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AIR QUALITY DATA
Definitions
Introduction
Urban Airshed Model
Evaluating
UAM Performance using Surface Air Quality Data
Example Graphical Displays
Statistical
Parameters for Model Performance Evaluation
Comparison
of UAM Results with Aloft Air Quality Data
Characterization
of Ozone Concentrations Aloft During SCAQS
Comparing
UAM Predictions and Aloft Air Quality
Result of Comparison
of Aloft Ozone and NOx Measurements with Model Predictions in SCAQS
Air Quality Regional
Boundaries
Summary
References
Lumped Carbon-Bond Species
Relationship Between
Individual Chemical Species and Lumped Carbon-Bond Species
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DEFINITIONS
CALMET = Diagnostic meteorological model
CALRAMS = Prognostic meteorological model
CBIV = Carbon bond IV chemical reaction mechanism scheme
NOx = NO + NO2 + poorly defined fraction of other
NOx species (given conventional analyzers)
NOy = NOx+ HNO3 + organic nitrates + inorganic
nitrates = NOx + NOz
NOz = Oxidation products of NOx = NOy
* (1 - NOx/NOy)
RHC = Reactive hydrocarbons
ROM = Regional oxidant model
UAM = Urban Airshed Model
IV = EPA Regulations version using CBIV; V = with variable grid
VOC = Volatile organic compounds
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INTRODUCTION
- Important to compare Urban Airshed Model (UAM) output
with ambient air quality data to assess model performance.
- Three broad types of ozone and precursor data useful for comparisons
to UAM output:
- Surface air quality
- Aloft air quality
- Boundary conditions
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URBAN
AIRSHED MODEL (UAM)
- The UAM is a 3-D grid model designed to calculate the concentrations
of both inert and chemically reactive pollutants by simulating physical
and chemical processes that take place in the atmosphere.
- The UAM uses a mass balance in which relevant emissions, transport,
chemical reaction, and removal processes are expressed in mathematical
terms.
- Simulations are usually 24- to 72-hour periods during which episodic
meteorological conditions persist.
- Typical UAM application:
- Select episode (usually widespread exceedance of ozone NAAQS,
typical meteorological conditions).
- Select modeling domain to encompass ozone monitors that reported exceedances
and all major source regions.
- Prepare model inputs using observed meteorological, emission, and air
quality data for an episode.
- Evaluate model performance.
- The UAM is used for analysis of spatially and/or temporally differentiated
future emission control strategies and their effect on air quality in various
parts of the modeling region.
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EXAMPLE
GRAPHICAL DISPLAYS
- Time series plots
- Compare observed and simulated pollutant concentrations for ozone,
NO, NO2 (or NOy) and selected VOC for all monitoring
sites within model domain.
- Compare observed ozone concentrations with the minimum and maximum
simulated concentrations within nine surrounding grid cells of a monitoring
site.
- Contour plots
- Show simulated pollutant concentrations and observed concentrations
for ozone, NO, NO2 (or NOy), and selected VOC for
each hour.
- Frequency distributions
- Of residuals (differences between hourly observed and predicted concentrations)
for ozone.
- Scatter plots
- Observed versus predicted hourly concentrations.
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Figure 1.

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Figure 2.

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Figure 3.

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Figure 4.

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Figure 5.

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Figure 6

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STATISTICAL
PARAMETERS FOR MODEL PERFORMANCE EVALUATION
|
EPA-Required Statistical Parameters
|
| Normalized accuracy of domainwide maximum 1-hr concentration
unpaired in space and time |
| Mean normalized bias of all predicted and observed concentration
pairs where the observed exceeds minimum concentrations |
| Mean normalized error of all predicted and observed concentration
pairs where the observed exceeds minimum concentrations |
| Observed domainwide maximum 1-hr concentration |
These definitions assume all observed peak concentrations
exceed the maximum concentrations.
|
Additional Statistical Parameters
|
| Absolute accuracy of domainwide maximum 1-hr concentrations
paired in space and time |
| Normalized accuracy of domainwide maximum 1-hr concentrations
paired in space and time |
| Absolute accuracy of domainwide maximum 1-hr concentrations
paired in space and unpaired in time |
| Normalized accuracy of domainwide maximum 1-hr concentrations
paired in space and unpaired in time |
| Absolute accuracy of domainwide maximum 1-hr concentrations
paired in time and unpaired in space |
| Normalized accuracy of domainwide maximum 1-hr concentrations
paired in time and unpaired in space |
| Absolute accuracy of domainwide maximum 1-hr concentrations
unpaired in space and time |
| Mean normalized bias of predicted and observed maximum
1-hr concentrations at all monitoring stations |
| Mean normalized error of predicted and observed maximum
1-hr concentrations at all monitoring stations |
| Mean absolute bias of predicted and observed maximum 1-hr
concentrations at all monitoring stations |
| Mean absolute error of predicted and observed maximum
1-hr concentrations at all monitoring stations |
| Mean absolute bias of predicted and observed pairs where
the observed exceeds minimum concentrations |
| Mean absolute error of predicted and observed pairs where
the observed exceeds minimum concentrations |
These definitions assume all observed peak concentrations
exceed the maximum concentrations.
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COMPARISON
OF UAM RESULTS WITH ALOFT AIR QUALITY DATA
Introduction
Knowledge of pollutant concentrations aloft is important for understanding
the evolution and sources of ozone concentrations measured at surface-based
monitoring sites.
The characteristics of aloft pollutant concentrations and the results
of comparisons between simulated and measured concentrations can provide
insights into ways to improve model representations of what is occurring
in the atmosphere and ways to improve model performance evaluations.
Analysis Approach
Characterize pollutant concentrations aloft (3-D analyses using aircraft
or other aloft air quality data).
Compare surface and aloft pollutant concentrations.
Compare aloft pollutant concentrations with model predictions.
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CHARACTERIZATION
OF OZONE CONCENTRATIONS ALOFT DURING SCAQS
High concentrations of ozone often exist in aloft layers.
Aloft ozone layers often mix down to the surface.
Aloft layers were generally horizontal in structure.
Mixed-layer average ozone concentrations were higher than surface concentrations.
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Figure 7

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Figure 8

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Figure 9

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COMPARING
UAM PREDICTIONS AND ALOFT AIR QUALITY
- Obtain UAM air quality output (all layers) for grid cells surrounding
air quality measurement location.
- Obtain gridded mixing heights for these cells.
- Bin aloft data to match UAM output layers.
- Plot comparisons.
- Investigate spatial and temporal variability of the UAM output.
- Review results with respect to meteorological conditions leading to
the ozone episode.
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Figure 10

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Figure 11

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Figure 12

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Figure 13

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Figure 14

Vertical profiles of NOx concentrations measured by aircraft
spiral compared to the UAM average for El Monte, June 25, 1987. The 15-m
vertical average aircraft NOx concentrations, 5-layer model
predictions, and model layer-averaged aircraft data are shown. The model
predictions were significantly lower aloft (particularly at about 500 to
100 m msl) and significantly higher in the surface layer all day. (Roberts
et al., 1993b)
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RESULTS
OF COMPARISON OF ALOFT OZONE AND NOx MEASUREMENTS WITH MODEL
PREDICTIONS IN SCAQS
- Model predictions of ozone below 200 m agl in the morning were ³
measured concentrations.
- Model predictions of ozone above about 200 m agl were typically about
50 to over 100 ppb lower than measured concentrations.
- Model predictions of NOx below about 400 m agl in the morning
were both higher and lower than measured concentrations.
- Model predictions of NOx above 400 m agl in the midday and
afternoon were typically lower than measured concentrations.
- Modeling recommendations included the need to properly represent significant
ozone concentrations aloft (esp. 500-1000 m), mixing of ozone layers to
the surface, horizontal pollutant structure aloft, and mixed-layer ozone
greater than surface ozone concentrations.
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AIR
QUALITY AT REGIONAL BOUNDARIES
- Surface air quality data not necessarily sufficient
- Regional models often underpredict ozone at upwind boundaries
- Important to look at precursors
- Definition of boundary
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Figure 15

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Average aloft (above 600 m msl) and surface NOx concentrations
along the 1991 LMOS southern boundary in the morning, midday, and evening
on July 18 (Roberts et al., 1994).
|
Sites
|
NOx Concentration (ppb)
|
|
Morning
|
Midday
|
Evening
|
| Surface |
|
|
|
| Streator |
5
|
3
|
2
|
| Kankakee |
9
|
5
|
13
|
| Jasper |
8
|
4
|
4
|
| Aloft |
2
|
4
|
4
|
Aloft and surface NMOC concentrations along the 1991 LMOS southern boundary
in the morning, midday, and evening on July 18 (Roberts et al., 1994).
|
Sites
|
NMOC Concentration (ppbC)
|
|
Morning
|
Midday
|
Evening
|
| Surface |
|
|
|
| Kankakee |
88
|
136
|
133
|
| Casper |
100
|
58
|
51
|
| Aloft |
|
|
|
| Streator (500 m) |
33
|
103
|
35
|
| Streator (1300 m) |
49
|
134
|
52
|
| Kankakee |
28
|
182
|
40
|
| Rochester |
36
|
241
|
|
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SUMMARY
- Comparisons should also be made with ozone and ozone precursors, including
NO, NOy, and speciated VOC.
- Comparisons at domain boundary are important.
| Analysis/Procedure |
Example Tool(s) |
| Process UAM output |
Programming |
| Compare surface ambient air quality
with UAM output |
Statistical packages, spreadsheets,
other data display |
| Examine aloft air quality |
Statistical packages, spreadsheets,
surfer |
| Compare UAM output and aloft air quality |
Spreadsheets, graphics |
| Investigate domain boundary conditions |
Statistical packages, spreadsheets,
other data display |
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COMPARISON OF URBAN
AIRSHED MODEL REFERENCES
Adamski W. (1997) An analysis of measured and predicted concentrations
aloft of ozone and total reactive oxides of nitrogen in the eastern U.S.
during July 1995. Draft report prepared by Wisconsin Department of Natural
Resources, Racine, WI, January.
California Air Resources Board (1995) Sacramento area modeling analysis
for the 1994 state implementation plan. Report prepared by Technical Support
Division, California Air Resources Board, Sacramento, CA, April.
Cassmassi J., Mitsutomi S., Bassett M., Lester J.C., and Zhang X. (1994)
Ozone modeling - performance evaluation. Draft technical report V-B prepared
by South Coast Air Quality Management District, Diamond Bar, CA, June.
Eisinger, D.S., Deakin E.A., Mahoney L.A., Morris R.E., and Ireson R.G.
(1990) Transportation control measures: state implementation plan guidance.
Revised final report prepared by Systems Applications International, San
Rafael, CA, SYSAPP-90/084, September.
Hanna S.R., Moore G.E., and Fernau M.E. (1996) Evaluation of photochemical
grid models (UAM-IV, UAM-V, and the ROM/UAM-IV couple) using data from
the Lake Michigan Ozone Study (LMOS). Atmos. Environ. 30,
3265-3279.
McNair L.A., Harley R.A., and Armistead G.R. (1996) Spatial inhomogeneity
in pollutant concentrations, and their implications for air quality model
evaluation. Atmos. Environ. 30, 4291-4301.
Roberts P.T. and Main H.H. (1992a) Characterization of three-dimensional
air quality during the SCAQS. In Southern California Air Quality Study
Data Analysis. Proceedings from SCAQS Data Analysis Conference, University
of California, Los Angeles, CA, July 21-23, Air & Waste Management
Association, Pittsburgh, PA, (STI-1223), VIP-26.
Roberts P.T., Main H.H., Lindsey C.G., and Korc M.E. (1993a) Ozone and
particulate matter case study analysis for the Southern California Air
Quality Study. Final report prepared for the California Air Resources Board,
Sacramento, CA by Sonoma Technology, Inc., Santa Rosa, CA, STI-90020-1222-FR,
May.
Roberts P.T., Main H.H., and Korc M.E. (1993b) Comparison of 3-D air
quality data with model sensitivity runs for the South Coast Air Basin.
Paper No. 93-WP-69B.05 presented at the Air & Waste Management Association
Regional Photochemical Measurement and Modeling Studies Conference, San
Diego, CA, November 8-12, (STI-1244).
Roberts P.T., Dye T.S., Korc M.E., and Main H.H. (1994) Air quality
data analysis for the 1991 Lake Michigan Ozone Study. Final report prepared
for Lake Michigan Air Directors Consortium, Des Plaines, IL by Sonoma Technology,
Inc., Santa Rosa, CA, STI-92022-1410-FR.
Stoeckenius T.E., Ligocki M.P., Shepard S.B., and Iwamiya R.K. (1994a)
Analysis of PAMS data: application to summer 1993 Houston and Baton Rouge
data. Draft report prepared by Systems Applications International, San
Rafael, CA, SYSAPP94-94/115d, November.
Systems Applications International, Sonoma Technology Inc., Earth Tech,
Alpine Geophysics, and A.T. Kearney (1995) Gulf of Mexico Air Quality Study.
Vol. I: summary of data analysis and modeling. Final report prepared for
U.S. Department of the Interior, Minerals Management Service, Gulf of Mexico
OCS Region, New Orleans, LA, OCS Study MMS-95-0038.
Tesche T.W., Georgopoulos P., Seinfeld J.H., Cass G., Lurmann F.W.,
and Roth P.M. (1990) Improvement of procedures for evaluating photochemical
models. Draft final report prepared for Research Division, California Air
Resources Board, Sacramento, CA by Radian Corporation, Sacramento, CA,
Contract No. A832-103, March.
U.S. Environmental Protection Agency (1991) Guideline for regulatory
application of the Urban Airshed Model (UAM). Report prepared by U.S. Environmental
Protection Agency, Research Triangle Park, NC, EPA 450/4-91-013.
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LUMPED
CARBON-BOND SPECIES
|
Carbon Number
|
MW
|
Carbon-bond Species
|
Comments
|
|
1
|
15
|
PAR |
Represents single-bonded carbon groups |
|
2
|
28
|
OLE |
Represents terminal double-bonded carbon groups |
|
2
|
28
|
ETH |
Represents ethylene |
|
7
|
92
|
TOL |
Represents toluene and other aromatics with
a single side chain |
|
8
|
106
|
XYL |
Represents xylene and other aromatics with
multiple side chains |
|
5
|
68
|
ISOP |
Represents isoprene |
|
2
|
30
|
FORM |
Represents primarily formaldehyde |
|
2
|
44
|
ALD2 |
Represents higher aldehydes and internal double-bonded
carbon groups |
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RELATIONSHIP BETWEEN INDIVIDUAL CHEMICAL SPECIES
REPORTED IN PAMS DATA SETS AND LUMPED CARBON-BOND SPECIES
| Carbon Number |
Carbon-bond Speciesa
|
Individual Chemical Species Splits
|
|
1
|
PAR
|
0.2´ethan + 0.5´acety + 0.5´propa
+ nbuta + isbta + ispna + npnta + cypna + nhexa + 23dmb + 0.83´22dmb
+ 2mpna + 3mpna + cyhxa + mcpna + nhept + 2mhxa + 3mhxa + 24dmp + mcyhx
+ noct + 2mhep + 3mhep + 0.875´224tmp + 234tmp + nnon + ndec + nundec
+ 0.33´prpyl +0.5´1bute + 0.6´(1pnte + 3m1be + 2m2be
+ cypne) + 0.2´(c2pne + t2pne) + 0.17´benz + 0.125´ebenz
+ 0.22´(ispbz + npbz) + 0.11´(124tmb + 135tmb) + 0.33´(c2hex
+ t2hex) + 0.83´2m1pe + 0.67´4m1pe |
|
2
|
OLE
|
0.67´prpyl + 0.5´1bute + 0.4´(1pnte
+ 3m1be) + 0.33´4m1pe + 0.125´styr |
|
2
|
ETH
|
ethyl |
|
7
|
TOL
|
tolu + 0.875´(styr + ebenz) + 0.78´(npbz
+ ispbz) |
|
8
|
XYL
|
pxyl + m/pxyl + pxyl + 0.89´(124tmb
+ 135tmb) |
|
5
|
ISOP
|
Ispre |
a The relationships between FORM and ALD2 and individual chemical
species are not indicated because ambient data for important components
of those lumped species are not available.
Source: Stoeckenius et al., 1994a
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