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108    CHAPTER 3 Forecasting of Intermittent Solar Energy Resource




                         of NWP based on a postprocessing technique to reduce systematic forecast errors.
                         The MOS technique consists in using ground irradiance measurements to correct
                         localized errors from NWP models. The technique gives very good results and
                         should allow to generate a global and valuable method coupling machine learning
                         and NWP.
                         7.2.2 Nonhydrostatic Atmospheric Models
                         The goal of the NWP use is to produce a model of solar irradiation with an error
                         below 25% (nRMSE). Actually, the global models are not efficient but in the future,
                         local models based on nonhydrostatic equations will allow to obtain very good fore-
                         casts (for all the horizons). Note that, with this kind of models, the time and spatial
                         resolution can be increased and the global irradiation is available for an overall ter-
                         ritory with a resolution upper than 500 m.
                         7.2.3 High Accuracy Irradiance Measurement
                         For all the models tested it is important to validate the output with ground measure-
                         ment. The problem is obvious, but there is not enough installed sensors to validate all
                         the model through the world map. To overcome this problem, a database such as
                         Helioclim, for instance, should play an important role in the next few years. Indeed,
                         Helioclim-3 regroups time series of radiation components over a horizontal, fix-
                         tilted, and normal plane for the actual weather conditions as well for clear-sky con-
                         ditions. Geographical coverage corresponds to the Meteosat satellite field of view,
                         that is, it covers Europe, Africa, Atlantic Ocean, and Middle East. The spatial res-

                         olution is 3 km at Nadir, and approximately 4e5km at 45 latitude. Data are avail-
                         able with a time step ranging from 15 min to 1 month. The time coverage is from
                         February 2004 up to current day-2 for HC3v5 and up to day-1 for HC3v4 (http://
                         www.soda-pro.com/fr/home).




                         8. CONCLUSION
                         This chapter has demonstrated the fundamental importance of the production fore-
                         casting for intermittent and stochastics power plants. Without reliable predictions,
                         renewable energy will not reach a high level of integration as their management
                         would add considerable complexity to the electricity network.
                            Some information about the intermittence cost, increasing the energy production
                         cost, were introduced and a literature review is in total agreement with the fact that a
                         reliable forecasting of the renewable production at various temporal horizons can
                         decrease these costs and make the intermittent renewable energy more competitive.
                            The main forecasting methods for solar radiation have been presented and clas-
                         sified according to the temporal horizon. The accuracy of these methods depends on
                         the meteorological characteristics of the site where the solar plant is installed.
                            At last, new perspectives of the forecasting science were shown and prove that
                         significant progress remains to be made to reach the perfect forecasting model.
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