TM5-4DVAR inverse modelling system for atmospheric CH ... · TM Meeting, SRON, Utrecht, 01- 02.12....
Transcript of TM5-4DVAR inverse modelling system for atmospheric CH ... · TM Meeting, SRON, Utrecht, 01- 02.12....
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TM Meeting, SRON, Utrecht, 01- 02.12. 2008 1
TM5-4DVAR inverse modelling system for atmospheric CH4: Sensitivity of derived European emissions on
observational network
Maria Gabriella Villani1Peter Bergamaschi1Frank Dentener1
Jan Fokke Meirink2
Maarten Krol3,4
[1] European Commission Joint Research Centre, Institute for Environment and Sustainability, I-21027 Ispra (VA), Italy[2] KNMI, The Netherlands[3] Wageningen University and Research Centre, Wageningen, The Netherlands[4] Netherlands Institute for Space Research, Utrecht, The Netherlands
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basic principle + objective of inverse modelling
top down estimate of emissions
Kyoto protocol
verification
monitoring of global CH4cyclenatural sources and their feedback to climate change (wetlands, permafrost, CH4hydrates,...)
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Motivation
Objective:
Influence of ground based network on retrieved emissions:
almost (no) knowledge of the apriori distribution (uniform spatial and temporal distribution of a priori emissions)
sets of ground based observations: sites locations; sampling frequency, network density
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Methodology: Sensitivity Experiments
FIRST STEP : Ground-based observations generated by model forward runCH4 emissions inventories = 'true' emissions
Sensitivity experiments use synthetic observations
‘true’CH4 emissions
TM5-4DVARforward mode
CH4 concentrations
INPUT: OUTPUT:
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Methodology: Sensitivity Experiments
SECOND STEP: measurements are assimilated in model runCH4 a-priori emissions = spatially and temporally constant
TM5-4DVARInverse mode
CH4 concentrations
OUTPUT:INPUT:
apriori/unknownCH4 emissions
derived/optimizedCH4 emissions
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TM5-4DVar inverse modeling system
atmospheric a posteriorimixing ratio
a priori
emission month1 month2 month3 month n
yr
observations
y
x =xINI
xEMIS
xPARA
⎡
⎣
⎢ ⎢ ⎢
⎤
⎦
⎥ ⎥ ⎥
Here we use the semi-linear version of the TM5-4DVAR system
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linear vs. non-linear: emissions
linear 4DVAR non-linear 4DVAR
negative emissions
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World-wide Observational network
Legend:Global background(flask)
“Manometer”
CS (current stations)
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EU Observational Networks
European map with the EU stations
Legend:Global background(flask)
CS (current stations)
“Manometer”
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Synthetic measurements
Sample frequency:
Continuous and flask measurements (once per day; per week) - Sampling:
at daytime [12:00-15:00 local time]- DYat nighttime [00:00-03:00 local time]- NI
- Stations: Mountain stations (NI), Boundary layer (DY)
Errors in Observations:- “standard error” [3ppb CH4]
Model errors:- “representativeness” error
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CH4 Emissions
True emissions [forward run] A priori emissions [4D-Var]
512.5 Tg CH4
44.6 Tg CH4 39.7 Tg CH4
517.0 Tg CH4
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Influence of Station Locations
CB4MHD SIL
Mace Head, 25m asl:boundary layer /marine background
Cabauw, 200m asl:boundary layer
Schauinsland, 1205m asl:mountain station
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Influence of Station Locations
CB4
MHD
SIL
Mace Head: boundary layer / marine background
Cabauw: boundary layer
Schauinsland: mountain station
“TRUE”
01-12/2001
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Influence of Station Locations at EU scale
“TRUE”
MHD
SIL
CB4
apriori
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Derived CH4 emissions with observational network
“True”
A posteriori- derived emissions
Larger-scale regionalCH4 emissions close to station locations satisfactorily retrieved
01-2001
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CH4 concentration at selected stations: MHD, CB4, SIL
a priori runa posteriori run
observations
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Sensitivity spatial correlation length
“true”
10 km
100 km
300 km
“Smoothing” effect due to increasing correlation length
01-2001
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EU-Observational Networks
Synthetic Observations ID symbol
Global background (flask)
Global background
“CS”
“CSMAN”
“CSMANCM”
CS (current network)
CS+Manometer
CS+ManometerEU all CM
Datasets shown here:
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Derived CH4 emissions
“True”
CS
CS + Manometer
CS + Manometer (all CM)
Increasing number of stations and sampling frequency:
retrieved CH4 emissions closer to true values and better resolved in NWE countries
01/2001
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Derived CH4 Emissions at EU countries base
CS
CS + Manometer
CS + Manometer (all CM)
apriori
“TRUE”
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Derived CH4 Emissions on EU countries base: NWE
CS
CS + Manometer
CS + Manometer (all CM)
apriori
“TRUE”
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Conclusions
- Current observational network constrain the NWE sector satisfactorily
- Increased network density -> better top-down CH4 emission estimates
-Extended network:-> Significant improvement over Scandinavia -> Major signals from Southern and Eastern Europe cannot be resolved
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Limitations / outlook
-Analyses limited to one month
-Synthetic Observations calculated by assuming no errors in:- measurements- transport model
-Further experiments with additional stations in poorly resolved regions (e.g. Southern and Eastern Europe)
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End of the presentation
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Derived CH4 emissions
“True”
CS
CS + Manometer
CS + Manometer (all CM)A posteriori - true :
01/2001
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Methodology: runs-planning
TM5 runs :- year 2001- ECMWF meteorology - TM5 25 out of 60 vertical layers- Global domain 6x4 deg + zoom over Europe(3x2 and 1x1 deg)- one total source category
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Methodology: TM5