Report to WGOMD on GFDL Ocean Modelling Activities Stephen Griffies NOAA/GFDL (and CSIRO) IPCC AR4 activities Model developments

IPCC activities Completed development of AR4 coupled climate model in 2004, and submitted simulations to PCMDI 2004/2005. ~1 degree ocean (mom4) with 50 levels and 1/3 degree at equator. Described at previous meetings. Numerous studies now being conducted to document the model’s design and simulation characteristics. Will take years to fully evaluate.

GFDL Coupled Model results

References

Ocean Model

Plans for GFDL ocean model development A briefing to WGOMD Inform WGOMD of plans for MOM4 over next 6 months Speculate on 3-5 years research/development goals and applications involving ocean models.

MOM4 as of November 2005 Four public releases MOM4p0a Jan2004 MOM4p0b Mar2004 MOM4p0c Oct2004 MOM4p0d May2005 Roughly 300 registered users from 30 countries using ~35 computational platforms. They represent about 1200 scientists, engineers, and programmers using the code and simulation results for research and development.

MOM4 user statistics Vertical lines are intermediate code releases: mom4p0a mom4p0b mom4p0c mom4p0d

GFDL Applications of MOM4 IPCC Global climate change modelling: –Ocean component to the GFDL AR4 climate change models. –Developed largely for global climate modeling applications. –~50 GFDL scientists directly involved with this research and development. Earth system modelling: –interactive land, atmosphere, ocean biogeochemistry and ecosystems –~30 scientists at GFDL and Princeton University Global and regional process studies: –paleo-oceanography –idealized climate change simulations –thermohaline shutdown –physical process studies –~20 scientists, visiting researchers, post-docs, graduate students

Gravity current-entrainment CPT

Eddy mixed layer interactions CPT

MOM4p1: vertical coordinate features Partial step topography Trivial pressure gradient errors Decades of experience Well known limitations Irregular and variable computational domain (i.e., land/sea masks and vanishing surface layer) free surface z-model: mom4p0 Terrain following σ-model Smooth topography Regular computational domain (no land/sea masks) Time independent computational domain (-1 < sigma < 0) Pressure gradient errors: requires topography filters Difficult neutral physics implementation: not commonly done in sigma- models Irregular computational domain (i.e., land/sea masks needed) Time independent computational domain (-H < z* < 0): no vanishing layers. Negligible pressure gradient errors since isosurfaces are quasi- horizontal. Correspondingly, can use the same neutral physics technology as in z-models.

Evolution of GFDL ocean codes Evolution is in response to many inputs –New applications: Refined resolution climate models Biogeochemistry and ecosystem applications Earth system modeling Coastal impacts of climate change Non-hydrostatic processes at very refined resolutions –Enhanced features: physical parameterizations (e.g., mixed layers, mesoscale eddies) algorithm fundamentals (e.g., time stepping, vertical coordinates) better understanding of the ocean (e.g., equation formulations) –Computational efficiency and platform portability –Input from the international user communities (HIM, MITgcm, MOM4) Main developers: Alistair Adcroft, Bob Hallberg, Steve Griffies

Evolution Path MOM4p1: ~March 2006 with rudimentary generalized vertical coordinate features to expand mom4 applications. HIM-Fortran: Hallberg Isopycnal Model, publicly supported within GFDL Flexible Modeling System (FMS); GFDL development now aimed at coupled simulations to compare w/ mom4-based coupled model. Research: Merge three fundamental perspectives –non-hydrostatic z-modeling from MIT (Adcroft) –hydrostatic isopycnal modeling from HIM (Hallberg) –Global ocean climate modeling from MOM4 (Griffies) Key NOAA application: climate impacts on coasts –Global “BackBone Model” ~10 km with nest to ~1 km –Tides, wave breaking, storm surge, sediment transport, etc. ~ for first public code release

Horizontal grids: nesting and cubed sphere Multiple 2-way nested regions Mass and tracer conservation: Most nesting implementations in ocean and atmospheric models are non-conservative Time sub-cycling: coarse region not constrained by time step used in fine region. Essential for economical global models with nests. Envision applications in areas such as –global climate models: boundaries, choke points, etc. –Regional modeling with nests to estuary scale –Coastal biogeochemistry and ecosystems Present development –general grid description –tools for parallel computing and coupled modeling –analysis/visualization tools –shallow water test cases Cubed Sphere –technology from MITgcm –Also envisioned for finite volume atmosphere model

Main Applications Coastal impacts of climate change Earth System Modelling w/ eddying simulations (~1/3 to 1/4 degree mercator with twoway nesting in selected critical regions) NOAA “BackBone” model, with ~1/10 global to be nested with finer grids in certain coastal areas. For use by many projects within NOAA. nonHydrostatic process studies and very refined coastal and estuary simulations University PI and student research and education

HYDROSTATIC NON-HYDROSTATIC ~100 km ~10 km ~1 km ~20 m ~100 m ~1000 km HIM + MIT + MOM = ???

Unified GFDL Ocean Code Bring together our understanding of the ocean and how to simulate a wide range of scales. Various algorithms with stepwise evolution involving suites of applications to test methods and flesh out favourable approaches. This effort is a major research and development project, presently in its early stages at GFDL. Much research remains to determine particulars of algorithms. Various efforts (e.g., HOME) to develop a US community model have failed to garner funds. GFDL is committed to this project using in-house resources, and will involve outside collaborators as best as possible.