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Research Axes
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www.eo4geo.eu |
@EO4GEOtalks |
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GHI = BNI + DNI×cos(θ)
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How we can apply Earth Observation data to meet the demands for typical solar energy applications? What are the benefits and drawbacks of such an approach? |
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Surface solar radiation is variable spatiotemporaly
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Forecasting approaches
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Forecasting approaches
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INSAT 3D satellite full domain
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INSAT 3D satellite use for India
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In Sun We Trust is providing free, accurate and easy-to-use tool
for the general public to assess solar potential of rooftop PV systems with the
support of:
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Static yearly irradiation on tilted plans (1-m res.)
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Near on-the-fly computation of intra-day irradiation on tilted plans (1-m res.)
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Clouds are not the only source of solar variability. The irradiance for clear-sky (cloud-free) condition from McClear (CAMS), integrating aerosols, water vapor depending on the Sun topocentric position
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Clear-Sky GHI with Climatology Monthly Linke Turbidity (ESRA Model)
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Clear-Sky GHI from McClear (Aerosol + WV from CAMS)
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Satellite-based all-sky solar data HelioClim-3/CAMS Rad (3 km, 15 min, 2004-,
15+ years)
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At least one year of in-situ pyranometric measurements for local calibration |
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Study of a PV parking shades (100 kWp) impacted by a “new” building
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Example:urban area of of 1.5 km x 1.5
km 20 % PV penetration:
Nameplate PV power injected in the source points
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Temporal evolution of instantaneous PV power potentially injected within a day
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www.eo4geo.eu |
@EO4GEOtalks |
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https://www.atmosphere-upatras.gr/en/ |