A/S Lyngsø Allé 3 DK-2970 Hørsholm www.enfor.dk Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 1

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

Wind Power Forecasting - History Our methods for probabilistic wind power forecasting have been implemented in the Anemos Wind Power Prediction System and WPPT The methods have been continuously developed since 1993 - in collaboration with Energinet.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 Denmark since 1996. Anemos/WPPT is now used all over Europe, Australia, and North America. Now in Denmark: Wind power covers on average about 27 pct of the system load. Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 3

Prediction Performance A typical performance measure. 13 large parks. Installed power: 1064 MW. Period: August 2008 - March 2010. MET input is in all cases ECMWF. Criterion used: RMSE (notice: Power Curve model only) WPPT PC Simple model Commercial model 1 Commercial model 2 0.15 Nominal power: 1064 MW RMSE Normalized power 0.10 0.05 0.00 0 12 24 36 48 Forecast horizon (hours) Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 4

Uncertainty and adaptivity Errors in MET forecasts will end up in errors in wind power forecasts, but other factors lead to a need for adaptation which however leads to some uncertainties. The total system consisting of wind farms measured online, wind turbines not measured online and meteorological forecasts will inevitably change over time as: the population of wind turbines changes, changes in unmodelled or insufficiently modelled characteristics (important examples: roughness and dirty blades), changes in the NWP models. A wind power prediction system must be able to handle these time-variations in model and system. An adequate forecasting system may use adaptive and recursive model estimation to 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 to the actual situation. Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 5

The power curve model The wind turbine power curve model, p tur = f(w tur ) is extended to a wind farm model, p wf = f(w wf,θ wf ), by introducing wind direction dependency. By introducing a representative area wind speed and direction it can be further extended to cover all turbines in an entire region, p ar = f( w ar, θ ar ). P HO - Estimated power curve k k P The power curve model is defined as: Wind direction k Wind speed Wind direction k Wind speed ˆp t+k t = f( w t+k t, θ t+k t, k ) P P where w t+k t is forecasted wind speed, and θ t+k t is forecasted wind direction. Wind direction Wind speed Wind direction Wind speed The characteristics of the NWP change with the prediction horizon. Plots of the estimated power curve for the Hollandsbjerg wind farm. Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 6

Configuration Example This configuration of Anemos Prediction System/WPPT is used by a large TSO. Characteristics for the installation: A large number of wind farms and stand-alone wind turbines. Frequent changes in the wind turbine population. Offline production data with a resolution of 15 min. is available for more than 99% of the wind turbines in the area. Online data for a large number of wind farms are available. The number of online wind farms increases quite frequently. Offline prod. data Online prod. data NWP data Power Curve Model Dynamic Model Upscaling Model Area prod. prediction Total prod. prediction Online prod. prediction Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 7

Spatio-temporal forecasting Predictive improvement (measured in RMSE) of forecasts errors by adding the spatio-temperal module in WPPT. 23 months (2006-2007) 15 onshore groups Focus here on 1-hour forecast only Larger improvements for eastern part of the region Needed for reliable ramp forecasting. The EU project NORSEWinD will extend the region Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 8

Combined forecasting DMI DWD Met Office A number of power forecasts are weighted together to form a new improved power forecast. These could come from parallel configurations of WPPT using NWP inputs from different MET providers or they could come from other power prediction providers. In addition to the improved performance also the robustness of the system is increased. WPPT WPPT WPPT Comb Final The example show results achieved for the Tunø Knob wind farms using combinations of up to 3 power forecasts. RMS (MW) 5500 6000 6500 7000 7500 hir02.loc mm5.24.loc 5 10 15 20 Hours since 00Z C.all C.hir02.loc.AND.mm5.24.loc Typically an improvement on 10-15 pct in accuracy of the point prediction is seen by including more than one MET provider. Two or more MET providers imply information about uncertainty Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 9

Uncertainty estimation In many applications it is crucial that a prediction tool delivers reliable estimates (probabilistc forecasts) of the expected uncertainty of the wind power prediction. We consider the following methods for estimating the uncertainty of the forecasted wind power production: Ensemble based - but corrected - quantiles. Quantile regression. Stochastic differential equations. The plots show raw (top) and corrected (bottom) uncertainty intervales based on ECMEF ensembles for Tunø Knob (offshore park), 29/6, 8/10, 10/10 (2003). Shown are the 25%, 50%, 75%, quantiles. kw kw kw kw kw kw 0 2000 4000 0 2000 4000 0 2000 4000 0 2000 4000 0 2000 4000 0 2000 4000 Tunø Knob: Nord Pool horizons (init. 29/06/2003 12:00 (GMT), first 12h not in plan) 12:00 18:00 0:00 6:00 12:00 18:00 0:00 Jun 30 2003 Jul 1 2003 Jul 2 2003 Tunø Knob: Nord Pool horizons (init. 08/10/2003 12:00 (GMT), first 12h not in plan) 12:00 18:00 0:00 6:00 12:00 18:00 0:00 Oct 9 2003 Oct 10 2003 Oct 11 2003 Tunø Knob: Nord Pool horizons (init. 10/10/2003 12:00 (GMT), first 12h not in plan) 12:00 18:00 0:00 6:00 12:00 18:00 0:00 Oct 11 2003 Oct 12 2003 Oct 13 2003 Tunø Knob: Nord Pool horizons (init. 29/06/2003 12:00 (GMT), first 12h not in plan) 12:00 18:00 0:00 6:00 12:00 18:00 0:00 Jun 30 2003 Jul 1 2003 Jul 2 2003 Tunø Knob: Nord Pool horizons (init. 08/10/2003 12:00 (GMT), first 12h not in plan) 12:00 18:00 0:00 6:00 12:00 18:00 0:00 Oct 9 2003 Oct 10 2003 Oct 11 2003 Tunø Knob: Nord Pool horizons (init. 10/10/2003 12:00 (GMT), first 12h not in plan) 12:00 18:00 0:00 6:00 12:00 18:00 0:00 Oct 11 2003 Oct 12 2003 Oct 13 2003 Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 10

Quantile regression A (additive) model for each quantile: Q(τ) = α(τ)+f 1 (x 1 ;τ)+f 2 (x 2 ;τ)+...+f p (x p ;τ) Q(τ) x j α(τ) Quantile of forecast error from an existing system. Variables which influence the quantiles, e.g. the wind direction. Intercept to be estimated from data. f j ( ;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

Quantile regression - An example Effect of variables (- the functions are approximated by Spline basis functions): 25% (blue) and 75% (red) quantiles 2000 0 1000 2000 25% (blue) and 75% (red) quantiles 2000 0 1000 2000 25% (blue) and 75% (red) quantiles 2000 0 1000 2000 0 1000 3000 5000 pow.fc 20 25 30 35 horizon 0 50 150 250 350 wd10m 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

Example: Probabilistic forecasts 100 90 power [% of Pn] 80 70 60 50 40 30 20 10 90% 80% 70% 60% 50% 40% 30% 20% 10% pred. meas. 0 5 10 15 20 25 30 35 40 45 look ahead time [hours] 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

Correlation structure of forecast errors It is important to model the interdependence structure of the prediction errors. An example of interdependence covariance matrix: horizon[h] 40 35 30 25 20 15 1 0.8 0.6 0.4 0.2 10 5 5 10 15 20 25 30 35 40 horizon [h] 0 0.2 Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 14

Correct (top) and naive (bottom) scenarios % of installed capacity 0 20 40 60 80 100 100% 90% 80% 70% 60% 50% 40% 30% 20% 10% 0 24 48 72 96 120 144 hours % of installed capacity 0 20 40 60 80 100 100% 90% 80% 70% 60% 50% 40% 30% 20% 10% 0 24 48 72 96 120 144 hours Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 15

Use of Stoch. Diff. Equations The state equation describes the future wind power production dx t = θ(u t ) (x t ˆp t 0 )dt+ 2 θ(u t )α(u t )ˆp t 0 (1 ˆp t 0 )x t (1 x t )dw t, with α(u t ) (0,1), and the observation equation y h =x th 0 +e h, where h {1,2,...,48}, t h = k, e h N(0,s 2 ), x 0 = observed power at t=0, and ˆp t 0 point forecast by WPPT (Wind Power Prediction Tool) u t input vector (here t and ˆp t 0 ) Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 16

Examples of using SDEs Obs. p^t 0 p^sde 0 12 24 36 48 May 5. 2003, 18h October 22. 2002, 00h 1.0 1.0 0.8 0.6 0.8 0.4 0.2 0.6 Power 1.0 0.8 April 22. 2001, 12h May 19. 2001, 12h 0.0 0.4 0.6 0.4 0.2 0.2 0.0 0 12 24 36 48 Time 0.0 Use of SDEs provides a possibility for a joint description of both non-symmetrical conditional densities as well as the interdependence of the forecasts. Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 17

SDE approach Correlation structures 12 24 36 48 1.0 May 5. 2003, 18h October 22. 2002, 00h 48 36 0.8 24 12 0.6 Time 48 April 22. 2001, 12h May 19. 2001, 12h 0.4 36 24 0.2 12 12 24 36 48 0.0 Time Use of SDEs provides a possibility to model eg. time varying and wind power dependent correlation structures. SDEs provide a perfect framework for combined wind and solar power forecasting. Today both the Anemos Prediction Platform and WPPT provide operations forecasts of both wind and solar power production. Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 18

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 time point 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

Value of knowing the uncertainties Case study: A 15 MW wind farm in the Dutch electricity market, prices and measurements 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 are diminished by nearly 38 pct. compared to the costs of using the persistance forecasts. Added value of reliable uncertainties: A further decrease of regulation costs up to 39 pct. Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 20

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

Wind power asymmetrical penalties The revenue from trading a specific hour on NordPool can be expressed as P S Bid+ { P D (Actual Bid) if P U (Actual Bid) if P S is the spot price and P D /P U is the down/up reg. price. Actual > Bid Actual < Bid The bid maximising the expected revenue is the following quantile E[P S ] E[P D ] E[P U ] E[P D ] in the conditional distribution of the future wind power production. Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 22

Wind power asymmetrical penalties It is difficult to know the regulation prices at the day ahead level research into forecasting is ongoing. The expression for the quantile is concerned with expected values of the prices just getting these somewhat right will increase the revenue. A simple tracking of C D and C U is a starting point. The bids maximizing the revenue during the period September 2009 to March 2010: Quantile 0.0 0.4 0.8 Monthly averages Operational tracking 2009 09 01 2009 11 01 2010 01 01 2010 03 01 Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 23

Balancing wind by varying other production Correct Naive Density 0.00 0.10 0.20 0.30 Density 0.00 0.10 0.20 0.30 10 5 0 5 10 10 5 0 5 10 Storage (hours of full wind prod.) Storage (hours of full wind prod.) (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

Use of scenarios - Examples Ramp forecasting; probabilities of ramp events Calculation of required storage as a function of horison (possibly obtained by varying hydro power production). Also show is the probability that this storage will be sufficient. Probability of 10%, 2h up regulation event (%) Energy stored (h of full production) 0 10 20 30 10 5 0 5 0 5 10 15 20 25 30 35 100% 99% 98% 95% 90% 80% 70% 60% 50% 40% 30% 20% 10% h 0 5 10 15 20 25 30 35 h Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 25

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

Method Based on readings from the systems and weather forecasts Two-step method Step One: Transformation to atmospheric transmittance τ with statistical clear sky model (see below). Step Two: A dynamic model (see paper). Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 27

Example of hourly forecasts Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 28

Conclusions The forecasting models must be adaptive (in order to taken changes of dust on blades, changes roughness, etc., into account). Reliable estimates of the forecast accuracy is very important (check the reliability by eg. reliability diagrams). Reliable probabilistic forecasts are important to gain the full economical value. Use more 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 the correlation in forecasts errors important. Forecasts of cross dependencies between load, prices, wind and solar power are important. Probabilistic forecasts are very important for asymmetric cost functions. Probabilistic forecasts can provide answers for questions like What is the probability that this storage is large enough for the next 5 hours? What is the probability of an increase in wind power production of more that 50 pct over the next two hours? What is the probability of a down-regulation due to wind power on more than x GW within the next 4 hours. The same conclusions hold for our tools for eg. solar power forecasting. Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 29

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

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 forecasts of 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

Some references (Cont.) C.L. Vincent, P. Pinson, G. Giebel (2011). Wind fluctuations over the North Sea. International Journal of Climatology, available online 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 F. Thordarson, H.Aa. Nielsen, H. Madsen, P. Pinson (2010). Conditional weighted combination of wind power forecasts. Wind Energy 13(8), pp. 751-763 P. Pinson, G. Kariniotakis (2010). Conditional prediction intervals of wind power generation. IEEE Transactions on Power Systems 25(4), pp. 1845-1856 P. Pinson, H.Aa. Nielsen, H. Madsen, G. Kariniotakis (2009). Skill forecasting from ensemble predictions of wind power. Applied Energy 86(7-8), pp. 1326-1334. P. Pinson, H.Aa. Nielsen, J.K. Moeller, H. Madsen, G. Kariniotakis (2007). Nonparametric probabilistic forecasts of wind power: required properties and evaluation. Wind Energy 10(6), pp. 497-516. T. Jónsson, P. Pinson (2010). On the market impact of wind energy forecasts. Energy Economics, Vol. 32(2), pp. 313-320. T. Jónsson, M. Zugno, H. Madsen, P. Pinson (2010). On the Market Impact of Wind Power (Forecasts) - An Overview of the Effects of Large-scale Integration of Wind Power on the Electricity Market. IAEE International Conference, Rio de Janeiro, Brazil. Seminario International de Clausura del Proyecto TRES, Las Palmas 2012 p. 32