Investigating Chaos Seeding in Perturbation Experiments

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Chaos Seeding within
Perturbation Experiments
             Brian Ancell, Allison Bogusz, Matthew Lauridsen, Christian Nauert
Texas Tech University
11
th
 Workshop on Meteorological Sensitivity Analysis and Data Assimilation
July 1-6, 2018
Aveiro, Portugal
Funded by NSF
Grant AGS1151627
 
?
Background
Project Goal
 Determine the atmospheric effects at a range of temporal and spatial scales
from irrigation, wind farms, and urban development
    
Local Modification
: Observational/modeling evidence for modification
 
                        of temperature, moisture, precipitation, wind, pressure
    
Nonlocal Modification
: Substantially less clear, and prior studies suggest
   
significant downstream modification might occur…
 
Background
Project Goal
 Determine the atmospheric effects at a range of temporal and spatial scales
from irrigation, wind farms, and urban development
    
Local Modification
: Observational/modeling evidence for modification
 
                        of temperature, moisture, precipitation, wind, pressure
    
Nonlocal Modification
: Substantially less clear, and prior studies suggest
   
significant downstream modification might occur…
 
Zhang et al. 2003, JAS
Perturbation energy growth
36-hr accum. precipitation difference
(contour interval=0.5 cm)
12 HR
6 HR
Discovering Chaos Seeding
 WRF perturbation experiments were conducted, and it was
quickly found that tiny perturbations propagated at
unrealistic speeds
 
 
12km
4km
Initial Soil Moisture Perturbation
 
 
PCP DIFFERENCE LAST 6 HRS
 
mm
12 HR
6 HR
Discovering Chaos Seeding
 WRF perturbation experiments were conducted, and it was
quickly found that tiny perturbations propagated at
unrealistic speeds
 
 
12km
4km
Initial Soil Moisture Perturbation
 
 
PCP DIFFERENCE LAST 6 HRS
 
mm
Chaos Seeding
Propagation of Perturbations to Surface Potential Temperature
WRF  Single  Precision
WRF  Double  Precision
Propagation Speed
3600 km/hr!!
Chaos Seeding
Surface pressure differences due to wind farm aggregate in box
Chaos Seeding
These unrealistically fast perturbation propagation speeds are due to
errors communicated through spatial discretization schemes…
Chaos Seeding
These unrealistically fast perturbation propagation speeds are due to
errors communicated through spatial discretization schemes…
 The expansion of the 
numerical domain of influence 
far exceeds that
of any realistic dynamical influence
Chaos Seeding
Chaos Seeding Characteristics
:
 
 Independent of variable (all variables affected)
 Propagates three-dimensionally
 Rapidly seeds entirety of most mesoscale
modeling domains with 1-2 hrs
 A universal problem
- Hohenegger and Schar 2007 
 grid point model
- Hodyss and Majumdar 2007 
 spectral model
Chaos Seeding
Chaos Seeding Characteristics
:
 
 Independent of variable (all variables affected)
 Propagates three-dimensionally
 Rapidly seeds entirety of most mesoscale
modeling domains with 1-2 hrs
 A universal problem
- Hohenegger and Schar 2007 
 grid point model
- Hodyss and Majumdar 2007 
 spectral model
 What are the consequences?
Chaos Seeding: Consequences
Perturbation Below Precipitation
Perturbation in California
Chaos Seeding: Consequences
2-5km Updraft Helicity Tracks (maximum last hour)
Perturbation in California
Chaos Seeding: Consequences
Key Issue
: Chaos seeding excites ALL possible growth
EVERYWHERE, but realistic processes are substantially more
limited
Chaos Seeding: Consequences
Key Issue
: Chaos seeding excites ALL possible growth
EVERYWHERE, but realistic processes are substantially more
limited
Dire Consequence
: Chaos seeding can lead to misinterpretation
of experimental results
 
Chaos seeding unknown
: Evolution of differences
attributed completely to prescribed perturbation
 
Chaos seeding known
: Separation of realistic signal
from growth of “seeds” required
Chaos Seeding: Consequences
Key Issue
: Chaos seeding excites ALL possible growth
EVERYWHERE, but realistic processes are substantially more
limited
Dire Consequence
: Chaos seeding can lead to misinterpretation
of experimental results
 
Chaos seeding unknown
: Evolution of differences
attributed completely to prescribed perturbation
 
Chaos seeding known
: Separation of realistic signal
from growth of “seeds” required
Can Affect the Following Types of Experiments
 Examination of the effects of model parameterizations
 Any initial condition perturbation experiment in a twin
model framework
 Observation impact/data assimilation
 Assessing the effects of boundary conditions
Chaos Seeding: Mitigation
1)
Comparison of realistic vs. chaos seeding spatial patterns
Chaos Seeding: Mitigation
1)
Comparison of realistic vs. chaos seeding spatial patterns
2)
Ensemble sensitivity analysis to distinguish trends not
caused by chaos seeding
Chaos Seeding: Mitigation
1)
Comparison of realistic vs. chaos seeding spatial patterns
2)
Ensemble sensitivity analysis to distinguish trends not
caused by chaos seeding
Chaos Seeding: Mitigation
1)
Comparison of realistic vs. chaos seeding spatial patterns
2)
Ensemble sensitivity analysis to distinguish trends not
caused by chaos seeding
3)
EOF analysis to reveal the leading modes of variability of
atmospheric variables
Chaos Seeding: Mitigation
 96-hr Accumulated Precipitation
Difference in Leading EOFs (Control-Perturbed)
REALISTIC
UNREALISTIC
Chaos Seeding: Mitigation
1)
Comparison of realistic vs. chaos seeding spatial patterns
2)
Ensemble sensitivity analysis to distinguish trends not
caused by chaos seeding
3)
EOF analysis to reveal the leading modes of variability of
atmospheric variables
4)
The use of double precision?
Double Precision?
Summary and Conclusions
1.
Any change to model variables (through initial condition perturbations,
physics, or boundary conditions) causes an unavoidable and rapid
propagation of tiny numerical noise through common spatial discretization
schemes
2.
This tiny noise quickly saturates mesoscale modeling domains, and acts as
perturbation seeds that can grow extremely rapidly through chaotic
processes
3.
Subsequent rapid growth in magnitude and scale of perturbation seeds can
severely limit the ability to accurately diagnose the effects of prescribed
perturbations in the first place
4.
Ensemble sensitivity and EOF analysis are two techniques that can be
effective in discerning a relationship between atmospheric perturbation
variables and downstream evolution
                  
 More detail in Ancell et al. 2018, BAMS Vol. 99, No. 3
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This research project conducted at Texas Tech University delves into the effects of chaos seeding within perturbation experiments on atmospheric conditions, with a focus on local and nonlocal modifications resulting from factors such as irrigation, wind farms, and urban development. By analyzing tiny perturbations, the study reveals rapid propagation speeds and potential impacts on temperature, moisture, precipitation, wind, and pressure, shedding light on the complex dynamics of atmospheric processes.

  • Perturbation Experiments
  • Chaos Seeding
  • Atmospheric Effects
  • Texas Tech University
  • Meteorological Analysis

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  1. Chaos Seeding within Perturbation Experiments Brian Ancell, Allison Bogusz, Matthew Lauridsen, Christian Nauert Texas Tech University 11thWorkshop on Meteorological Sensitivity Analysis and Data Assimilation July 1-6, 2018 Aveiro, Portugal ? Funded by NSF Grant AGS1151627

  2. Background Project Goal Determine the atmospheric effects at a range of temporal and spatial scales from irrigation, wind farms, and urban development Local Modification: Observational/modeling evidence for modification of temperature, moisture, precipitation, wind, pressure Nonlocal Modification: Substantially less clear, and prior studies suggest significant downstream modification might occur

  3. Background Project Goal Determine the atmospheric effects at a range of temporal and spatial scales from irrigation, wind farms, and urban development Local Modification: Observational/modeling evidence for modification of temperature, moisture, precipitation, wind, pressure Nonlocal Modification: Substantially less clear, and prior studies suggest significant downstream modification might occur 36-hr accum. precipitation difference (contour interval=0.5 cm) Perturbation energy growth Zhang et al. 2003, JAS

  4. Discovering Chaos Seeding WRF perturbation experiments were conducted, and it was quickly found that tiny perturbations propagated at unrealistic speeds 6 HR Initial Soil Moisture Perturbation 12 HR 4km 12km mm PCP DIFFERENCE LAST 6 HRS

  5. Discovering Chaos Seeding WRF perturbation experiments were conducted, and it was quickly found that tiny perturbations propagated at unrealistic speeds 6 HR Initial Soil Moisture Perturbation 12 HR 4km 12km mm PCP DIFFERENCE LAST 6 HRS

  6. Chaos Seeding Propagation of Perturbations to Surface Potential Temperature WRF Single Precision Propagation Speed WRF Double Precision 3600 km/hr!!

  7. Chaos Seeding Surface pressure differences due to wind farm aggregate in box

  8. Chaos Seeding These unrealistically fast perturbation propagation speeds are due to errors communicated through spatial discretization schemes

  9. Chaos Seeding These unrealistically fast perturbation propagation speeds are due to errors communicated through spatial discretization schemes The expansion of the numerical domain of influence far exceeds that of any realistic dynamical influence

  10. Chaos Seeding Chaos Seeding Characteristics: Independent of variable (all variables affected) Propagates three-dimensionally Rapidly seeds entirety of most mesoscale modeling domains with 1-2 hrs A universal problem - Hohenegger and Schar 2007 grid point model - Hodyss and Majumdar 2007 spectral model

  11. Chaos Seeding Chaos Seeding Characteristics: Independent of variable (all variables affected) Propagates three-dimensionally Rapidly seeds entirety of most mesoscale modeling domains with 1-2 hrs A universal problem - Hohenegger and Schar 2007 grid point model - Hodyss and Majumdar 2007 spectral model What are the consequences?

  12. Chaos Seeding: Consequences Perturbation Below Precipitation Perturbation in California

  13. Chaos Seeding: Consequences Perturbation in California 2-5km Updraft Helicity Tracks (maximum last hour)

  14. Chaos Seeding: Consequences Key Issue: Chaos seeding excites ALL possible growth EVERYWHERE, but realistic processes are substantially more limited

  15. Chaos Seeding: Consequences Key Issue: Chaos seeding excites ALL possible growth EVERYWHERE, but realistic processes are substantially more limited Dire Consequence: Chaos seeding can lead to misinterpretation of experimental results Chaos seeding unknown: Evolution of differences attributed completely to prescribed perturbation Chaos seeding known: Separation of realistic signal from growth of seeds required

  16. Chaos Seeding: Consequences Key Issue: Chaos seeding excites ALL possible growth EVERYWHERE, but realistic processes are substantially more limited Dire Consequence: Chaos seeding can lead to misinterpretation of experimental results Chaos seeding unknown: Evolution of differences attributed completely to prescribed perturbation Chaos seeding known: Separation of realistic signal from growth of seeds required Can Affect the Following Types of Experiments Observation impact/data assimilation Assessing the effects of boundary conditions Examination of the effects of model parameterizations Any initial condition perturbation experiment in a twin model framework

  17. Chaos Seeding: Mitigation 1) Comparison of realistic vs. chaos seeding spatial patterns

  18. Chaos Seeding: Mitigation 1) Comparison of realistic vs. chaos seeding spatial patterns 2) Ensemble sensitivity analysis to distinguish trends not caused by chaos seeding

  19. Chaos Seeding: Mitigation 1) Comparison of realistic vs. chaos seeding spatial patterns 2) Ensemble sensitivity analysis to distinguish trends not caused by chaos seeding

  20. Chaos Seeding: Mitigation 1) Comparison of realistic vs. chaos seeding spatial patterns 2) Ensemble sensitivity analysis to distinguish trends not caused by chaos seeding 3) EOF analysis to reveal the leading modes of variability of atmospheric variables

  21. Chaos Seeding: Mitigation Difference in Leading EOFs (Control-Perturbed) REALISTIC UNREALISTIC 96-hr Accumulated Precipitation

  22. Chaos Seeding: Mitigation 1) Comparison of realistic vs. chaos seeding spatial patterns 2) Ensemble sensitivity analysis to distinguish trends not caused by chaos seeding 3) EOF analysis to reveal the leading modes of variability of atmospheric variables 4) The use of double precision?

  23. Double Precision?

  24. Summary and Conclusions 1. Any change to model variables (through initial condition perturbations, physics, or boundary conditions) causes an unavoidable and rapid propagation of tiny numerical noise through common spatial discretization schemes 2. This tiny noise quickly saturates mesoscale modeling domains, and acts as perturbation seeds that can grow extremely rapidly through chaotic processes 3. Subsequent rapid growth in magnitude and scale of perturbation seeds can severely limit the ability to accurately diagnose the effects of prescribed perturbations in the first place 4. Ensemble sensitivity and EOF analysis are two techniques that can be effective in discerning a relationship between atmospheric perturbation variables and downstream evolution More detail in Ancell et al. 2018, BAMS Vol. 99, No. 3

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