hereinafter referred to as the ccsm consortium phil jones (lanl) on behalf of all the consorts
DESCRIPTION
COLLABORATIVE DESIGN AND DEVELOPMENT OF THE COMMUNITY CLIMATE SYSTEM MODEL FOR TERASCALE COMPUTING (CDDCCSMTC). Hereinafter referred to as the CCSM Consortium Phil Jones (LANL) On behalf of all the consorts. - PowerPoint PPT PresentationTRANSCRIPT
COLLABORATIVE DESIGN AND DEVELOPMENT OF THE
COMMUNITY CLIMATE SYSTEM MODEL FOR TERASCALE
COMPUTING (CDDCCSMTC)Hereinafter referred to as the CCSM Consortium
Phil Jones (LANL)
On behalf of all the consorts
The SciDAC CCSM Consortium consists of PI: R. Malone4, J. Drake5 , Site-Contacts: C. Ding2, S. Ghan6, D. Rotman3, J. Taylor1, J. Kiehl7, W. Washington7, S.-J. Lin8, Co-Is: J. Baumgardner4, T. Bettge7, L. Buja7, S. Chu4, T. Craig7, P. Duffy3, J.
Dukowicz4, S. Elliot4, D. Erickson5, M. Ham5, Y. He2, F. Hoffman5, E. Hunke4, R. Jacob1, P. Jones4, J. Larson1, J. Lamarque7, W. Lipscomb4, M. Maltrud4, D. McKenna7, A. Mirin3, W. Putman8, W. Sawyer8, J. Schramm7, T. Shippert6, R. Smith4, P.
Worley5, W. Yang2
1Argonne National Lab, 2Lawrence Berkeley National Lab, 3Lawrence Livermore National Lab, 4Los Alamos National Lab,
5Oak Ridge National Lab, 6Pacific Northwest National Lab, 7National Center for Atmospheric Research, 8NASA-Goddard Space Flight Center
Science Goals• Assessment and prediction
– IPCC, national assessments (alarmist fearmongering)
– Energy policy (Dick Cheney’s private sessions)• Regional climate prediction
– High resolution, downscaling, water!• Atmospheric chemistry/ocean
biogeochemistry– Carbon cycle– Aerosols
Project Goals• Software
– Performance portability– Software engineering (repositories,
standardized testing – No Code Left Behind initiative)
• Model Development– Better algorithms– New physical processes (esp. chemistry,
biogeochemistry)
Coupler ArchitectureIssues:Issues: •sequencingsequencing•frequencyfrequency•distributiondistribution•parallelism parallelism •single or multiple single or multiple executablesexecutables•stand alone executionstand alone execution
Version 1.0 ReleasedNovember 2002
• MPH3 (multi-processor handshaking) library for coupling component models
• CPL6 -- Implemented, Tested, Deployed
• ESMF/CCA
Performance Portability• Vectorization
– POP easy (forefront of retro fashion)– CAM, CICE, CLM
• Blocked/chunked decomposition– Sized for vector/cache– Load balanced distribution of blocks/chunks– Hybrid MPI/OpenMP– Land elimination
• Performance modeling w/PERC
Performance
Regional Prediction
Mississipi State
Stanford
Kentucky
Oklahoma State
Atmosphere/Land
Subgrid Orography Scheme
• Reproduces orographic signature without increasing dynamic resolution
• Realisitic precipitation, snowcover, runoff
• Month of March simulated with CCSM
Eddy-Resolving Ocean
0.1 deg0.28 deg
Obs 2 deg
Greenhouse Gases• Energy production• Bovine flatulence• Presidential campaigning
•Source-based scenarios
Aerosol Uncertainty
Atmospheric Chemistry• Gas-phase chemistry with emissions, deposition, transport and photo-
chemical reactions for 89 species. • Experiments performed with 4x5 degree Fvcore – ozone concentration at
800hPa for selected stations (ppmv)• Mechanism development with IMPACT
– A) Small mechanism (TS4), using the ozone field it generates for photolysis rates.
– B) Small mechanism (TS4), using an ozone climatology for photolysis rates.
– C) Full mechanism (TS2), using the ozone field it generates for photolysis rates.
Zonal mean Ozone, Ratio A/C
Zonal mean Ozone, Ratio B/C
Ocean Biogeochemistry• LANL Ecosystem Model
– nutrients (nitrate, ammonium, iron, silicate)– phytoplankton (small, diatom, coccolithophores)– zooplankton– bacteria, dissolved organic material, detritus– dissolved inorganic carbon (DIC), alkalinity– trace gases (dimethyl sulfide, carbonyl sulfide,
methyl halides and nonmethane hydrocarbons)– elemental cyclings (C,N,Fe,Si,S)
Ocean Biogeochemistry
•Iron Enrichment in the Parallel Ocean Program•Surface chlorophyll distributions in POPfor 1996 La Niña and 1997 El Niño
Global DMS Flux from the Ocean using POP
The global flux of DMS from the ocean to the atmosphere is shown as an annual mean. The globally integrated flux of DMS from the ocean to the atmosphere is 23.8 Tg S yr-1 .
Potential U.S. ParticipantsRuns completed• Starley Thompson LLNL, David Erickson ORNL (PCM-IBIS)
C-cycle code completed, tested coupled to relevant GCM• Inez Fung, Scott Doney UC Berkeley (CCSM1-OCMIP2-CASA derivative)• Fung, Hoffman, Doney, Lindsay (CCSM3-CLM3-CASA’ )?
C-cycle code completed, run off-line completed• Gordan Bonan NCAR (CCSM2-LPJ derivative - see Bonan et al. 2003. GBC
11:1543-1566)• Joerg Kaduk Stanford (CCM? Or UCLA-SiB2)• Robert Dickinson Georgia Tech (CCSM?-CLM enhanced)
C-cycle code under development• Peter Thornton NCAR (CCSM3-Biome-BGC derivative)• Erickson, Post, King, Gu ORNL (PCM-IBIS-GTEC loose coupling) [acclimation,
moisture profile, diffuse radiation effects on veg]• Ocean POP - OBGCM LANL (CCSM3-POP)• DOE Deliverables: aerosol chemistry-carbon coupled model (CCSM3-IBIS)
Extensions for Carbon CycleDecadal-Cent.Priority
CarbonDynamicsGPPRespirationAllocation YESDecompositionNitrogen dynamics YESTrop Ozone effects YESTemp. acclimation YESCO2 acclimation YESDiffuse solar effects YES
Decadal-Cent.Priority
VegetationDynamicsDisturbance-recovery
YES
BiogeographyLand use/land coverchange
YES
HydrologicalEffectsConsistent w/ LSMGrowthForest Mortality YESDecompositionETWetlands-trace gases
Accept CAM chemistry package from SciDAC (July 2004)• Meet with NCAR BGC working group to mesh science plans of this project to those of
the NCAR BGC working group (July 2004)• Perform additional CAM/FV vectorization enabling chemistry/sulfur simulations on the
X1 (Oct 2004)Accept CCSM3/IBIS model from LLNL LDRD (Oct 2004)• Implement sulfur chemistry in CAM ozone photochemistry package (Oct 2004)• Enable ocean produced DMS emissions to be processes through coupler and into CAM
atmospheric physics/chemistry package (Oct 2004)
Where we would like to beAccurate regional modeling of carbon sources and sinksCoupling of biogeochemical processes for climate variability on decadal to century time scales