Handout (23.5 MB)
POM-TC utilizes different initialization procedures in different ocean basins in the GFDL, GFDN, and HWRF coupled systems, and the antiquated architecture of the POM-TC code varies from basin to basin to accommodate the various initialization procedures and grid specifications. URI has now developed a new methodology to initialize a unified, basin-independent MPIPOMTC code from different global real-time ocean products available at NOAA and the U.S. Navy. By separating the ocean initialization and grid specification module from the core MPIPOMTC code, the initializations and grid specifications become a plug-and-play feature that facilitates simplified testing, evaluation, and operational implementation. As an alternative to the feature-based initialization in the Atlantic and NCODA elsewhere, for example, MPIPOMTC initialization modules for NOAA's Global HYCOM RTOFS and the U.S. Navy's Global HYCOM products have been developed. By continuing to perform careful evaluation of various ocean initialization products in all ocean basins, it will be possible to ensure that MPIPOMTC is initialized with the best product available for subsequent GFDL, GFDN, and HWRF operational implementations.
MPIPOMTC, like the sbPOM/mpiPOM, is suitable for community distribution for ocean research applications. However, MPIPOMTC is uniquely suited for simulating coupled hurricane-ocean interaction. A key feature of MPIPOMTC is that it can be easily configured to run in an idealized mode rather than real-case mode to isolate the impact of specific physics changes in a scientifically meaningful way. Idealized options include removal of 3D physics (thereby isolating 1D vertical mixing) and using an idealized initial ocean condition, grid specification, bathymetry, and/or forcing. Some of these capabilities were included in research mode in POM-TC, but MPIPOMTC has the new capability to run in a purely 1D mode in which POM's C-grid architecture has be reconfigured to the A-grid, thereby allowing all variables to be calculated at the same horizontal location, with no horizontal averaging or differencing, so each vertical profile is completely independent of the others.