Render the existing JPV Develop a fully method fully probabilistic probabilistic Joint by means of bivariate H? 2-3 2015? > 500 1 Peak-Volume Copula probability theory method. and refine its regionalisation. Develop PMP isohyets for southern Africa as per the Modernise and refine updated WMO method, the existing refine and regionalise SANCOLD H? 2 2016? 100 - 500 2 existing empirical minimum Guidelines storm rainfall losses and PMF method. implement new refined SUHs. Update the Kovacs historical maximum flood methods 1.2.7.1 and 1.2.7.3 peak database with latest Postgraduate (Part 1) Update and flood peak measurements study refine the RMF and with a H? 2 2015? 100-500 1 flood started at Univ. method and its of RMF Stellenbosch regionalisation. according to design measurable rationales. By consolidating large A.1.2.7.2 Approach annual maximum flood Extreme 1: Develop peak samples of about annual 1000 station-years, exceedence according to spatially H? 3 2015? > 500 1 probability extensive homogeneous methodology for flood regions, high-RI flood extreme floods. peaks, or the RIs of empirically/
Develop a fully probabilistic Joint Peak-Volume method. Render the existing JPV method fully probabilistic by means of bivariate Copula probability theory and refine its regionalisation. H? 2-3 2015? > 500 1 Extreme design flood methods Modernise and refine the existing SANCOLD Guidelines PMF method. Develop PMP isohyets for southern Africa as per the updated WMO method, refine and regionalise existing empirical minimum storm rainfall losses and implement new refined SUHs. H? 2 2016? 100 - 500 2 1.2.7.1 and 1.2.7.3 (Part 1) Update and refine the RMF method and its regionalisation. Update the Kovacs historical maximum flood peak database with latest flood peak measurements and with a of RMF according to measurable rationales. H? 2 2015? 100-500 Postgraduate study started at Univ. Stellenbosch 1 A.1.2.7.2 Approach 1: Develop annual exceedence probability methodology for extreme floods. By consolidating large annual maximum flood peak samples of about 1000 station-years, according to spatially extensive homogeneous flood regions, high-RI flood peaks, or the RIs of empirically/ H? 3 2015? > 500 1
NFSP_SANCOLD_2014.docx