Title Progress in the development and results of the UNIFIED EMEP model Presented by Leonor Tarrason...
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Transcript of Title Progress in the development and results of the UNIFIED EMEP model Presented by Leonor Tarrason...
TitleProgress in the development and results of the UNIFIED
EMEP model
Presented by Leonor TarrasonEMEP/MSC-W
29th TFIAM meeting, Amiens, France, 10-12 May 2004
Outline
Meteorologisk Institutt met.no
• TFMM workshop REVIEW OF THE UNIFIED EMEP MODEL
• Progress at MSC-W in modelling PM mass
• PM emission speciation
• Water bound PM mass
• SOA empirical approaches to SOA modelling
• Meteorological variability and consequences for SR calculations
Evaluation of the EMEP model Mandate
Meteorologisk Institutt met.no
Examination of the processes and meteorological parameterizations, chemical mechanisms and the sources of model input data; and
Evaluation of the model performance against daily observations of key model species and fluxes from the EMEP, AIRBASE and national monitoring networks for 1980, 1985, 1990, 1995, 1997, 1998, 1999 and 2000; and
A consideration of the source-receptor relationships for sulphur, nitrogen, ozone and suspended particulate matter (PM mass).
TFMM workshop to review and evaluate the Unified EMEP model was hold in Oslo 3-5 november 2003, with 72 participants, 2 European model inter-comparisons (TNO-EMEP, EURODELTA), individual country reviews
Evaluation of the EMEP model Conclusions O3
Meteorologisk Institutt met.no
For ozone, it was concluded that the model:
is suitable for the assessment of vegetation exposure and for the assessment of human health effects on the regional scale with the aim to support European air quality strategies.
is suitable for the establishment of source-receptor data for human health exposure and vegetation exposure/uptake of ozone on the regional scale.
is able to predict changes in ozone concentrations caused by changes in precursor emissions on a European level.
“The model showed an excellent level of performance for daily maximum ozone concentrations. For nitrogen dioxide, the performance was less good, in common with all other models, possibly due to subgrid variations. The model shows a tendency to underestimate the episodic ozone peak concentrations (>60ppb) and uncertainties will be higher for source-receptor compared with extreme value statistics”
Evaluation of the EMEP model Conclusions O3
Meteorologisk Institutt met.no
Long-term work plan recommendations:
Further consideration should be given to:
• interactions with local scale air pollution (particularly concerning the outcome of the CITY-DELTA exercise)
• the continued increase in background ozone concentrations for the assessment of trends
• the model and measured trends in VOCs and oxidation products and
• to developing improved partitioning of stomatal and non-stomatal fluxes of ozone to vegetation, validated against field observations.
Evaluation of the EMEP model Conclusions PM
Meteorologisk Institutt met.no
For suspended particulate matter, it was concluded that the model:
in its present form significantly underestimates total PM concentrations due to unknown processes and emissions.
is however able to calculate the regional component of main anthropogenic PM fractions (sulphate, nitrate, ammonium, some primary components) with enough accuracy for the assessment of the outcome of different control measures.
requires urgent attention with the aim of developing the model further for the full assessment of the anthropogenic fraction of PM2.5.
Evaluation of the EMEP model Conclusions PM
Meteorologisk Institutt met.no
Short term recommendations:In the short term, attention should be given to:
• the evaluation of present emission inventories
• the analysis of measurements and anthropogenic emissions of specific species of PM and the contribution to particle mass from particle-bound water
• the exploration of empirical approaches to the development of a model for secondary organic aerosol formation based on available data and knowledge.
Long-term recommendations: In the longer term, evaluations are required against speciated monitoring data,
the inclusion of improved emission inventories, the inclusion of biogenic primary emissions, the formation of secondary biogenic aerosols in order to achieve full mass closure.
Meteorologisk Institutt met.no
Progress at MSC-W modelling PM mass
still plenty of uncertainties …..
PM EmissionsChemical speciation and size distribution of PM Emissions on-going work at PM Expert Group under TFEIP
Meteorologisk Institutt met.no
PM2.5OC (%) EC (%) Mineral dust (%)
Power generation 33 33 33
Residential and other combustion 50 20 30
Industrial combustion 33 33 33
Production processes 0 20 80
Extraction & distribution of fossil fuels 40 50 10
Solvent and other product use 40 20 40
Road transport 40 20 40
Other mobile sources and machinery 40 20 40
Waste treatment and disposal 10 60 30
Agriculture 70 0 30
Size distribution (Aitken/accum) 15 / 85 (20 / 80) 15 / 85 (20 / 80) 0 / 100
Coarse PM = PM10 - PM2.5- - 100
Density, (kg/m3) 2000 2000 2600
Diameter 0.05/0.3 µm (0.02/ 0.2)µm 5 (6.5) µm
Chemical composition of PM (1):
Meteorologisk Institutt met.no
Spain
0
5
10
15
20
25
Obs Bemantes
Mod Bemantes
Obs Monagrega
Mod Monagrega
Obs Montseny
Mod Montseny
NDotherdustSSOC+ECNH4NO3SO4
Unaccounted PM mass
Vienna Streithofen
PM2.5 Austria,1-6/2000
PM10 PM25
Largest discrepancy:
OC, EC,
dust
Chemical composition of PM (2):
Meteorologisk Institutt met.no
Non-C atoms in organic aerosol
Particle-bound water
Measurement artefacts
Full chemical mass closure is rarely achieved .
Unaccounted PM mass - up to 35-40%
Gravimetric method (Reference, EU and EMEP) for determining PM mass requires 48-h conditioning of dust-loaded filters at T=20C and Rh=50% -does not remove all water! At Rh=50% particles can contain 10-30% water
Gravimetrically measured PM mass does not represent
dry PM mass!!!
Chemical composition of PM (3):
Meteorologisk Institutt met.no
Spain
0
5
10
15
20
25
Obs Bemantes
M od Bemantes
Obs M onagrega
M od M onagrega
Obs M ontseny
M od M ontseny
ND/waterotherdustSSOC+ECNH4NO3SO4
Unaccounted PM mass in obs
Aerosol water in model
Vienna Streithofen
PM2.5 Austria,1-6/2000 (AUPHEP)
PM10 PM25
To what extend can particle-bound water explain the model underestimation of measured PM?
Meteorologisk Institutt met.no
Accounting for particle-bound water in PM2.5
Model calculations vs. gravimetric PM2.5 (EMEP, 2001)
Dry PM2.5
N=13
Bias=- 47%
Corr=0.69
N=13
Bias=-28%
Corr=0.68
Dry PM2.5 + water
Meteorologisk Institutt met.no
Model calculated dry PM2.5 (blue) and PM2.5 including aerosol water (black) vs. measured PM2.5 (red)
Accounting for water in modelled PM2.5 gives better agreement with measurements…BUT: verification of model calculated aerosol water is needed
An example: Vienna
Meteorologisk Institutt met.no
Daily PM2.5 (June 1999 - June 2000) :
What is needed:
“component-wise” verification of modelled PM
Daily series of SO4, NO3 and NH4 in PM2.5
Meteorologisk Institutt met.no
NO3
NH4
SO4
OC
EC
Na
EC PM emissions validation
Adding a “standard” SOA module to EMEP model gives too much OC and produces summer maxima that are not observed!
(D. Simpson, on-going research)
Organic aerosol in the EMEP model
Meteorological variability - Daily summer ozone (JJA)
AVG -1995
AVG -2000
AVG -1996
AVG -1998
AVG -1999
AVG -1997
Percentage variability of PM2.5due to meteorological conditions
Meteorologisk Institutt met.no
2003-1999 2002-2001
25-35% over European countries 10-20% over European countries
O3 mean Differences due to meteorological conditions
Meteorologisk Institutt met.no
5-10% variations due to meteorology
Reduction in mean concentrations of PM2.5
due to emission changes in 2010
Meteorologisk Institutt met.no
1999 met 2003 met
25-35% changes due to envisaged reduction in emissions (2010)
Similar to meteorological variability ranges from 1999 – 2003
Reduction in mean O3 concentrations due to emission changes in 2010
Meteorologisk Institutt met.no
1999 met 2003 met
5-7% changes due to envisaged reduction in emissions (2010)
Similar to meteorological variability ranges from 1999 – 2003
Reduction in mean concentrations of PM2.5
due to emission changes in 2020
Meteorologisk Institutt met.no
1999 met 2003 met
35-50% changes due to envisaged reduction in emissions (2020)
Considerably larger than meteorological variability ranges from 1999 – 2003
Reduction in mean O3 concentrations due to emission changes in 2020
Meteorologisk Institutt met.no
1999 met 2003 met
5-7% changes due to envisaged reduction in emissions (2020)
Similar to meteorological variability ranges from 1999 – 2003
Meteorologisk Institutt met.no
Closing remarks (I)
• Model calculations vs. gravimetric PM2.5 over Europe show an with average 28% underestimation and correlations of 0.68 for n=17 stations – similar to other state-of-art models.
• Conclusions on model performance are at present hampered by the availability of measured PM2.5 chemical components and information on primary PM emissions.
• SOA theories are too immature for application within the EMEP policy framework.
• The EMEP model results should not be used in studies dependent of the analysis of absolute values of PM2.5 but …they are reasonable to study the effect of identified emission changes.
Meteorologisk Institutt met.no
Closing remarks (II)
• Changes in meteorological conditions introduce variability in the scenario analysis that are comparable to the expected variations in PM concentrations due to emission reductions in 2010. In 2020, expected changes due to emission reductions become more significant than the meteorological variations.
• For ozone, envisaged emission reductions both in 2010 and 2020 would impose concentration changes similar to those expected from meteorological variations.
• Calculation of source-receptor calculations for IAM needs to be carried out for as many different meteorological years as plausible : 2003 (on-going), 1999, 2000 …