Impact of Tropical Convective conditions on Solar Irradiance Forecasting based on Cloud Motion Vectors

Abstract

Cloud Motion Vector (CMV) estimation from consecutive images is widely used commercially for providing hours-ahead intraday forecasts of solar irradiance and PV power production. The modelling assumptions in these methods are generally satisfied for advective motion, common in mid-latitudes, but strained for tropical meteorological conditions dominated by convective clouds. The region under analysis in this study encompasses both tropical and sub-tropical climatic zones and is affected by seasonal strong convection, i.e., the South Asian Monsoon. The purpose of this study is to benchmark the monthly forecast error of three commonly used motion estimation techniques - Block-match, Farnebäck and TV-L1, for analysing their performance on a seasonal basis. Especially the analysis of the limitations of image processing based Block-match and Optical flow techniques in predicting irradiance during the Monsoon period with frequent convective formation and dissipation is the main focus of this work. Forecasted Cloud Index (CI) maps are validated against reference analysis CI maps for the period 2018-2019 at forecast lead times of 0 to 5.5 hours ahead using the Peak Signal to Noise Ratio (PSNR) metric for estimation of accuracy. Persistence of analysis cloud index maps are used as the reference worst case scenario forecast. Site-level forecasts of irradiance for the same period are validated against ground measured irradiance from two BSRN stations - Gurgaon and Tiruvallur, located in Northern and Southern India respectively. Summer Monsoon pattern of forecast error dominates at the image-wide level and a marked reduction of the 30 minutes ahead forecast accuracy by 3 dB in terms of Peak Singal to Noise Ratio (PSNR) from March to August, can be observed for all the three methods and the worst case persistence scenario. Both the optical flow methods outperform Block-match by 0.5 dB for the entire period of analysis. The Gurgaon BSRN site is affected by Summer Monsoon and shows an increase in nRMSE by a factor of 3 for all the methods from March to August, with the seasonal pattern of forecast error closely matching the image-wide forecast accuracy. The forecast error for the Tiruvallur BSRN station on the other hand reaches its peak in December (Data for October and November are absent), due to its location in the Winter Monsoon climatic zone. Again, the nRMSE for all methods increase by a factor of almost 3 from March to December. The inter-method difference in accuracy is not significant and the seasonal difference (20% nRMSE) dominates.