cdep consortium ocean data assimilation consortium for seasonal-to-interannual prediction (odasi)
DESCRIPTION
CDEP Consortium Ocean Data Assimilation Consortium for Seasonal-to-Interannual Prediction (ODASI). COLA, GFDL, IRI, LDEO, NCEP, GMAO(NSIPP). Ed Schneider (COLA) and Chaojiao Sun (GMAO) Michele Rienecker, Steve Zebiak, Tony Rosati Jim Kinter, Alexey Kaplan, Dave Behringer. - PowerPoint PPT PresentationTRANSCRIPT
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CDEP ConsortiumOcean Data Assimilation Consortium for Seasonal-to-Interannual Prediction
(ODASI)
COLA, GFDL, IRI, LDEO, NCEP, GMAO(NSIPP)
Ed Schneider (COLA) and Chaojiao Sun (GMAO)
Michele Rienecker, Steve Zebiak, Tony RosatiJim Kinter, Alexey Kaplan, Dave Behringer
http://nsipp.gsfc.nasa.gov/ODASI
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CDEP ConsortiumOcean Data Assimilation Consortium for Seasonal-to-Interannual Prediction
(ODASI)
COLA, GFDL, IRI, LDEO, NCEP, GMA
http://nsipp.gsfc.nasa.gov/ODASIhttp://nsipp.gsfc.nasa.gov/ODASI
COLAJim KinterEd SchneiderBen KirtmanBohua Huang
GMAOMichele RieneckerChaojiao SunJossy JacobRobin KovachAnna Borovikov
GFDLTony RosatiMatt HarrisonAndrew Wittenberg
IRISteve ZebiakEli GalantiMichael Tippett
LDEOAlexey KaplanDake Chen
NCEPDave Behringer
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ODASI Themes:1. ODA product intercomparisons (models, assimilation
methodologies, assimilation parameters) using a common forcing data set and common QC’d in situ data streams
Models: MOM4, MOM3, Poseidon, Cane-Patton, LDEO4Methodologies: 3DVAR, OI, EnKF, Reduced state KF and optimal
smoother, bias correction strategiesCoupled Forecast Sytems: CGCMs, Hybrid models, Intermediate
models
2. Development of observational data streams3. Validation of assimilation products in forecast experiments
4. Observing system impacts - focused on TAO:TAO array was established for S-I forecasting.
• Is it effective in its present configuration?• Could it be modified to provide better support for S-I
forecasts?• what is its role c.f. other elements of the ocean observing
system?
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Coupled Data Assimilation Workshop, Portland, April 2003:• Assimilation of subsurface temperature improves Niño-3 forecast skill (usually), but we aren’t sure why (initialization of state, anomalies)
• Forecast errors are dominated by coupled model shocks and drifts
• It is not yet clear as to the “best” method for forecast initialization
• consistent with observed state• consistent with CGCM climatological biases• initialize the model’s coupled modes
Can we use seasonal forecast skill to comment on observing system issues?
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The Experiments:** initial conditions for 1 January and 1 July, 1993 to 2002
** Forecast duration: 12 months
** 6-member ensembles for each system
** The observations: assembled and QC'd by Dave Behringer at NCEP— historical XBTs from NODC, MEDS— TAO from PMEL web site— Argo profiles from GODAE/Monterey server
** Surface forcing: assembled by GFDL— NCEP GDAS daily forcing: momentum, heat, freshwater— surface wind climatology replaced by Atlas’s SSMI surface wind analysis— include a restoration to observed SST and SSS
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The Experiments (ctd):
Initial conditions for forecast experiments prepared using1. All in situ temperature profiles, including the full TAO array2. Western Pacific (west of 170W) TAO moorings3. Eastern Pacific TAO moorings
Hypothesis: the Eastern Pacific data important for shorter lead forecasts and the Western Pacific data important for longer lead forecasts.
Address uncertainty in the results by use of• ensembles• different assimilation systems• different CGCMs• different classes of models (CGCMs, hybrid, intermediate)
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Outline
• Niño 3 SST anomaly Forecast skill — from different models, assimilation systems, observational constraints— January consensus forecast from CGCMs— Reynolds SST is verification
• Ensemble spread
• Skill in the equatorial band (analysis is verification)
• Impacts on the Analysis
• Conclusions
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CGCM1
hybrid1 hybrid2a hybrid2b Intermed1
CGCM2a CGCM2b
January StartsJanuary Starts
All TAO moorings
West TAO moorings
East TAO moorings
Obs (Reynolds)
Niño-3 SST anomaliesNiño-3 SST anomalies
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hybrid2b
Intermed1
CGCM2a CGCM2b
July StartsJuly Starts
hybrid2a Intermedhybrid1
All TAO moorings
West TAO moorings
East TAO moorings
Obs (Reynolds)
Niño-3 SST anomaliesNiño-3 SST anomalies
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CGCM Forecast skill - January starts - multimodel ensemble
All TAO moorings
West TAO moorings
East TAO moorings
Obs (Reynolds)
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Niño3Niño3
Niño4Niño4
January startsJanuary starts July startsJuly starts
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CGCM2a - forecast anomaly correlationsCGCM2a - forecast anomaly correlations
SST - July start HC - July start HC - Jan start
3mo3mo
6mo6mo
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Jan
Jul
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Analysis: Average Temperature in upper 300mAnalysis: Average Temperature in upper 300m
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XBT profiles available per month
Dec 1996: 1440 Jun 1997: 2021
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Vintzileos et al. (GSFC)
Seasonal drift of NSIPP CGCMv1 as a function of forecast lead time
June for each initialization month. January for each initialization monthNiño 3 anomaly correlation of 0.9.
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Coupled Data Assimilation Workshop, Portland, April 2003:• Assimilation of subsurface temperature improves Niño-3 forecast skill (usually), but we aren’t sure why (initialization of state, anomalies)
• Forecast errors are dominated by coupled model shocks and drifts
• It is not yet clear as to the “best” method for forecast initialization
• consistent with observed state• consistent with CGCM climatological biases• initialize the model’s coupled modes
Can we use seasonal forecast skill to comment on observing system issues?
![Page 18: CDEP Consortium Ocean Data Assimilation Consortium for Seasonal-to-Interannual Prediction (ODASI)](https://reader036.vdocuments.mx/reader036/viewer/2022081519/56814558550346895db227b7/html5/thumbnails/18.jpg)
Conclusions:
Early stage of the analysis - we have to study the results in more detail
Statistical significance of results - need more ensemble members and more cases of both warm and cold events for robust conclusions
• Eastern array definitely improves forecast skill• Western array improves skill in central Pacific• Entire array
— best results— probably associated with atmospheric response across the entire Pacific— some indication that get a tighter spread
• results are subtle - complicated by coupled model shocks and drifts