Title: E' S' Takle1, B' Rockel2, W' J' Gutowski, Jr'1, J' Roads3,
1Toward Improving Predictability through
Transferability Experiments
- E. S. Takle1, B. Rockel2, W. J. Gutowski, Jr.1,
J. Roads3, - R. W. Arritt1, I. Meinke2, and C. Jones4
- 1Iowa State University, Ames, IA
- 2GKSS Research Centre, Geesthacht , Germany
- 3Scripps Institution of Oceanography,
UCSD,LaJolla, CA - 4Université du Québec à Montréal
- gstakle_at_iastate.edu
Indo-US Workshop on High-Performance Computing
for Regional Weather and Climate 30 June - 2 July
2005, NCAR, Boulder, CO
2Transferability is proposed as the next step
beyond model intercomparison projects (MIPs)
for advancing our understanding of the global
energy balance and the global water cycle by use
of models
3Regional Model Intercomparison Projects
ARCMIP
GLIMPSE
BALTIMOS
GKSS/ICTS
PRUDENCE
RMIP
SGMIP
QUIRCS
PIRCS
AMMA
IRI/ARC
LA PLATA
4Lessons Learned from MIPs
- No single model stands out as being best at
simulating all variables - Most MIPs have helped individual modelers
identify specific shortcomings of their models - Regional models run in climate mode simulate real
sequences of events if such events are strongly
coupled to the large-scale flow (stratiform
precip vs. convective precip)
5Project to Intercompare Regional Climate
Simulations (PIRCS) Experiment PIRCS 1a
6Lessons Learned
- MIP ensemble means frequently are closer to
observations than any individual model - MIP ensembles recognize extreme events but fail
to capture the magnitude of such extremes - Models generally capture well the diurnal and
seasonal cycles of temperature, although with
larger error under extreme cold and stably
stratified surface conditions (ARCMIP)
7Project to Intercompare Regional Climate
Simuations (PIRCS) Experiment PIRCS 1b
Precipitation (mm/day)
8Lessons Learned
- MIP ensemble means frequently are closer to
observations than any individual model - MIP ensembles recognize extreme events but fail
to capture the magnitude of such extremes - Models generally capture well the diurnal and
seasonal cycles of temperature, although with
larger error under extreme cold and stably
stratified surface conditions (ARCMIP)
9Lessons Learned
- Most models produce too many high-level clouds,
too few mid-level clouds, and too many low clouds - There is wide disagreement on partitioning
between convective and stratiform precipitation
even when precipitation totals agree - Some but not all models can capture the diurnal
cycle of precipitation even with nocturnal
convection - All models tend to produce to many light rain
events and not enough high-intensity rain events
10Lessons Learned
- All models (with 50 km resolution) fail to
capture the timing between maximum and minimum
3-hourly precipitation accumulation from MCSs - Seasonal cycles of precipitation are captured
over a wide range of climate regimes - Precipitation generally is underestimated in both
extreme events and very moist climates
11Transferability Objective
- Regional climate model transferability
experiments are designed to advance the science
of high-resolution climate modeling by taking
advantage of continental-scale observations and
analyses.
12Objective
- Regional climate model transferability
experiments are designed to advance the science
of high-resolution climate modeling by taking
advantage of continental-scale observations and
analyses. - MIPs have helped modelers eliminate major model
deficiencies. Coordinated studies with current
models can advance scientific understanding of
global water and energy cycles.
13Use of Regional Models to Study Climate
- How portable are our models?
14Use of Regional Models to Study Climate
- How portable are our models?
- How much does tuning limit the general
applicability to a range of climatic regions?
15Use of Regional Models to Study Climate
- How portable are our models?
- How much does tuning limit the general
applicability to a range of climatic regions? - Can we recover some of the generality of
first-principles models by examining their
behavior on a wide range of climates?
16Slide source J Roads
17Transferability Working Group
Slide source J Roads
18Transferability Working Group (TWG) Overall
Objective
- To understand physical processes underpinning the
global energy budget, the global water cycle, and
their predictability through systematic
intercomparisons of regional climate simulations
on several continents and through comparison of
these simulated climates with coordinated
continental-scale observations and analyses
19Types of Experiments
- Multiple models on multiple domains (MM/MD)
- Hold model choices constant for all domains
20Types of Experiments
- Multiple models on multiple domains (MM/MD)
- Hold model choices constant for all domains
- Not
- Single models on single domains
- Single models on multiple domains
- Multiple models on single domains
21TRANSFERABILITY EXPERIMENTS FOR ADDRESSING
CHALLENGES TO UNDERSTANDING GLOBAL WATER CYCLE
AND ENERGY BUDGET
ARCMIP
GLIMPSE
BALTEX
BALTIMOS
BALTEX
GKSS/ICTS
PRUDENCE
RMIP
MAGS
SGMIP
QUIRCS
PIRCS
CAMP
GAPP
GAPP
GAME
GAME
AMMA
LBA
LBA
IRI/ARC
CATCH
MDB
LA PLATA
MDB
22Specific Objectives of TWG
- Provide a framework for systematic evaluation of
simulations of dynamical and climate processes
arising in different climatic regions
23Specific Objectives of TWG
- Provide a framework for systematic evaluation of
simulations of dynamical and climate processes
arising in different climatic regions - Evaluate transferability, that is, quality of
model simulations in non-native regions
24Specific Objectives of TWG
- Provide a framework for systematic evaluation of
simulations of dynamical and climate processes
arising in different climatic regions - Evaluate transferability, that is, quality of
model simulations in non-native regions - Meta-comparison among models and among domains
25We recognize that
- The water cycle introduces exponential, binary,
and other non-linear processes into the climate
system
26We recognize that
- The water cycle introduces exponential, binary,
and other non-linear processes into the climate
system - Water cycle processes occur on a wide range of
scales, many being far too small to simulate in
global or regional models
27We recognize that
- The water cycle introduces exponential, binary,
and other non-linear processes into the climate
system - Water cycle processes occur on a wide range of
scales, many being far too small to simulate in
global or regional models - The water cycle creates spatial heterogeneities
that feed back strongly on the energy budget and
also the circulation system
28Strategy
- Identify key processes relating to the water
cycle and energy budget that express themselves
to different degrees in different climatic
regions
29Strategy
- Identify key processes relating to the water
cycle and energy budget that express themselves
to different degrees in different climatic
regions - Create hypotheses that can be tested by use of
MM/MD experiments.
30Locations of hotspots having high
land-atmosphere coupling strength as identified
by Koster et al. (2004) with GEWEX Continental
Scale Experiments overlain.
31Considerations for Developing Hypotheses
- Exploit the availability of CEOP data
- Vertical profiles at isolated points
- Components of energy budget and hydrological
cycle - Sub-daily data
- High-resolution observations of events
- Recognize the limitations of reanalyses in
data-sparse regions
32Slide source B. Rockel
33Candidate Issues Highly Relevant to Hypotheses on
the Water and Energy Cycles
- Static stability (CAPE)
- Diurnal timing
- Seasonal patterns
- Spatial patterns
- Monsoon characteristics
- Diurnal timing of precip
- Onset timing
- Precip spatial patterns
- Snow processes
- Rain-snow partitioning
- Snow-water equivalent
- Snowmelt
- Snow-elevation effects
- Soil moisture
- Frozen soils
- Cloud formation
34Expected Outcomes
- Improved understanding of the water cycle and its
feedbacks on the energy budget and circulation
system
35Expected Outcomes
- Improved understanding of the water cycle and its
feedbacks on the energy budget and circulation
system - Improved capability to model climate processes at
regional scales
36Expected Outcomes
- Improved understanding of the water cycle and its
feedbacks on the energy budget and circulation
system - Improved capability to model climate processes at
regional scales - Improved applicability to impacts models
37Simulating Future Climates with Models Trained
on Current Climates
FCA
Climates
FCAFuture, region A
Variable or Process 2
Variable or Process 1
38Simulating Future Climates with Models Trained
on Current Climates
FCA
Climates
FCAFuture, region A
CCACurrent, region A
Variable or Process 2
CCA
Variable or Process 1
39Simulating Future Climates with Models Trained
on Current Climates
FCA
Climates
FCAFuture, region A
CCACurrent, region A
Variable or Process 2
Model Simulations
CCA, model 1 (on its home domain)
CCA
Variable or Process 1
40Simulating Future Climates with Models Trained
on Current Climates
FCA
Climates
FCAFuture, region A
CCACurrent, region A
Variable or Process 2
Model Simulations
CCA, model 1
CCA, model 2
CCA
Variable or Process 1
41Simulating Future Climates with Models Trained
on Current Climates
FCA
Climates
CCB
FCAFuture, region A
CCACurrent, region A
CCBCurrent, region B
Variable or Process 2
Model Simulations
CCA, model 1
CCA, model 2
CCA
Variable or Process 1
42Simulating Future Climates with Models Trained
on Current Climates
FCA
Climates
CCB
FCAFuture, region A
CCACurrent, region A
CCBCurrent, region B
Variable or Process 2
Model Simulations
CCA, model 1
CCA, model 2
CCB, model 2 (on its home domain)
CCA
Variable or Process 1
43Simulating Future Climates with Models Trained
on Current Climates
FCA
Climates
CCB
FCAFuture, region A
CCACurrent, region A
CCBCurrent, region B
Variable or Process 2
Model Simulations
CCA, model 1
CCA, model 2
CCB, model 2
CCB, model 1
CCA
Variable or Process 1
44Simulating Future Climates with Models Trained
on Current Climates
FCA
Climates
CCB
FCAFuture, region A
CCACurrent, region A
CCBCurrent, region B
Variable or Process 2
Model Simulations
CCA, model 1
CCA, model 2
CCB, model 2
CCB, model 1
CCA
Fully spanning FCA requires More models More
domains
Variable or Process 1
45Plan of Work
- Phase 0 Write an article for BAMS summarizing
lessons learned from various MIPs and describe
how transferability experiments will provide new
insight on the global climate system,
particularly the water cycle and energy budget,
report preliminary results
46Plan of Work
- Phase 0 Write an article for BAMS summarizing
lessons learned from various MIPs and describe
how transferability experiments will provide new
insight on the global climate system,
particularly the water cycle and energy budget,
report preliminary results - Phase 1 Conduct pilot studies
47Transferability Domains and CSE Reference Sites
Slide source B. Rockel
48Plan of Work
- Phase 0 Write an article for BAMS summarizing
lessons learned from various MIPs and describe
how transferability experiments will provide new
insight on the global climate system,
particularly the water cycle and energy budget,
report preliminary results - Phase 1 Conduct pilot studies
- Phase 2 Perform sensitivity studies on key
processes relating to the water cycle. Create and
test hypotheses by MM/MD
49Plan of Work
- Phase 0 Write an article for BAMS summarizing
lessons learned from various MIPs and describe
how transferability experiments will provide new
insight on the global climate system,
particularly the water cycle and energy budget,
report preliminary results - Phase 1 Conduct pilot studies
- Phase 2 Perform sensitivity studies on key
processes relating to the water cycle. Create and
test hypotheses by MM/MD - Phase 3 Prediction, global change, new
parameterizations
50Transferability Consolidates Lessons Learned from
Modeling and Observations
- Models Use experience gained from simulating
home domains
51Transferability Consolidates Lessons Learned from
Modeling and Observations
- Models Use experience gained from simulating
home domains - CEOPS Use dominant features of the water cycle
and energy budget of each CSE to generate
testable hypotheses - Review what has been learned
- Identify unique climate features
52Transferability Experiments Meet GEWEX Phase II
Objectives
- Produce consistent descriptions of the Earths
energy budget and water cycle
53Transferability Experiments Meet GEWEX Phase II
Objectives
- Produce consistent descriptions of the Earths
energy budget and water cycle - Enhance the understanding of how the energy and
water cycle processes contribute to climate
feedback
54Transferability Experiments Meet GEWEX Phase II
Objectives
- Produce consistent descriptions of the Earths
energy budget and water cycle - Enhance the understanding of how the energy and
water cycle processes contribute to climate
feedback - Develop parameterizations encapsulating these
processes and feedbacks for atmospheric
circulation models
55Current Status
- Three models (RSM/Scripps, Lokalmodell/GKSS,
RegCM3/ISU) simulating seven domains - Additional groups have expressed interest (R.
Leung, MM5, WRF C. Jones, Canadian Regional
Model Y. Wang, self-developed model) - More collaborating modeling groups are being
sought - Contact E. S. Takle (gstakle_at_iastate.edu)
56Examples of Analyses
57Slide source B. Rockel
58Slide source B. Rockel
59Slide source B. Rockel
60Slide source B. Rockel
61Summary
- Transferability experiments will allow new
insight on global water and energy cycles that
will advance climate and weather modeling on all
time and spatial scales - Modeling groups are invited to participate and
simulate periods defined by the CEOP on the
transferability domains - Countries are encouraged to consider establishing
Continental Scale Experiments to attract
international interest in studying water and
energy cycles in different climates - Collaborations with the operational and research
communities of India are invited to further
advance this GEWEX activity
http//rcmlab.agron.iastate.edu/twg gstakle_at_iastat
e.edu