global modeling and assimilation office nasa/gsfc gmao merger of nsipp and the dao offices at gsfc...
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Global Modeling and Assimilation OfficeNASA/GSFC
GMAO
Merger of NSIPP and the DAO offices at GSFC
•Science areas:• Subseasonal-to-Seasonal-to-Decadal Prediction• Weather prediction• Chemistry-climate connections• Hydrological Cycle
• Technical areas: satellite data assimilation: usage, new mission design, instrument team products
• Agency Partnerships: NOAA/NCEP, JCSDA, ESMF, NCAR, GFDL, NOAA/CDEP
Merger of NSIPP and the DAO offices at GSFC
•Science areas:• Subseasonal-to-Seasonal-to-Decadal Prediction• Weather prediction• Chemistry-climate connections• Hydrological Cycle
• Technical areas: satellite data assimilation: usage, new mission design, instrument team products
• Agency Partnerships: NOAA/NCEP, JCSDA, ESMF, NCAR, GFDL, NOAA/CDEP
Ensemble mean precipitation and ground temperature anomalies forecast for NDJ
2003
Rienecker, Suarez, et al.
GSFC/GMAO (NSIPP)
Seasonal forecasts with NSIPP CGCMv1:• High resolution: 2° AGCM & 1/3° OGCM• Ocean initial states from ocean data assimilation• Ensembles used to indicate uncertainty
Nino3 SST forecast, initialized in September 2003
NSIPP CGCMv1 Forecast Ensembles NSIPP CGCMv1 Forecast Ensembles
12 month Coupled Integrations: 18 ensemble members
AGCM (AMIP forced with Reynolds SST)
Ocean DAS (Surface wind analysis from R. Atlas, Reynolds SST, Temperature profiles by TAO)
Ocean state estimate perturbations:’s randomly from snapshots
Atmospheric state perturbations: ’s randomly from previous integrations
AGCM: NSIPP1 AGCM, 2 x 2.5 x L34LSM: Mosaic (SVAT)OGCM: Poseidon v4, 1/3 x 5/8 x L27, with embedded mixed layer physicsCGCM: Full coupling, once per day
ODAS: Optimal Interpolation of in situ temperature profiles - daily, salinity adjustment (Troccoli & Haines), Jan1993-present, starting in every month
NASA/GMAO Atmospheric Model
• NASA’s Seasonal-to-Interannual Prediction Project (NSIPP) version 1, Bacmeister et al. (2001)
• Operational prediction model and tested up to ½ degree resolutions
Numerics Finite Difference (Suarez and Takacs 1995)
Cumulus convection
Relaxed Arakawa-Schubert (Moorthi and Suarez 1992)
More detailed condensate budget in the updraft
Large-scale condensation
Diagnostic cloud scheme based on RH, similar to Slingo (1987)
PBL/vertical diffusion
Local diffusion by Louis et al. (1982)
Radiation Chou and Suarez (1999) for SW and Chou and Suarez (1994) for LW
Others Gravity wave drag (Zhou et al., 1996)Mosaic LSM (Koster and Suarez, 1992,1996)
New approach: - weather capable climate model and climate-reliable weather model
– Unified Goddard modeling system (GEOS-5)• AGCM: FVcore + evolving physics: combining GSFC developments
with NCAR, GFDL collaborations• Working to include GISS under a common Goddard model “toolkit”
(with Code 930)• LSM: Catchment LSM + features required for carbon, NWP, long-term
climate
– Modular, ESMF-based development of atmospheric model and subcomponents
New approach: - weather capable climate model and climate-reliable weather model
– Unified Goddard modeling system (GEOS-5)• AGCM: FVcore + evolving physics: combining GSFC developments
with NCAR, GFDL collaborations• Working to include GISS under a common Goddard model “toolkit”
(with Code 930)• LSM: Catchment LSM + features required for carbon, NWP, long-term
climate
– Modular, ESMF-based development of atmospheric model and subcomponents
“Snapshot” of water vapor (white) and precipitation (orange) at 1/2 degree lat/lon resolution.