SLIDE 5 PR calculation
𝑄𝑆(𝜀𝑢) = 𝜃𝑏𝑑ℎ𝑗𝑓𝑤𝑓𝑒(𝜀𝑢) 𝜃𝑡𝑞𝑓𝑑 = 𝐻𝑓𝑜𝑓𝑠𝑏𝑢𝑗𝑝𝑜(𝜀𝑢) 𝜃𝑡𝑞𝑓𝑑 × 𝐽𝑠𝑠𝑏𝑒𝑗𝑏𝑢𝑗𝑝𝑜(𝜀𝑢)
Global Horizontal Irradiation (GHI) interpolated from UK Met Office ground based pyranometers [1] as per Colantuono et al. [2]. GHI is transposed to the Global Tilted Irradiation (GTI) using Klein & Theilacker [3]. Provided by donor Calculated from donor’s generation readings
[1] Met Office, “Met Office Integrated Data Archive System (MIDAS) Land and Marine Surface Stations Data (1853-current),” NCAS British Atmospheric Data Centre, 2012. [Online]. Available: http://catalogue.ceda.ac.uk/. [Accessed 17 03 2015]. [2] G. Colantuono et al., “Monitoring nationwide ensembles of PV generators: Limitations and
- uncertainties. The case of the UK,” Solar Energy, 2014.
[3] J. A. Klein and J. C. Theilacker, “An Algorithm for Calculating Monthly-Average Radiation on Inclined Surfaces,” Journal of Solar Energy Engineering, 1981. Jamie Taylor - Sheffield Solar 5