Lara-Fanego DNI Solar Forecasts WRF Spain for CPV applications-CPV8

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    CPV-8Conf.,Toledo,Spain(2012)

    Evaluation Of DNI Forecast Based On The WRFMesoscale Atmospheric Model For CPV Applications

    V. Lara-Fanego1, J. A. Ruiz-Arias

    1, A. D. Pozo-Vzquez

    1,

    C. A. Gueymard2 and J. Tovar-Pescador1

    1Department of Physics, University of Jan. Campus Las Lagunillas A3-066, 23071, Jan (Spain)

    2Solar Consulting Services, P.O. Box 392, Colebrook, NH 03576, USA

    [email protected]

    Abstract. The integration of large-scale solar electricity production into the energy supply structures depends es-sentially on the precise advance knowledge of the available resource. Numerical weather prediction (NWP) modelsprovide a reliable and comprehensive tool for short- and medium-range solar radiation forecasts. The methodologyfollowed here is based on the WRF model. For CPV systems the primary energy source is the direct normal irradi-ance (DNI), which is dramatically affected by the presence of clouds. Therefore, the reliability of DNI forecasts isdirectly related to the accuracy of cloud information. Two aspects of this issue are discussed here: (i) the effect of

    the models horizontal spatial resolution; and (ii) the effect of the spatial aggregation of the predicted irradiance.Results show that there is no improvement in DNI forecast skill at high spatial resolutions, except under clear-skyconditions. Furthermore, the spatial averaging of the predicted irradiance noticeably reduces their initial error.

    Keywords: DNI, WRF, NWP, forecast.PACS: 88.05.Lg, 96.60.Ub, 92.60.Vb, 94.20.Cf

    INTRODUCTION

    Technologies for harnessing the solar resourcehave experienced a significant development in recentyears. Their future looks even more promising. TheInternational Energy Agency expects that, accordingto a reference scenario, the worlds installed solar

    power capacity will increase from 14 GW in 2008 to119 GW in 2035, with a 8.3% average annual in-crease [1]. Therefore, the challenge for the next fewyears is to achieve a high level of development andintegration, to make this resource competitive com-

    pared to traditional sources of energy, or even tomore established renewable sources, like wind. A

    major effort is being made in this regard [2]. Toachieve this goal, a key aspect concerns the resourceitself (technology aside). The safe and optimal inte-gration of large-scale solar electric power productioninto the energy grid of any country depends on theknowledge of the solar production capacity, which

    in turn is directly related to the available resource.An important intrinsic characteristic of solar ra-

    diation is its very high variability over space andtime, itself directly dependent on weather character-istics. This intermittency in the resource makes a so-lar plants operation and management particularlydifficult. It also makes solar production troublesomefor grid system operators, since it is hardly con-

    trolled and may not be available when it would be ofgreatest value [1]. This ultimately translates into in-cremental exploitation and integration costs. There-fore, prior knowledge of the available resource ofthe near future is essential. Previous experience with

    the wind energy sector has shown that accurate fore-casts play a key role toward the successful integra-

    tion of variable energy sources.

    CPV systems use the beam component of solar

    radiationor direct normal irradiance (DNI)astheir energy source. DNI is primarily affected byclouds, aerosols, and water vapor. Clouds are nor-mally the principal factor affecting the incident solarradiation at the earths surface, since they are mostoften completely opaque to DNI. In contrast, aero-

    sols are most influential under cloudless conditions.The uncertainty in the determination of the physical

    parameters associated with these atmospheric con-stituents is the main source of error in DNI predic-tions. This study focuses on how the latter is affect-ed by cloudiness forecasts.

    Numerical weather prediction (NWP) modelshave been proved to be powerful tools for solar radi-

    ation forecasting [3, 4]. One particular tool that iswidely used by the research community is theWeather Research and Forecasting (WRF) model[5]. WRF, like other NWP models, has a wide rangeof physical parameterizations, providing the possi-

    bility to achieve high spatial and temporal resolu-tions. It is commonly assumed that the higher the

    resolution, the better the physical description andresults will be. This should apply, for instance, to therepresentation of processes that lead to the formationof clouds. In turn, high resolutions are computation-ally very expensive. Therefore, an optimal spatialresolution may exist in solar forecasting.

    This contribution evaluates the role of the WRF

    models horizontal spatial resolution in the reliabil-ity of the DNI forecasts that it can (indirectly) gen-erate. Additionally, the intentional use of spatial av-eraging of the gridded WRF-derived solar field toimprove the models accuracy is evaluated. Themethodology applied is described first. A descriptionof the forecast results is presented in a second step.

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    METHODOLOGY

    Observations and Evaluation Procedure

    This study is conducted for the Andasol SolarThermal Power Plant (37.228 N, 3.069 W; 1100

    m.a.s.l.), Fig. 1. Ten-minute DNI measurements arecollected with an RSR2 radiometer. This instrumentis well maintained and calibrated. Data for the 12-month period 01/12/2009 to 30/11/2010 were first

    corrected for spectral effects, and finally filteredwith a series of quality control tests. For this study,irradiance values corresponding to solar zenith an-gles above 85 were filtered out to avoid the highmeasurement uncertainties associated with low-sunconditions. The original 10-minute data were alsoaveraged to obtain hourly values. From a climato-

    logical standpoint, 2010 was an exceptionallyrainyand therefore cloudyyear.

    Two forecast horizons are studied separatelyhere: hours 124 (day 1, or day ahead), and hours2548 (day 2). Sky conditions are characterized bythe clearness index (kt) to separate clear-sky (0.65