The key enhancements to the RUC20 assimilation of observations are 1) an improved optimal interpolation (OI) analysis and 2) the assimilation of GOES cloud-top pressure, as discussed below. The most important changes in the RUC20 OI analysis are the observation preprocessing and a more intelligent matching to background values for surface temperature and dewpoint, near-surface rawinsonde structures, and precipitable water observations.
The RUC20 forecast model is also significantly modified from the RUC40 version, including the following: · Grell/Devenyi (2001) convective parameterization, with ensemble approach to closures (driving parameterized convection) and feedback. · Improved linkage between convective parameterization and other components of the RUC model. · Modified version of Smirnova-RUC land-surface parameterization (Smirnova et al. 2000a) including frozen soil processes and two-layer snow model. · Upgraded RUC/MM5 mixed-phase cloud microphysics (Brown et al. 2000), with improved representation of supercooled liquid water and reduction of excessive amounts of graupel. The microphysics is now called with a 2-min time step in RUC20 instead of the previous 10-min time step.
The presentation will include case study comparisons with the RUC40 and also overall verification statistics from warm, cold, and transition seasons.
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