The IBM Global high-Resolution Atmospheric Forecasting (GRAF) system has extended these capabilities to the Model for Prediction Across Scales (MPAS), the underlying unstructured-mesh model for all current and future operations. To date, the Grid-point Statistical Interpolation software has been utilized to assimilate surface weather observations (operationally) and radiosondes (experimentally) in a partially cycled 3D-variational approach. The analysis increments are computed on a Gaussian grid and interpolated back to a native MPAS mesh at 15/4-km. A cloud analysis utility has also been developed, which ingests site-specific radar reflectivity and operates directly on the mesh, after the DA.
The static B matrix was derived from 180 retrospective cold-start forecasts across a continuous 3-month period, initialized at 00Z and 12Z from the 0.25-degree GFS, 2.5-km global SST analyses, and daily updated NESDIS 4-km green vegetation fraction data. The resolution and duration of each forecast was 15/3-km and 36 hours, respectively. The output at 12- and 36-hours was used as input to the NMC method, to compute the perturbations for regression on a Gaussian grid.
Moving forward, GRAF is employing more advanced DA techniques using the JCSDA’s Joint Effort for Data assimilation Integration (JEDI) software. TWC’s objective is to develop a rapidly updating, fully cycled 3D/4D-EnVar capability with JEDI, driven by an in-house MPAS ensemble (EnKF/LETKF) and higher-resolution deterministic forecast. A summary of the ongoing JEDI work will be discussed, including updates to the static B matrix, observation conversions and priorities, and recent experiments. The latest GRAF roadmap/workflow will be outlined as well.

