Title: Other Developments in CCSP Related to WOAP: Emphasis on Reanalysis Randall M' Dole, NOAA CoChair, Cl
1Other Developments in CCSP Related to WOAP
Emphasis on ReanalysisRandall M. Dole,
NOAACo-Chair, Climate Variability and Change
IWGU.S.Climate Change Science Program
2Climate Variability and Change (CVC) IWG -
context for developing research priorities
- Some important considerations
- Recently completed IPCC AR4 assessments
- - Identification of key areas of scientific
uncertainties - - Science research needs related to impacts,
adaptation, and mitigation - Potential emergence of a National Climate
Service. - Key adaptation needs. Provide information at
primary scales for decision-making - regional to
local scales, and across temporal scales from
short-term weather to longer-term climate change. - Key mitigation needs. Must establish closer
connections between climate science and
technological solutions. In U.S., better connect
CCSP to CCTP. - Decision-maker concerns. Major issues How might
climate change alter weather and climate
variability, particularly extreme events? What is
the potential for abrupt changes?
3Current and emerging CVC priority areas
- Major unresolved science issues (AR4) that affect
climate sensitivity and transient climate
response, e.g., cloud feedbacks, aerosol-cloud
interactions, carbon cycle feedbacks, ocean heat
uptake - Climate analysis and reanalysis - Integrated
Earth System Analysis - Attribution of causes for observed climate
variations and changes - Seamless predictions decadal predictability
- Climate variability in a non-stationary climate
- Regional modeling and predictability
- Abrupt climate change
- Ice sheet dynamics/modeling
- Extreme events in a changing climate
4CVC Analysis Priority
- Beginning in 2005, CVC proposed as a high CCSP
priority the Development of an Integrated Earth
System Analysis Capability (IESA). - IESA Goal
- To provide an internally consistent,
comprehensive, high quality record of the state
of the Earth system and how it is evolving over
time. - Achieving this goal requires advances in the
scientific capacity to assimilate observations
from disparate observing systems into earth
system models that include physical, chemical,
and biological processes.
5Key points
- IESA has as an objective to optimize use of the
full array of Earth observations to monitor and
understand changes in climate. - IESA fundamentally links advances in Earth
observations with Earth System Models. - Developing this capability poses a scientific
grand challenge that will require many years to
accomplish. - Developing an IESA will require sustained and
collaborative multi-agency, U.S. and
international efforts.
6Earth System Analysis
Terrestrial Marine Ecosystems
Biogeochemical
Land Surface
Hydrologic
Cryosphere
Glacier and Sea Ice
Ocean
OGCM
Atmosphere
AGCM
Observations
Models
7IESA
Component Analyses
Component Analyses
Component Analyses
(etc.)
Integration Tools, Facilities
8Key Challenges
- Data set preparation and quality control
(inhomogeneities) - Understanding and addressing model biases
- Differences in dominant time scales of various
components - Estimates of error covariances
- Advantages/disadvantages of different
assimilation techniques - Nonlinearities in the coupled system
- Major infrastructure challenges - computing,
data management and delivery needs
9Related U.S. efforts
- Modern Era Retrospective-Analysis for Research
and Applications (MERRA) - Climate Forecast System Reanalysis and
Reforecast Project (CFSRR) - Twentieth Century Reanalysis Project
- Note there are several other related U.S.
efforts, e.g., in carbon data assimilation,
coupled ocean-atmosphere data assimilation, other
components (ocean, land) that are ongoing that
are not covered here. Russ Vose will discuss
another critical component, GCOS/WCRP Working
Group on Observational Data Sets for Reanalysis.
This group is developing a plan for constructing
and managing reanalysis-related data sets, which
will be essential to future efforts.
10Modern Era Retrospective-Analysis for Research
and Applications (MERRA)
- NASA led project (Don Anderson, M. Bosilovich,
S. Schubert, POCs). - GEOS-5 is the core atmospheric model.
- Focus is on the modern satellite era,
1979-present. - Major emphases on climate applications of NASA
research satellites, on improving the water
cycle. - Data assimilation scheme is the gridpoint
statistical interpolation (GSI) scheme with
incremental analysis updates (IAU). - MERRA processing will be followed by a replay
with aerosols for a consistent time series of
meteorology and aerosol distributions. - Production began May 2008, anticipated
completion, Fall 2009.
11GEOS-5 Atmospheric DAS for MERRA (Supported by
NASA MAP Program)
- Analysis
- Grid Point Statistical Interpolation (GSI from
NCEP) - Direct assimilation of satellite radiance data
using JCSDA Community Radiative Transfer Model
(CRTM) - Variational bias correction for radiances
- AGCM
- Finite-volume dynamical core (S.J. Lin)
- Moist physics (J. Bacmeister, S. Moorthi and M.
Suarez) - Physics integrated under the Earth System
Modeling Framework (ESMF) - Generalized vertical coord to 0.01 hPa
- Catchment land surface model (R. Koster)
- Prescribed aerosols (P. Colarco)
- Interactive ozone
- Prescribed SST, sea-ice
- Assimilation
- Apply Incremental Analysis Increments (IAU) to
reduce shock of data insertion (Bloom et al.) - IAU gradually forces the model integration
throughout the 6 hour analysis period
Model predicted change
Correction from DAS
Total observed change
Analysis
12A special thanks to Jack Woollen for help with
the conventional data streams and Leo Haimberger
for the radiosonde corrections!!!!
This builds upon previous collaborative efforts
between NCEP and ECMWF to improve input
observations
13Next Steps
- Developing Components of Future Integrated Earth
System Analysis, with consistent analyses across
all components. - Efforts underway
- Assimilation of constituents (ozone)
- Aerosols
- Land surface (assimilation of ASMR-E soil
moisture retrievals) - Ocean biology (chlorophyll)
- Physical ocean (TOPEX/Jason Altimeter Data)
14Climate Forecast System Reanalysis and Reforecast
Project (CFSRR)
- NOAA/NCEP-led (Hua-Lu Pan, Sura Saha principal
POCs). - Goal is to provide consistent initial conditions
for reforecasts from the CFS for the post-1979
period to enable calibrations for NCEP
operational seasonal predictions. - The NOAA CFS is used to provide a first guess
from a coupled atmosphere-ocean- sea ice - land
system model. - The analysis uses a loose-coupling method the
coupled model provides a common first guess, but
separate data assimilation schemes are used for
each component. - Much higher resolution than earlier reanalysis
efforts (approximately 30-40 km horizontal
resolution vs. 200 km resolution). - Incorporate radiance measurements from
satellites that were not assimilated in earlier
global reanalysis. - Started production runs in June 2008 planned
completion in late 2009.
15CFSRR Components
- Reanalysis
- 31-year period (1979-2009 and continued in NCEP
operations) - High resolution (T382 35 km/L64 levels)
- Coupled system (A-O-L-S) provides background for
analysis - Atmosphere
- Ocean
- Land
- Sea ice
- Required for consistent initial conditions for
seasonal forecasts - Research data set for predictability,
calibration, reforecast studies - Reforecast
- 28-year period (1982-2009 and continued in NCEP
operations ) - Provides stable calibration and skill estimates
for new operational seasonal system - Research for improved (ensemble) postprocessing
studies - Includes upgrades for A-O-L-S developed since CFS
originally implemented in 2004 - Upgrades developed and tested for both climate
and weather prediction - Unified weather-climate strategy (1 day to 1
year)
16Component Upgrades to the CFS
17NCEP Future Plans
- CFS will be upgraded every 7 years
- New forecast system
- Upgrades from operations
- New techniques (4D Var, etc.)
- Higher resolution analysis
- Aerosol and trace gas analysis
- Carbon cycle
- Hydrology, ground water, etc.
- New observations from data mining
- Satellite data treatment (e.g. bias correction)
- Evolution to Integrated Earth System Analysis
- Ongoing work to incorporate these improvements
- Preparation for Reanalysis production phase
- All additions carefully tested
18Twentieth Century Reanalysis Project
- Principal POCS Gil Compo, Jeff Whitaker and
Prashant Sardeshmukh, NOAA/ESRL and CU/CIRES/CDC. - Summary An international collaborative project
led by NOAA and CIRES with support by DOE to
produce high-quality tropospheric reanalyses for
the last 100 years using only surface
observations. - The reanalyses will provide
- First-ever estimates of near-surface and
tropospheric 6-hourly fields extending back to
the beginning of the 20th century - Estimates of biases and uncertainties in the
basic reanalyses - Estimates of biases and uncertainties in derived
quantities (storm tracks, etc.) -
- Initial product will have higher quality in the
Northern Hemisphere than in the Southern
Hemisphere. - US Department of Energy computing award and NOAA
support to produce 1892-2007 by early 2009,
extend back to 1871 by late 2009.
19International Surface Pressure Databank
Subdaily observations assembled under GCOS
AOPC/OOPC Working Group on Surface Pressure
GCOS/WCRP Working Group on Observational Data
Sets for Reanalysis NOAA NCDC, NOAA ESRL, and
CU/CIRES merging station data NOAA ESRL and
NCAR (ICOADS) merging marine data Partners
contributing observations
- NOAA Climate Database Modernization Program
- NOAA Earth System Research Laboratory
- NOAA National Climatic Data Center
- NOAA National Centers for Environmental
Prediction - NOAA Northeast Regional Climate Center at Cornell
- NOAA Midwest Regional Climate Center at UIUC
- Norwegian Meteorological Institute
- Ohio State U. Byrd Polar Research Center
- Proudman Oceanographic Laboratory
- SIGN - Signatures of environmental change in the
observations of the Geophysical Institutes - South African Weather Service
- UK Met Office Hadley Centre
- U. of Colorado-CIRES/Climate Diagnostics Center
- U. of East Anglia-Climatic Research Unit
- U. of Lisbon-Instituto Geofisico do Infante D.
Luiz - U. of Lisbon- Instituto de Meteorologia
- U. of Milan-IFGA
- U. Rovira i Virgili-CCRG
- All Union Research Institute of
Hydrometeorological - Information WDC
- Atmospheric Circulation Reconstructions over the
Earth - Australian Bureau of Meteorology
- British Antarctic Survey
- Danish Meteorological Institute
- Deutscher Wetterdienst
- EMULATE
- Environment Canada
- ETH-Zurich
- GCOS AOPC/OOPC Working Group on Surface Pressure
- Hong Kong Observatory
- ICOADS
- Instituto Geofisico da Universidade do Porto
- Japanese Meteorological Agency
- Jersey Met Dept.
- KNMI
- MeteoFrance
- Meteorological and Hydrological Service, Croatia
20Twentieth Century Reanalysis Project Status
- Fall 2008 1908-1958 (complete and will be
released soon) - Spring 2009 1892-2008 (including time-varying
CO2, aerosols, upgraded GFS) - Fall 2009 1871-1891(coordinate with GFDL
coupled model decadal prediction project) - Data Access Analyses and integrated surface
pressure data base (with feedback) will be freely
available from NCAR, NOAA/ESRL and NOAA/NCDC. - Proposed 2012 Surface Input Reanalysis for
Climate Applications 1800s-2011 - Higher resolution
- improved methods (e.g., Kalman Smoother)
- More input data (e.g., winds and T, extratropical
and tropical storm positions) - latest GFS
- Include uncertainty in forcings (e.g., ensemble
of SSTs and sea ice)
21Near-term CVC Priorities Related to Reanalysis
- Continued development of Earth system models as
a basis for IESA - Data set preparation and quality control
- Research to assess and apply MERRA, CFSRR, 20th
century reanalyses - Research to advance
- - carbon data assimilation
- - assimilation of additional atmospheric trace
gases and aerosols - - coupled ocean-atmosphere data assimilation
- - improved modeling and assimilation of snow
cover and sea ice - - coupled atmosphere-land surface reanalysis
22General Recommendations
- From CCSP Synthesis and Assessment Product 1.3
Reanalysis of Historical Climate Data for Key
Atmospheric Features Implications for
Attribution of Observed Changes. - To better detect changes in the climate system,
improve the quality and consistency of the
observational data and reduce effects of
observing system changes. - Develop analysis methods that are optimized for
climate research and applications. These methods
should include uncertainty estimates for all
reanalysis products. - To improve decision support, develop future
climate reanalysis products at finer space scales
and emphasize products that are most relevant for
applications. - Develop the longest possible consistent record of
past climate conditions. - Develop integrated Earth system models and
analysis systems that include key climate
elements that were not contained in initial
atmospheric reanalyses. Such variables include
those required to monitor changes in the carbon
cycle and to understand interactions among Earth
system components that may lead to accelerated or
diminished rates of climate change. - Develop a more coordinated, effective, and
sustained national capability in analysis and
reanalysis to support climate research and
applications.
23Concluding remarks
National and international partnerships will be
essential to achieving optimal progress in
climate analysis, and more generally developing
an IESA capability. GCOS and WCRP (WOAP) have
been very helpful in providing overall direction
and in helping to make the case for the
importance of climate analysis/reanalysis efforts
in the U.S. CCSP, and specifically CVC IWG,
believe stronger connections to WOAP would be
helpful in improving coordination of U.S. and
international efforts in climate analysis and
reanalysis. One idea CVC could propose to U.S.
agencies a workshop on Critical Needs for
Developing an IESA Capability. Would there be
interest in WOAP in participating in such a
workshop? Questions Would a longer period
reanalysis, e.g. SIRCA, be desirable? Timing?
International role in developing required data
sets? Mechanisms for sharing information on
data/QC issues? Can gold standard data sets be
identified for evaluating reanalyses? What are
metrics that might be used for evaluating
progress?