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An Introduction to NCAR Community Climate System Model (CCSM). Wanli Wu (wanliwu@ucar.edu) National Center for Atmospheric Research (NCAR). What is CCSM. Community Climate System Model, one of elite climate models in the world to picture the complexity of the Earth’s climate.
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An Introduction to NCAR Community Climate System Model (CCSM) Wanli Wu (wanliwu@ucar.edu) National Center for Atmospheric Research (NCAR)
What is CCSM • Community Climate System Model, one of elite climate models in the world to picture the complexity of the Earth’s climate. • It has been developed by NCAR scientists in collaboration with researchers at Universities, National Laboratories. • The CCSM program is sponsored by US NSF and Dept. of Energy. • It houses at National Center for Atmospheric Research with open source codes, documents for all interested users in the world.
Develop a comprehensive model to study the Earth’s Climate. Investigate seasonal and interannual variability of the climate. Explore the history of the Earth’s climate. Estimate the future of the climate. Release of a new version (CCSM3, June, 2004). Studies linking SST fluctuations, extreme events and extratropic variability. Simulations of paleoclimate. Contributions to IPCC AR4. Special issues: J. Climate (June 1, 2006) and IJHPCA (2005) CCSM Program:Scientific Objectives & Recent Accomplishments
CCSM: components • atm: Atmospheric model (CAM3, T85L26) • lnd: Land model (CLM3, T85) • ocn: Oceanic Model (POP 1.4, x1L40) • ice: Sea ice model (CSIM5, x1) • cpl: Coupler (CPL 6)
CCSM3: Computational Requirements • IBM power 3-5 • SGI Altix & Origin • Cray X1/X1E & XT3 • NEC SX • Xeon & Itanium Linux On IBM power 4: T85x1 1146 CPU hrs/myr T42x1 293 CPU hrs/myr T31x3 62 CPU hrs/myr
The Atmospheric model: CAM • Dynamics: • Spectral • Finite volume • Physics: • Deep & shallow convection • Prognostics condensate & precipitation parameterization • Diagnostic parameterization of cloud fraction • Band-model radiative transfer • Prognostic and diagnostic aerosols
The Ocean model: POP • A Bryan-Cox type and z-coordinate model. • Controlled by primitive equations subject to hydrostatic & Boussinesq approximations. • Conserved global ocean volume • Gent-McWilliam isopycnal mixing • KPP vertical mixing • x1L40 or x3L25 • 1/10 degree
Sea ice model: CSIM • Ice dynamics • Ice thermodynamics • Subgrid scale ice thickness distribution (ITD)
Coupling methodology • The physical component models communicate through the coupler in a completely asynchronous manner (different grid and different time steps). • The coupler • governs the execution and time evolution of the entire system. • provides interface flux conditions and state information to each model. • enforces flux conservation.
Pressing Issues, Challenges & Opportunity • Representation of major variability modes • Pacific double ITCZ • Continental precipitation and temperature biases • Eastern Ocean boundary SST biases • Eastern Pacific semiannual SST cycle • Arctic downward short-wave radiation bias
Work in progress: Chemistry • Atmospheric chemistry • Terrestrial C/N cycle, ecosystems • Marine biogeochemical cycle
Work in progress: Nesting • WRF --> CAM • ROMS --> POP
Work in progress: weather-climate interaction • Crossing-scale interaction • Test climate models as weather models
Work in progress: tropical variability • Reduce tropical biases related to MJO, ENSO
Work in progress: Air quality/pollution vs. climate • Climate model application
CCSM4: Community Earth System Model (CESM, 2009?) • A model of everything • More component model options