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NOAA Climate Reanalysis Task Force Technical Workshop
4 - 5 May 2015
Organizers: Jim Carton, Gilbert Compo, Arun Kumar, Suru Saha, Heather Archambault
To view the archive of the presentations, click here to be redirected to the agenda page on the MAPP website.
Workshop Report: Compo, G., J. Carton, X. Dong, A. Kumar, S. Saha, J. S. Woollen, L. Yu, and H. M. Archambault, 2016: Report from the NOAA Climate Reanalysis Task Force Technical Workshop. NOAA Technical Report OAR CPO-4, Silver Spring, MD. doi: 10.7289/V53J39ZZ. Full Report.
Workshop Objectives:
- Report on NOAA Climate Reanalysis Task Force progress
- Exchange reanalysis approaches, algorithms, and techniques currently in use and under development.
- Discuss techniques for addressing outstanding issues in the reanalysis efforts, e.g., presence of spurious discontinuities and trends, coupling of Earth System components, inclusion of new areas such as aerosols.
- Identify the various requirements for reanalysis products.
- Determine strategies and overlaps for national and international reanalysis efforts based on scientific drivers for climate and weather research.
Monday 4 May
9:00 a.m. Welcome
Arun Kumar, NCEP/CPC
9:05 a.m. Introduction to the Climate Reanalysis Task Force and Workshop
Gil Compo, U. of Colorado/CIRES & NOAA/ESRL/PSD
9:20 a.m. What is Reanalysis for?
Huug van den Dool, NCEP/CPC
1. National and International Reanalysis Efforts
Objective: Determine strategies and overlaps for national and international reanalysis efforts based on scientific drivers for climate and weather research.
Scientific and Technical Questions:
1. Would a centralized database for reanalysis observations that all centers can write to and read from be desirable? If so, what software should it based on? ECMWF ODB?
2. How do we bridge the gap between reanalysis requirements for monitoring vs. supporting hindcasts/forecasts?
3. How does long term reanalysis project into long term climate predictions?
4. What advances in integration of the oceans with the earth system are appropriate now?
- Integrated atmospheric correction for SST, SSS, ocean color, and sea level?
- What can we do towards coupled assimiliation?
Session Chair: Gil Compo, U. of Colorado/CIRES & NOAA/ESRL/PSD
Rapporteur: Jeff Whitaker, NOAA/ESRL/PSD
9:40 a.m Plans for Reanalysis at NCEP’s Environmental Modeling Center
Suru Saha, NCEP/EMC
10:00 a.m. Issues, Requirements, and Research towards NOAA’s Next Generation of Climate Reanalyses
Arun Kumar, NCEP/CPC
10:20 a.m. Coffee Break
10:40 a.m. Reanalysis at ECMWF
Dick Dee, ECMWF
11:00 a.m. CMA 40-year GSI based reanalysis: plans and progress
Zhiquan Liu, NCAR
11:20 a.m. MERRA-2, GMAO reanalysis efforts/plans
Ron Gelaro, NASA/GMAO
11:40 a.m. Discussion
Moderator: Heather Archambault, NOAA/CPO
12:10 p.m. Lunch
2. Developments in the Stratosphere
Objective: Discuss techniques for addressing outstanding issues in the reanalysis efforts
Scientific and Technical Questions:
1. What types of observations are needed to ensure accurate stratospheric analyzes going forward?
2. For poorly observed regions, such as stratosphere, what are advantages and disadvantages of bias-correcting observations compared to allowing jumps in reanalysis?
3. How to handle model bias in the stratosphere?
Session Chair: Ron Gelaro, NASA/GMAO
Rapporteur: Erica Dolinar, U. of North Dakota
1:30 p.m. Status at NCEP to improve the stratosphere in reanalysis
Craig Long, NCEP/CPC
1:50 p.m. Aerosol modeling
Sarah Lu, SUNY-Albany
2:10 p.m. Water vapor in the stratosphere
John McCormack, Naval Research Laboratory
2:30 p.m. Aerosol Reanalysis at NASA Goddard Space Flight Center
Arlindo da Silva, NASA/GMAO
2:50 p.m. Discussion
Moderator: Dan Barrie, NOAA/CPO
3:10 p.m. Coffee Break
3. Assimilation Development and Experiments: Atmosphere
Objectives: Exchange reanalysis approaches, algorithms, and techniques currently in use and under development. Discuss techniques for addressing outstanding issues in the reanalysis efforts
1. Can we prove (analytically or by cleverly designed numerical experiment) that we can produce (temporally) homogeneous analyses from an inhomogeneous data input, no matter how egregious the inhomogeneity of the latter?
2. What research approach(es) are required to understand reasons for jumps in climate reanalysis with new observational platforms?
3. In a "pure" Ensemble Kalman Filter, is the ensemble mean analysis meaningful?
Session Chair: Arun Kumar, NCEP/CPC
Rapporteur: Lisan Yu, WHOI
3:30 p.m. Developments in the Ensemble Kalman Filter
Jeff Whitaker, NOAA/ESRL/PSD
3:50 p.m. Forecast results and QBO response from NCEP conventional data only T254 EnKF only cycling semi-Lagrangian Reanalysis in 1970, 1981
Jack Woollen, IMSG & NCEP/EMC
4:10 p.m. Hybrid Data Assimilation at NCEP
Daryl Kleist, U. of Maryland
4:30 p.m. New applications of Data Assimilation to Reanalysis
Eugenia Kalnay, U. of Maryland
4:50 p.m. Reanalysis for Tambora 1815
Gil Compo, U. of Colorado/CIRES & NOAA/ESRL Physical Sciences Division
5:10 p.m. Discussion
Moderator: Gil Compo
5:30 p.m. Close for day
6:30 p.m. Informal dinner
Tuesday 5 May
4. Assimilation Development and Experiments: Ocean and Sea ice
Objectives: Exchange reanalysis approaches, algorithms, and techniques currently in use and under development. Discuss techniques for addressing outstanding issues in the reanalysis efforts
Science and Technical Questions:
1. How far back it is feasible to extend sea ice thickness analysis?
2. What are relative merits of comprehensive couple data assimilation vs. offline analysis of component systems, e.g., ocean, sea-ice?
3. How to interface with ocean reference sites in reanalysis efforts?
4. How to improve the land surface reanalysis?
5. How does long term reanalysis project into long term climate predictions?
6. What advances in integration of the oceans with the earth system are appropriate now?
- Integrated atmospheric correction for SST, SSS, ocean color, and sea level?
- What can we do towards coupled assimiliation?
Session Chair: Suru Saha, NCEP/EMC
Rapporteur: Yan Xue, NCEP/CPC
8:30 a.m. NASA ocean data assimilation
Guilliame Vernieres, NASA/GMAO SSAI
9:00 a.m. Impacts of ocean observations on NCEP GODAS analysis
Yan Xue, NCEP/CPC
9:15 a.m. Advancing Ocean Data Assimilation and Reanalysis
Steve Penny, U. of Maryland & NCEP
9:30 a.m. UMD SODA -- problems and progress
Jim Carton, U. of Maryland
9:45 a.m. The development of NSST within the NCEP GFS/CFS
Xu Li, NCEP/EMC
10:00 a.m. Coffee Break
10:30 a.m. ENSO in a large ensemble of historical reanalyses
Ben Giese, Texas A&M University
10:45 a.m. Land data assimilation at NCEP/EMC
Mike Ek and Jesse Meng, NCEP/EMC
11:00 a.m. Sea ice development at NCEP/EMC
Xingren Wu, NCEP/EMC
11:15 a.m. Discussion
Moderator: Jim Carton, U. of Maryland
12:10 p.m. Lunch
5. Reanalysis Evaluation
Objective: Identify the various requirements for reanalysis products.
1. Should there be an effort by reanalyses providers or reanalysis data distributors to create output files that are as similar to each other as reasonably possible to facilitate use of the data. For example, providing time aggregated files, following certain netCDF standards, using similar attributes, providing long-term mean files, etc.?
2. Would there be a use for a shared code base that could more easily allow users to compare reanalyses and reanalyses derived products (such as budgets) to each other and to observations?
Session Chair: Jim Carton, U. of Maryland
Rapporteur: Steve Penny, U. of Maryland
1:30 p.m. Dry-mass conservation and water consistency in reanalysis
Ricardo Todling, NASA/GMAO
1:50 pm Air-sea heat and freshwater fluxes in Atmospheric Reanalyses
Lisan Yu, Woods Hole Oceanographic Institute
2:10 p.m. Impacts of NCEP Reanalysis R2 and CFSR fluxes on MOM4 simulations
Caihong Wen, NCEP/CPC
2:30 p.m. Evaluation and intercomparison of clouds, precipitation, and radiation budgets in recent reanalyses using satellite-surface observations
Erica Dolinar, U. of North Dakota
2:50 p.m. Coffee Break
3:10 p.m. Investigation of two extreme summer Arctic sea-ice extent anomalies in 2007 and 1996
Xiquan Dong, U. of North Dakota
3:30 p.m. Reanalysis evaluation in polar regions
Richard Cullather, NASA/GMAO
3:50 p.m. Rapporteurs give 5 minute summary of their session
4:15 p.m. Discussion and writing assignments
Moderator: Gil Compo
Leave comments below or Edit this page below to leave discussion topics:
Re: NOAA Climate Reanalysis Task Force Technical Workshop ...
I think Jack's question gets at half of our overarching goal. The other half relates to reconstruction of historical change.
Here are some questions that are an expansion of the CRTF charge:
1) How are we doing with our traditional responsibility monitoring of upper ocean heat content?
>> how is our monitoring of this?
2) What are the advantages (and how do we define this) of improving assimilation and adding new data types?
>> Is an ensemble system worth the computational cost?
>> Is eddy permitting resolution sufficient for now?
>> What new data types (e.g. SSS) need to be included as constraints?
3) How are we progressing towards a cryospheric analysis?
>> What are the outstanding problems to be solved?
>> How do we monitor and evaluate ice volume?
>> Are we putting sufficient resources on this critical area?
4) How is our analysis of nearsurface temperature?
>> Is this a problem that we feel is under control?
>> More generally, are we properly handling diurnal mixed layer dynamics?
5) What advances in integration of the oceans with the earth system are appropriate now?
>> Integrated atmospheric correction for SST, SSS, ocean color, and sea level?
>> What can we do towards coupled assimilation?
Re: NOAA Climate Reanalysis Task Force Technical Workshop ...
Re: NOAA Climate Reanalysis Task Force Technical Workshop ...
Re: NOAA Climate Reanalysis Task Force Technical Workshop ...
Perfection Re: NOAA Climate Reanalysis Task Force ...
Gil,
We have been wrestling with the issues in MERRA-2 that are not improvements over MERRA. We have many improvements, and a few degradations. Perfection, I don't think is attainable at this time. This will happen in any new reanalysis for a while, I suspect. There are many other reasons a MERRA-2 has to go forward with imperfections. Specifically, MERRA is running out of data, and this was the new system that came forward. We had a new method for maintaining mass balance, which we felt would ameliorate the jumps in the water cycle. The only way to fully test that was to run a full on reanalysis. Since it takes so long to integrate, we cannot hold this one, while we patch fix update and run another.
Re: NOAA Climate Reanalysis Task Force Technical Workshop ...