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09 - Kriging OK and DK correction
May 22, 2024 - PhD project - Modelling current and future water resources availability in an Alpine catchment exploited for hydropower production
Citrini, Andrea, 2024, "09 - Kriging OK and DK correction", https://doi.org/10.13130/RD_UNIMI/CZ8IOH, UNIMI Dataverse, V1
Spatial Kriging OK and DK correction of the hourly radar precipitation values for each centroid of the study area. Once the residuals at the rain gauge locations were calculated with respect to the radar, the error was interpolated exploiting the Ordinary (OK) and Detrended (DK)...
08 - IDW and TPS correction
May 22, 2024 - PhD project - Modelling current and future water resources availability in an Alpine catchment exploited for hydropower production
Citrini, Andrea, 2024, "08 - IDW and TPS correction", https://doi.org/10.13130/RD_UNIMI/YOL2C5, UNIMI Dataverse, V1
Spatial IDW and TPS correction of the hourly radar precipitation values for each centroid of the study area. Once the residuals at the rain gauge locations were calculated with respect to the radar, the error was interpolated exploiting the Inverse Distance Weighting (Thin Plate...
07 - CDF and Copula correction
May 22, 2024 - PhD project - Modelling current and future water resources availability in an Alpine catchment exploited for hydropower production
Citrini, Andrea, 2024, "07 - CDF and Copula correction", https://doi.org/10.13130/RD_UNIMI/EWFQQ2, UNIMI Dataverse, V1
Point – based CDF and copula correction of the hourly radar precipitation values for each centroid of the study area. Precipitation series for each centroid were extrapolated from the radar raster (for each hour) and then corrected via CDF and copula correction by exploiting obse...
06 - TIN correction
May 22, 2024 - PhD project - Modelling current and future water resources availability in an Alpine catchment exploited for hydropower production
Citrini, Andrea, 2024, "06 - TIN correction", https://doi.org/10.13130/RD_UNIMI/GCH3HM, UNIMI Dataverse, V1
Point – based TIN correction of the hourly radar precipitation values for each centroid of the study area. Precipitation series for each centroid were extrapolated from the radar raster (for each hour) and then corrected via TIN by exploiting observed data from the three nearest...
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