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Comercial mision japan
IrSOLaV is a Spanish company that provides solar resource consulting services and data. It was spun off from CIEMAT by researchers with experience in solar energy and radiation. IrSOLaV provides time series solar radiation data from 1994-2012 for India generated from Meteosat satellites. It also provides solar resource reports, typical meteorological year data, plant performance analyses, and consulting services on measuring and analyzing solar radiation data. IrSOLaV works with several research initiatives and partners in solar energy.
Comercial mision japan
- 1. Presentation of servicesfor the Commercial Mission to Japan. 05/2012
- 2. IrSOLaV company profile Spin-off from CIEMAT. Initially formed by researchers with broad experience in Solar Energy and solar radiation knowledge. Methodology for solar radiation derived from satellite information. Solar radiation data provider for most of the main promoters of solar energy projects in Spain and in the Mediterranean area. Consulting services on ground measurement, quality check and solar resource characterization. Close contact to several relevant R&D initiatives: Task 36 of IEA/SHC, COST action on solar radiation and wind forecast. Solar resource consulting services and data provider
- 3. IrSOLaV Products forIndia: 1) Solar Radiation Time series of solar irradiance (GHI and DNI) from 1994-2012 generated from Meteosat satellite information. Solar resource analysis reports with statistical study for the long term. Typical Meteorological Year (TMY) of solar radiation components and temperature. Consulting services on measuring solar radiation and quality reports of solar radiation ground stations and data quality checks. Solar resource consulting services and data provider
- 4. IrSOLaV Products forIndia: 2) Plant performance Analyis of energy production of the plant using SAM, TRSYS (STEC-library), etc.. Report on energy generation with long term analysis (probabilities P50, P70, P90) Solar resource consulting services and data provider
- 5. Solar Radiation extinctionbasis Top of Atmosphere radiation Ozone.……….….... Absorption ( 1%) Air molecules..…… Rayleigh scattering ( 15%) Aerosols…….………..…...…… Scattering and absorption (15% - 100%) Reflection, scattering, absorption (max. 100%) Clouds………….……….. Absorption ( 15%) Water vapor…….……...……… Atmosphere attenuants affect considerably to the DNI on surface Solar resource consulting services and data provider
- 6. Determination of cloudindex Imagen original A. Referencia 09/04/94 Brillancia 09/04/94 Actualizado mediante slot 21= 10 a 10:30 Filtro adaptativo ( ρ n , a ,σ ρ ref ) Albedo x 100 A. aparente Albedo x 100 09/04/94 slot 21= 10 a 10:30 C. de nubosidad x 100 ρ ap − ρ ref C. nubosidad 09/04/94 n= slot 21= 10 a 10:30 ρ nub − ρ ref Solar resource consulting services and data provider 10
- 7. Calculation of hourly clearness index Utilizando los datos medidos en tierra C. nubosidad simultáneamente a los tres años de imágenes de 09/04/94 slot 21 C. de nubosidad x 100 satélite, se entrena una expresión en la que se añaden a la nubosidad variables explicativas como: la declinación, y seis variables cualitativas binarias, fruto de la combinación de seis situaciones posibles: Latitud: sur (<38º), centro (38º<centro<42º) o norte (>42º). Hora del día: I. Claridad mañana (slot = 21) o tarde (slot = 25 o 27) 09/04/94 slot 21 I. de claridad x 100 K Gh = 0,060 ⋅ δ − 0,8073 ⋅ n + (0,7153 ⋅ SM + 0,7136 ⋅ CM + 0,7050 ⋅ NM + 0,7690 ⋅ ST + 0,7438 ⋅ CT + 0,7473 ⋅ NT ) Solar resource consulting services and data provider 11
- 8. Linke turbidity oldMeteotest database worldwide Solar resource consulting services and data provider
- 9. Linke turbidity oldMeteotest database worldwide Solar resource consulting services and data provider
- 10. Linke turbidity newMeteotest database worldwide Aerosol Optical Depth Linke turbidity factor Higher values in the new database of Meteotest Solar resource consulting services and data provider
- 11. Linke turbidity newMeteotest database worldwide Solar resource consulting services and data provider
- 12. Sensitivity of DNIto Linke turbidity on clear sky conditions Dia juliano=200, z=500, Lat=37º N Long=-2º E TL=4, dia juliano=200, Lat=37º N Long=-2º E 1200 1000 TL=2 z=0 m TL=4 900 z=500 m 1000 TL=6 z=1000 m 800 700 800 600 DNI (Wh m -2 ) DNI (Wh m -2 ) 600 500 400 400 300 200 200 100 0 0 0 2 4 6 8 10 12 14 16 18 20 22 24 0 5 10 15 20 25 Hora Hora −δ R mTL DNI = I SC ε e Solar resource consulting services and data provider
- 13. Satellite estimations comparedwith ground data Daily global irradiation in Nagpur estimated from satellite images for year 2007 compared to ground data available from World Radiation data Centre Solar resource consulting services and data provider
- 14. GHI in Ahmadabad Solar resource consulting services and data provider
- 15. Some GHI andDNI comparisons in Gujarat Global horizontal Direct normal Solar resource consulting services and data provider
- 16. Some results formonthly means Monthly means of DNI (1999-2009) estimated from satellite information for several Indian sites. Solar resource consulting services and data provider
- 17. Time series ofhigh temporal resolution: 10-minute data from hourly is needed for simulating system response to transient Solar resource consulting services and data provider
- 18. Solar radiation forecast Solar resource consulting services and data provider
- 19. Solar radiation forecast:short term horizon Predictions of hourly solar radiation with a temporal horizon of 72 hours. Predictions are done 4 times per day at: 00:00 UTC 06:00 UTC 12:00 UTC 18:00 UTC Delivered by FTP, mail or accesable in our web portal www.solarexplorer.info Solar resource consulting services and data provider
- 20. Solar radiation forecast:based on satellite images Predictions of 15-60 minutes solar radiation with a temporal horizon of 6 hours. Predictions are done every hour. Delivered by FTP, mail or accesable in our web portal www.solarexplorer.info Solar resource consulting services and data provider
- 21. Solar radiation forecast:based on sky imagers Predictions of 10-60 minutes solar radiation with a temporal horizon of 3 hours. Predictions are done x minutes. Solar resource consulting services and data provider
- 22. Application to solarplants with storage Solar resource consulting services and data provider
- 23. Solar radiation maps:India Solar resource consulting services and data provider
- 24. Solar radiation maps:Chile - region of ARICA Solar resource consulting services and data provider
- 25. www.solarexplorer.info Solar resource consulting services and data provider
- 26. www.solarexplorer.info Solar resource consulting services and data provider
- 27. Partners Global Forecasters:spin-off from CIEMAT. Wind energy services. STA: spin-off from CIEMAT. Expert in Concentrated Solar thermal power plants. (CSP) Design, simulation of CSP plants, research,…. Instituto de Energia solar: PV expert. Simulation of PV plants. Design of PV plants and auditory of the plants. Geonica: provision and installation of meteorological stations to measure solar radiation. Solar resource consulting services and data provider
- 28. For more detailedinformation please referred to: IrSOLaV, S.L. c/ Santiago Grisolía, 22 IrSOLaV, S.L. c/ Santiago Grisolía, Parque Científico de Madrid Parque Científico de Madrid 28760 Tres Cantos, Madrid 28760 Tres Cantos, Madrid Tfno. +34 (91) 1263612 Tfno. +34 (91) 1263612 Web: www.irsolav.com Web: www.irsolav.com E-mail: info@irsolav.com E-mail: info@irsolav.com Solar resource consulting services and data provider
Editor's Notes
- #7 La radiación que llega a la superficie de la atmósfera puede ser calculada analíticamente en función de la posición solar A su paso por la atmósfera sufre procesos de reflexión, difusión y absorción De esta forma, la radiación global que llega a la superficie terrestre está formada por directa+difusa Por otro lado, la Tierra refleja parte de la radiación solar recibida que junto con la reflejada por las nubes es la que da origen a la señal detectada por el satélite.
- #8 La radiación que llega a la superficie de la atmósfera puede ser calculada analíticamente en función de la posición solar A su paso por la atmósfera sufre procesos de reflexión, difusión y absorción De esta forma, la radiación global que llega a la superficie terrestre está formada por directa+difusa Por otro lado, la Tierra refleja parte de la radiación solar recibida que junto con la reflejada por las nubes es la que da origen a la señal detectada por el satélite.
- #26 Las predicciones de la irradiancia solar semidiaria y la gestión del almacenamiento térmico mediante estrategias óptimas de operación permitirán realizar la programación de la entrega de la producción de las plantas solares maximizando el beneficio económico de las mismas. Tesis Luis Martín
- #27 Las predicciones de la irradiancia solar semidiaria y la gestión del almacenamiento térmico mediante estrategias óptimas de operación permitirán realizar la programación de la entrega de la producción de las plantas solares maximizando el beneficio económico de las mismas. Tesis Luis Martín
- #28 Las predicciones de la irradiancia solar semidiaria y la gestión del almacenamiento térmico mediante estrategias óptimas de operación permitirán realizar la programación de la entrega de la producción de las plantas solares maximizando el beneficio económico de las mismas. Tesis Luis Martín