EPV600/9-89/058
                             PROCEEDINGS             March 1989

                           US/FRG WORKSHOP

                                  ON

             PHOTOCHEMICAL OZONE PROBLEM AND ITS CONTROL.

              US EXPERIENCES AND THE SITUATION IN EUROPE
                            May 4-6, 1988
                            Senats-Hotel
                            Cologne, FRG
                         WORKSHOP CO-CHAIRMEN
B. Dimitriades, US Environmental            D.  Jost,  Unweltbundesampt,  FRG
                Protection Agency
                          STEERING COMMITTEE
                       K. Becker,  FRG,  Chairman
                          K.  Demerjian,  USA
                           H. Jeffries,  USA
                           U. Schurath,  FRG
                              Edited by

                          Basil Dimitriades
       Atmospheric Research and Exposure Assessment Laboratory
                  Research Triangle Park, NC  27711
                                 USA

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                                 DISCLAIMER
Although the workshop  described in  this .report has been  funded partially
by the  U.  S. Environmental  Protection Agency  under contracts  to invited
participants, the  report has not been subjected to the Agency's  required
peer and policy review and therefore does not necessarily reflect the views
of the Agency and  no official endorsement should be  inferred.   Mention of
trade names  or  commercial  products  does not   constitute  endorsement  or
recorranendation for use.        .
                          Printed in March 1989

                                  by the

                    US Environmental Protection Agency

                    Research Triangle  Park,  NC  27711

                                   USA

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                                 PREFACE



     This Workshop was held within the framework of cooperation under the



IB-German Environmental  Agreanent.   It  contributes  to  high  priority



activities identified by Minister Toepfer and Administrator Thomas during



their December 1987 meeting.

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                            TABLE OF CONTENTS






                                                                     Page



Conference Agenda	  vi



Acknowledgment.	  ix



Proceedings Report



     1.0  Introduction	   1



     2.0  Magnitude and Trends of Ozone Problem	   4



     3.0  Emissions	   9



     4.0  Chemical and Meteorological Processes	  14



     5.0  Modeling Technology and Applications	  23



     6.0  Scientific Issues Associated with 03 Control Strategies...  25



     7.0  Conclusions and Recommendations	  27



     8.0  References	  30



List of Participants	  33

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                                    WORKSHOP
                THE PHOTOCHEMICAL OZONE PROBLEM AND ITS CONTROL
Senats-Hotel
Unter Goldschmied 9-17
Cologne, West Germany
            May 4-6,  1988
                                  AGENDA
Wednesday, May 4, 1988, 9:00 AM - 6:00 PM

SESSION I:   MAGNITUDE OF OZONE PROBLEM.
             TRENDS                                  Chairman:

             - Ozone and Precursor Emission Trends
               in the US

             - Concentrations of Ozone and Precursors
               in Germany

             - Ozone in Western Europe

             - Background Ozone.  Levels, Trends,
               and Origins

             - Ozone Trends Within Large Metropolitan
               Areas.  The Los Angeles Basin
           D. Jost, FRG

           T. Curran,  USA


           W. Fricke,  FRG


           K.  Nodop,  FRG

           K. Deraerjian,  USA


           T. McGuire, USA
                                   LUNCH

SESSION II:  ON-GOING CONTROL POLICIES

             - Ozone Control in Germany

             - Ozone Control Policy in the U.S.
             - Assessment of Effectiveness of
               Control as an Ozone Control Strategy

             - On the Effectiveness of the U3EPA
               Control Strategy for Ozone.  An
               Opposing Viewpoint
Chairman:  B. Dimitriades,  USA

           E. Weber, FRG

           E. Meyer, USA

           W. Sylte, USA


           H. Walker, USA
                                       VI

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 SESSION III;
SESSION IV:
 ESTIMATES OF EMISSION DATA
 FOR VOC AND NOX

 - Problems with Existing Emission
   Inventory Data Bases

                      BREAK

 - Auto Emission Estimates.   Current
   Improvements

 - European Inventory of Ozone  Precursor
   Emissions

 CHEMISTRY OF TROPOSPHERIC
 OZONE  FORMATION

 - Recent Developments in 03 Mechanism
   and  Existing  Issues

 - The  Chemistry of Ozone Formation
   Tested by Atmospheric OH Measurements

 - The  Present Knowledge of Kinetic Data
   Important for Ozone Chemistry
Chairman:
                                                                H. Jeffries, USA


                                                                K. Schere, USA
           F. Black, USA


           C. Veldt, NL


Chairman:  K. Becker, FRG


           H. Jeffries,  USA


           U. Platt, FRG


           A. Kerr,  UK
     7:00 PM  Dinner hosted by Workshop Organizers

Thursday. May 5, 1988, 9:00 AM - 5:00 'PM

SESSION V:    TRANSPORT/DISPERSION OF
              OZONE AND PRECURSORS

              - Transport of Ozone by Airborne
                Measurements

              - Model Prediction of Transport
                and Dispersion
                                       Chairman:  K. Demerjian, USA
                                                  D. Paffrath, FRG
SESSION VI:
- USEPA's Regional Ozone Model

MODELING RESULTS ON OZONE              Chairman-
FORMATION FROM PRECURSORS
UNDER DIFFERENT CONDITIONS

- Effectiveness of Alternative Urban/
  Regional Control Strategies for Ozone

- Assessment of Ozone-Related Controls
  in California Urban Areas
          J. Pankrath/
          I. Jacobsen, FRG

          K. Schere, USA

          H. Jeffries, USA
                                                               E. Meyer/
                                                               J. Tikvart, USA

                                                               T. McGuire, USA
                                      vii

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              - Results from Modeling of Ozone Formation        R.  Stern,  FRG
                in Germany and Neighboring Countries

                                   LUNCH

SESSION VII:  VALIDATION OF MODEL                    Chairman:   U.  Schurath,  FRG
              PREDICTIONS.  SENSITIVITY
              TO INPUT DATA/PARAMETERS

              - Sensitivity Analysis of EKMA Input              H.  Jeffries,  USA
                Parameters on VOC Control Require-
                ments

              - Evaluation of USEPA Regional Oxidant            K.  Schere, USA
                Model in the North East US

              - Sensitivity Analysis of Model Predictions       R.  G.  Derwent, UK
                Upon Chemical Input Data

                                   BREAK

              - Evaluation of Urban Airshed Models              S.  T.  Rao, USA
                with Recent Field Measurements in NY

              - Effects of Different Wind Field                 R.  Kessler, USA
                Analyses on Airshed Model Predictions


     5:00 PM  Visit to Bayer Plant and hosted dinner

Friday, May 6, 1988, 9;00 AM - 5:00 PM                ,

SESSION VIII: SO^IARY/CONCLUSIONS                  "  Chairman:   K.  Becker, FRG
                                                     Co-Chairman:   H.  Jeffries,  USA

              - Discussions.  End of Workshop.

                                   LUNCH

              - Steering Committee Meeting           Chairman:   K.  Becker, FRG


Saturday, May 7, 1988. 9:00 AM - As Needed      •          .

              - Steering Committee Meeting           Chairman:   K.  Becker, FRG
                                      Vlll

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                             Acknowledgement
     The Workshop was organized at the instigation of Drs. Gary Foley (USA)
and Erich  Weber  (FRG).   The Workshop program  and  agenda  were developed
by Drs.  Dimitriades and  Becker.  Workshop arrangements  were made  under
Dr. Becker's direction.  The Workshop  report was prepared based on meeting
presentations and  on  followup  discussions  by  all  Workshop  participants
under the  guidance of the Workshop Steering Committee.   Drs.  Dimitriades,
Demerjian, Curran, Derwent, Nodop, Fricke, KLey, Liibkert, Schere, Jeffries,
Kerr, Kessler,  Stern,  Meyer, Walker,  Sylte and McGuire  prepared  summary
statements which were  edited by Dr. Dimitriades  into  a  structured report.
The report was  reviewed and finalized by the  Steering  Committee.  Ms.  K.
Curtis and Ms.  C.  Morawa provided secretarial  assistance for  organization
of the Workshop and preparation of the Proceedings  report.  The contribu-
tions of these named individuals and of all other Workshop participants are
acknowledged with gratitude by the Workshop organizers.
                                   IX

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               PHOTOCHEMICAL OZONE PROBLEM AND  ITS CONTROL.
                US EXPERIENCES AND THE SITUATION IN EUROPE


1 .0  INTRODUCTION

     The understanding  of  the  significance  of  ozone  occurrence  in the
troposphere can  be  viewed from .three  distinct  points  of  view.   First,
ozone plays  an important role  in controlling the chemical  composition of
the troposphere  as  a result  of being  a major  source  of  hydroxyl   (HO)
radicals.  Second,  ozone  is  a  radiatively active  gas which impacts the
energy budget  of the troposphere so as  to  cause global  warming ("green-
house effect").  And third,  ozone has been found  to cause adverse effects
on human health,  vegetation and materials 1.   Thus,  ozone alone and  with
other pollutants  synergistically irritate  the  respiratory  system  causing
reduction in pulmonary  function  and  increase  susceptibility to infections
and asthma attacks.   Also,  it reduces crop yields and growth and lifetime
of trees,  and  damages rubber, paint,  and other materials^.   And finally,
ozone and  other oxidants  have  been  found to  instigate the  formation of
acid rain and  the  production in  air  of  toxic pollutants  such as formalde-
hyde and other mutagens.

     There has been significant  debate  as  to the quantitative details of
the sources  of ozone in the  relatively clean  free  troposphere, but, in
general, it  is widely accepted that the major sources are the stratosphere
and photochemical reactions of methane, carbon monoxide and nitrogen oxides
(NOx) (Figure 1-1).   In the polluted  tropospheres, however, that is,  within
the 1-2-Rn boundary  layer adjacent to the surface,  ozone and other oxidant
species are being formed mainly from photochemical reactions of non-methane
volatile organics  (NMVOC or  in short VOC with  respect to ozone formation,
including also CO)   and  NOX emissions  associated  with manmade activities
(Figure 1-1).  It is primarily this latter photochemical ozone arising from
polluted atmospheres  that  is  of  interest and  the  subject of this  report.

     The photochemical  ozone  phenomenon  has  been  studied extensively in
the US  and  to  some  extent in Europe,  Japan,  Canada, and  Australia also.
These studies yielded a reasonably good—but not necessarily sufficient—
understanding of the chemistry and meteorology underlying the photochemical
ozone formation process  and  led  to development of  models capable of pre-
dicting photochanical ozone formation in time  and  space.   In the US,  where
the photochemical  ozone problem  is  most  severe,  laws  have been  enacted
since 1970 that  required the  Federal and State Governments  to promulgate
emission control  regulations  sufficiently  stringent  to  reduce  ambient
ozone concentrations down to the national ambient ozone air quality standard
of 0.12 ppm (1-hour concentration not to be exceeded more than 1 day/year).
Progressively more stringent emission and "equipment design" standards were
promulgated during the 1970's  and 1980's, which were intended to bring about
reductions in emission levels that would more than offset the increases due
to growth.  Thus, VOC emissions were estimated to have decreased 19% during
the 1977-86 period and  NOX emissions 8%.  The  improvement associated  with
automobile emissions  was 39%  for VOC and 13%  for  NOX during that  period
and it occurred  despite a 24% increase in vehicle  kilometers  of  travel.

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                               1-A
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 CO
 "O


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 CO
      O3 dry deposition
Sources
                           Stratosphere-

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                          NOx ?
                              Figure 1-1

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Despite  such  supposed emission reductions, however,  and contrary to model
predictions,  the photochemical ozone problem in the US is still  severe and
very much  of  concern.   While  peak ozone  concentrations,  generally,  have
been reduced,  there  are still more than 60  "non-attainment" urban areas in
the US,  with  some 75 million of people exposed to ambient ozone  concentra-
tions  that  exceed the  air quality standard  by as much as 0.23 ppm.   The
reasons  for such persistence and pervasiveness of the ozone problem are not
well understood.

     This apparently inexplicable  and disappointingly small success of the
ozone  control  programs  in the IB  raised some questions on the sufficiency
of the current understanding  of the ozone problem.  Critics  have gone as
far as to allege that the  US ozone control policies are grossly misdirected
in being centered around unilateral control of the VOC precursor.  However,
a balanced view of the control program experience  in the US would be  that
progress has  been made but that  more  needs to be done.   Initial control
efforts  emphasized VOC reductions  but in some situations models may be  used
to evaluate  the effectiveness  of  additional NOx  controls particularly  in
terms  of the possible effect on population exposure.  There is an awareness
in the US that most  of the large  stationary  sources are already  controlled
and that future controls  on smaller sources  will be expensive.   For mobile
sources, the  USEPA has proposed onboard equipment  on all new vehicles  to
control  VOC emissions  during refueling.  Other  possibilities  being looked
at include  fuel volatility,  stricter inspection and maintenance require-
ments, and  the possible   use  of  alternative fuels.   Experience to  date
suggests that  future reductions will  be difficult and  there  are definite
concerns about what  an area such as Los Angeles would have to do to attain
the US ozone standard.

     Given the large socioeconoraic penalties incurred by the ozone-related
controls, the  above  uncertainties  and doubts were disturbing and led USEPA
to undertake an effort to  re-examine and revise its ozone control policies.
It is in this spirit of self-assessment that the USEPA agreed to participate
in this Workshop and committed itself to present and discuss the US experi-
ences and to expose its ozone control thinking and policies to the judgment
of the international scientific community.

     On  its part,  the  FRG Government  is  concerned  that  the effects of
photochemical  ozone  on human health and on  the  country's forest resources
have grown  in  severity  to the point  that  serious  consideration must be
given to commencing  a control effort.  The  FRG Government is also  keenly
interested in  assessing  problems   associated  with  the transport  of  ozone-
related  pollutants from or to neighboring  countries.  In the face  of the
questions raised by the US experience, however,  and  of  the costs and poli-
tical complications  associated with  even modest  control measures,  it is
imperative that any control initiatives to be undertaken by the FRG (or the
neighboring countries)  be designed  with  the utmost  care and  confidence.
The accuracy and completeness, therefore, of existing pertinent  scientific
evidence are  the  main  subjects of interest  to Germany  and  the  primary
reason for the German involvement  in this Workshop.

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     The two  co-organizer countries agreed  to pursue these  objectives by
convening a group  of experts both from within  and outside the two Govern-
ments .. The  experts  were  selected  among  those  with  internationally or
nationally recognized expertise and so as to achieve a balanced representa-
tion of existing viewpoints and diverse experiences.  A list of all Workshop
participants and  their  affiliations  is  attached  here  as  an  appendix.
Because of the substantial commitments in time and effort required of than,
the non-Government experts were offered monetary compensations.

     The organizers  agreed,  further,  on  a Workshop  format  that was to
dedicate 2  full days  to pre-prepared  presentations and  followup discus-
sions, one-half  day  to  a  plenary discussion,  and the last full  day to
Steering Committee discussions (see attached Workshop Agenda).  The Workshop
Steering Committee,  composed  of  four non-Government  participants,  guided
the Workshop discussion  so  as to  adhere to the Workshop objectives and, at
the end, digested all information presented at the Workshop and reported it
in terms  of relevant  conclusion  statements  and  recommendations included
here.

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 2.0  MAGNITUDE AND TRENDS OF OZONE PROBLEM

 2.1  Ozone Problem in Europe

      The general features of  the  ozone distribution throughout Europe have
 slowly emerged  over the  last  15  years  since  ground level  measurements
 commenced.  Elevated hourly ozone  concentrations  over  60  ppb have  been
 observed at some time during almost every year at every site.  The frequency
 of occurrences of higher hourly concentrations falls off so that 120 ppb is
 exceeded only during certain  years and  at  certain  sites.   The  extreme
 hourly ozone  concentrations  reported  for  each  country   cover  the  range
 100-300 ppb.  Meteorological  conditions conducive  to photochemical  ozone
 episodes are those  within high pressure systems  during  summer with  clear
 skies and low windspeed.  The  vertical  mixing is then inhibited and precur-
 sors and oxidants can accumulate.   In urban areas averaged ozone concentra-
 tions are generally lower compared to adjacent  rural (downwind)  areas most
 likely due to chemical  destruction  of ozone  by emitted  NO.   Quantitative
 identification of trends is complicated by the  short  observational record,
 year-to-year variability  in the  weather,   changes   in measurement method
 and calibration techniques  and  changes in  emission patterns.   Sub-micron
 particles can serve as an  indicator  of large-scale  anthropogenic pollution
 as well as PAN.   PAN is,  in addition, an excellent indicator of high photo-
 chemical activity.   Ozone and  PAN show a  similar  behavior both  in  their
 seasonal cycle and  diurnal variation^.

      In the Federal  Republic  of Germany, there were 156  ozone monitoring
 stations operating  during 1987.   Most of them are situated in  urban areas.
 The measurements are based on  chemiluminescenee and  UV absorption  tech-
 niques.   Ozone data up  to 1983 have been  published in a review  report3.
 Table 2-1  shows ozone  concentrations form  1976 to  1986  at some  selected
 sites across the Federal .Republic of Germany.   These measurements  indicate
 the average annual  ozone concentration  to  increase  with altitude and with
 distance from urban areas, presumably due to  dry deposition at the ground
 and the  influence of NO  emission.  Typical  annual averages ranged between
 20 and 80 (ig/nP (10  and 40  ppb).   The records  also show  both a  seasonal
 and diurnal cycle.  The seasonal cycle has a  minimum  in winter and a maximum
 in summer.    In  general,  the  annual  amplitude decreases  with  altitude.
Maximum  ozone concentrations are highest at low altitudes close to certain
 industrialized and urban areas.  They occur  during episodes  in  summer, when
high pressure systems over  Central  or Northern Europe are accompanied by
 easterly flow from  the  continent and  high temperatures.   Vertical ozone
profiles  taken by airplane under these conditions show that ozone concen-
 trations  in excess of those  found in the middle  troposphere are abundant in
 the mixing  layer all over the  warm  part of such  high  pressure systems.
The  spatial extent  of these elevated ozone  concentrations  is  of the order
of a million square  kilometers.  On this  regional  scale  200 jig/m3 (0.10
ppm)  appears  to  be die  upper  limit  for ozone within the  mixing  layer as
shown in  Figure  2-P.   Higher  concentrations  are  due to  local  sources.
The highest ozone concentration ever observed near  the surface in Germany
is 664 pg/nP  or  0.34 ppm (30 min. average)  on  June 23,  1976,  in Mannheim
 (Upper Rhine  Valley)J.    Due  to different  meteorological  conditions  from
year  to  year  the frequencies  of exceeding  certain ozone  concentration

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Figure 2-2.  Concentration profiles of ozone, NO,  NCv, and olefins
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            attributed to the plumes of large lignite-burning power
            stations (K power station, P petrochemical plant)

-------
     The ozone air quality data given here for the US were taken from pre-
viously published reports^ and were selected so as to provide two different
measures of the ozone problem in the US:  one in terms of peak ozone concen-
trations and  one in  terms  of  frequency  of violations  of the  ozone air
quality standard.   Figure 2-3  shows  levels  of second maximum  daily 1-hr
concentrations in  a variety  of  attainment (of  ozone standard) and non-
attainment urban  areas  in  the  US.   Figure 2-4  shows exceedances  of the
ozone standard  at the  non-attainment urban areas.   The two  figures show
that the most severe ozone problems in the US  occur in urban areas within
California, the  Northeast  States  and the Gulf  Coast  area.   The  ozone
standard was  exceeded  in some  urban areas  within  California  during the
1983-86 period  up to  140 days  and peak ozone  concentrations  observed in
some urban  areas of  California  in 1985  were  as  high as  and even higher
than 0.35 ppm.  Figures 2-5 and 2-6 show ozone  data  averaged over 242 urban
locations, depicting  trends during the 1977-1986 period.  The data reflect
a significant decrease  of  ozone  concentrations  with time,  but there are
two apparent  "anomalies":  the  strong deviation of the  1983  concentration
from the  pattern  and  the  rather abrupt  ozone  decrease from  1977-78 to
subsequent years.   A  detailed  examination of  ozone trends for  individual
urban areas  showed the year 1983 to be consistently associated with higher
ozone concentrations,  suggesting that the 1983 "anomaly" can  be attributed
to meteorological conditions being more  conducive to ozone formation  than
those in the  adjacent years.  The sharp ozone  decrease  from  1977-78  to the
subsequent years has been found  to be partly due to a change of the  cali-
bration method used   for ozone  measurement.   After adjustment for  this
artifact, however,  the data  still showed  a significant  downward trend for
the ozone concentration during the 1977-86 period.

2.3 Background Ozone

     Ozone occurring in  atmospheres not directly impacted  by anthropogenic
emissions is  referred  to as background  ozone.  Levels  of such ozone are
dependent upon:  (1)  the state  of the  stratospheric ozone  reservoir and
 its exchange rate; (2)  the  chemical  precursor content of  the troposphere;
 (3) actinic photon fluxes;  (4)  the nature of  the surface  exposed;  and (5)
horizontal transport.  These important,  but not all  inclusive  parameters,
would suggest that background  ozone  levels should  show temporal/seasonal,
 latitudinal and altitudinal  dependence as well as dependence with  regard
 to a marine  versus  a continental environment.  Some  data  relevant  to this
 suggestion are given in Table 2-2. With the qualifying dependencies, ozone
 background concentrations range typically from 20 to 40 ppb in rural/remote
 regions.  Figure 2-1 shows that in free troposphere (June 26, 1976,  Cologne
 area)  the ozone  concentration  is about 50 ppb.  Figure  2-7  which  presents
 the frequency  distribution  of the  ozone concentration as   1-hour  values
 averaged over  the period  1977-81 at different  sites  in South  Germany,
 indicates that  35  to 40 ppb seems to be a typical ozone  concentration  in
 the unperturbed troposphere.

      The typical  vertical distributions  of  ozone  in  the  troposphere  at
 remote sites are presented in Figure  2-8,,   Trends in background ozone levels
 reported at  NOAA/GMCC baseline stations,  Figure 2-9, indicate increases at
 sites in the Northern  Hemisphere while  sites in  the  Southern Hemisphere

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 show the  ozone  concentrations to decrease  with  time.   Interpretation of
 these trends,  however,  is somewhat  speculative,  given the various  factors
 affecting ozone  concentrations  in  the troposphere.   Additional evidence
 of  increasing  ozone  trends in continental  environments  include the observa-
 tions at Arkona  (GDR) and Hohenpeissenberg (FRG) and  the historical  account
 constructed  for  Montsouris,   France  (Figures  2-10 and  2-11).  At  Arkona,
 ozone increases  between  1%  and  3%  or  by 0.37 ppb per year,, if a linear
 regression analysis  is made.   This station, which  is  continuously reporting
 since 1956,  has  the longest  record of  recent times.   Somewhat shorter,
 starting in  1971,  is the Hohenpeissenberg record  where an annual increase
 of  0.41 ppb  is observed.  Although,  as  seen in Figure 2-10, the  two German
 stations show  somewhat different  absolute levels  of ozone  over the  time
 that they  can  be compared,  the  trends  in units of ppb per year are quite
 comparable.

      Crutzen5  and  KLey and  Volz6  have  arrived at the  conclusion that the
 current trend  of ozone in western Europe began about  1940.  Compared to the
Montsouris series (Figure 2-11), which  was obtained  from 1876 to 1905 near
 Paris, background ozone  concentrations  in Europe have increased  since  then
 considerably7»8.  An upward  trend  of  the  ozone  concentration has  been
 observed in  the  free troposphere and the  upper part  of the boundary layer
 between 1967 and 1982  over   South Germany at Hohenpeissenberg  (Figure 2-
 12)9.  Measurements  from  East Germany10 support the ozone increase near the
 surface between  the mid-1950's  and 1984;  however,  they  do  not  show a
 significant  ozone increase within the  free  troposphere at  5.5 Rn altitude
 in  the monitoring period 1975-84.   Model  calculations11  suggest that this
 ozone increase can  be   attributed  to  the   increase  of  NOX  emissions.

      An increase  of background ozone might  be occurring in most parts of
 the Northern Hemisphere.  Monitoring data  suggest  that  increases  are occur-
 ring, for  example,   at  Barrow, Alaska  and Mauna  Loa,  Hawaii  (see  Figure
 2-9).  The latter station, situated  at  an altitude of  3000 m, samples air
 that  is characteristic  of the free  troposphere.   Therefore,  two stations,
apart by nearly 180° of longitude experience a similar phenomenon.

      It is extremely important for  the assessment of the  role of ozone
 transport to know the,, latitudinal dependence  of this molecule between the\
North American and   European  Continents.   No trends  of  ozone  have  been
 reported over  the Atlantic Ocean.  The meridional  cross section of  surface
ozone is reproduced  in Figure 2-13.   It was  obtained mostly  along the 30°
meridian.  The simultaneously measured -vertical  ozone profiles are  also
reported in  Figure 2-13.  They show that, north of 20° northern latitude,
 there was hardly any vertical gradient of ozone in  the lower troposphere so
that  the surface  values  are  representative  for the  lower  troposphere.   A
comparison of  Figure 2-13 with  the  values measured  at Hawaii (20°N)  and
Boulder (40°N),  respectively  (see  Table  2-2),  shows  good   agreement  at
corresponding  latitudes.  Figure  2-13  represents  the best information on
the large scale features of surface ozone between the American and European
continent.   It is not  possible,  at present,  to   specify  the  surplus  of
background ozone in  the Northern  over the Southern Hemisphere in terms of
anthropogenic  causes versus natural  ones,  i.e. a higher flux  of ozone from

-------
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1965
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1985     1990
Figure 2-10.   Ozone Trends in Hohenpeisseriberg (FRG)  and Arkona (GDR)

-------
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1950
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Figure 2-11.
     Near surface ozone concentrations (annual means)
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     Arkona, German Democratic Republic 1956-1984.

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                                     10

research groups  or  within  other  international bodies)  established  the
OEGD/CEC inventory as the most complete  and  accurate one currently available
for Western Europe.  Nevertheless, concrete  estimates of overall reliability
and completeness  are still  lacking.   For  some  individual  source  sectors
uncertainty calculations have  been carried'out.   For vehicular ^ NOX emis-
sions, for example, Eggleston and  Mclnnes^  calculated an uncertainty of 40%
which compared well  witi^ uncertainties  measured in UK of  15% for S02, 45%
for NOX and 80% for VOC1'.

3.2    Emissions  in  the US

3.2.1  Anthropogenic Emissions in the US

     Emission inventories used in the modeling of ozone concentrations must
include the major precursor species,  NOX, hydrocarbons and  CO.   In the US
major efforts have gone  into producing  nationwide emission inventories for
the base years of 1980 and most recently, 1985.  The inventory is constructed
by assimilating annual  emissions  from major point sources provided by the
individual states with estimates of area source emissions generally made by
the USEPA using surrogate activity-level indicators for the emissions, such
as statistics on VMT (vehicle miles traveled), population, housing, employ-
ment, etc.  The level at  which the area source emissions are estimated are
annual totals  by  county  within  each state.  The  emissions must  then be
"disaggregated" to  produce hourly  gridded   emissions  for  use  by  the air
quality models.   Spatial, temporal and species  allocation factors must be
applied to  the annual point and area  source emissions to  accomplish the
disaggregation.   Considerable  uncertainty is introduced into the emissions
estimates by the  disaggregation process (see later discussion of uncertain-
ties) .

     The inventories are  constructed such that total mass emissions are
estimated for  certain "classes"  of emissions.   For  example, exhaust  emis-
sions from  light-duty  vehicles  (most  automobiles)  might  be  one class,
architectural surface coatings would be another, domestic  solvents another,
etc.  Classes  exist for every major industrial, commercial and residential
point or  area source emissions  class.  This is  the  Source Classification
Code  (SCC)  system,  an  important  building  block in the emission inventory
process.  A  profile of  individual compounds with their  associated weight
percentages exists for each SCC  code.   In the disaggregation process the
individual organic  species  are  "lumped" together  into similarly-reacting
groups of compounds, such as olefins, paraffins, etc., in  order to minimize
the  total  nvmber  of species carried in  the final  gridded inventory.  The
particular groupings of  organics are  somewhat dependent  on the  chemical
kinetic reaction  scheme used by the air quality model.

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-------
                                      11

                                  Table 3-4.
     1980 Continental US  Emissions  (NAPAP-Version  4.0)  by  Source Category
                            (1,000,000 tons/year)
                                                                 VOC
Electric Utilities
Industrial Combustion
Residential/Commerical Combustion
Non-ferrous Smelters
Other Industrial Processes
Transportation
Miscellaneous
17.3
3.7
0.9
1.2
3.0
0.9
0.1
8.1
4.5
0.7

1.0
9.1
0.3
0.1
1.0
0.1

4.5
8.0
9.6
        Total                                  27.1      23.7    23.3


      Tables 3-4 and 3-5 present a  summary of total anthropogenic emissions
 from the continental US and Canada from the NAPAP-Version 4.0 and 5.0 (final)
 emissions  inventory for 1980.

 3.2.2  Biogenic VOC Emissions  in the US

      Biogenic  emissions of  organic  species  have  been estimated  for  the
 US  in several  recent  studies.   Regional modeling tests  show that  these
 compounds  contribute  to the total reactivity of the lower  troposphere when
 sufficient NOX is  present.   Emission factors for isoprene  and monoterpenes
 have been  estimated for many tree,  crop  and  grass  species in the  US.   The
 total mass of  individual species have been estimated from land-use  invento-
 ries satellite imagery.  Although estimates of biogenic emissions are still
 in  crude stages, the  total mass of biogenic  organics  (29,000 tons/day) is
 of  the  same order of magnitude as the anthropogenic organics in the North-
 east US  where  there are large contributions from  the  anthropogenic side.
 In  the  Northeast US,  the total biogenic hydrocarbon is estimated to be 41%
monoterpene, 18% isoprene, and 42% unidentified organics.

 3.2.3  Emissions Uncertainties in the US

     Estimates of  uncertainty  in  the  1980  US  inventory  have  been  made
subjectively by  a  panel of  experts  in  the  development   of inventories.
Table 3-6  shows  these estimates for some  of  the principal  component steps
in the  inventory developent process  for both anthropogenic and biogenic
emissions.  The  uncertainties  in VOC  are generally greater  than those in
either NOX  or  CO,  and the  species and temporal allocation processes intro-
duce the greatest components of uncertainty in the emissions disaggregation.
For  the biogenics (Table 3-7),  the temperature-dependence of the monoterpene
emissions is a very uncertain  factor.  The estimated composite error Table
3-8) in the hourly gridded emissions varies from 109% for the bioeenic VOCs
to 33% for NO-sr.     .

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                11-D
              Table 3.8


     UNCERTAINTY  ESTIMATES
(Composite From All Sources of Uncertainty)

        1980 ROM Grid-level
          Hourly Emissions

                        Percent Error
              _CP_°JQl &. Ar?9l_ .(Area _0n !y)
 Speciated VOC
 (Anthropogenic)

 Speciated VOC      _          ino
  (Biogenic)                    1U9

 Speciated NOV     32          33
            /\

     CO           49          54

-------
                                     12

     It is generally accepted that the anthropogenic VOC inventory has been
underestimated.  Indications of this come from a number of areas, including
the disparities  in  the. VOC/NOx ratios in the  emission inventories  and 6-9
am ambient data  (see  next section), and  the exclusion of  some  known VOC-
eraitting source  types,  including hazardous  waste  treatment  facilities.
The 1985  US   inventory effort has made  great  strides in  correcting many
of the known  deficiencies in the process of building  an inventory.  Among
the improvements  are  the development  of  methodologies for missing source
types, temperature-dependence of evaporative emissions from mobile sources,
updating and  improvement of temporal and  speciation  allocation factors,
formalized and rigorous quality assurance procedures,  and  a high level of
coordination with state and local pollution agencies involved with assimi-
lating data for  the inventories.

3.2.4  Ambient VOC/NOx and VOC Composition  in  IB

     In 1984  the USEPA  started  an urban VOC  data collection program that
continued through 1988.  In this program,  local  agencies  collected 6-9 am
integrated ambient  air samples  using SUMMA polished stainless steel canis-
ters.  These  were shipped  overnight to  an EPA laboratory  where they were
analyzed by  three different groups.  In addition to using the cryogenic
preconcentration direct  flame  ionization  detection  method  (PDFID)10,  a
large number  of  the canisters  (ca. 900) were selected  for detail  speciation
using gas  chroraatography19'20.   The  program  involved extensive  quality
assurance procedures  and the  results demonstrate  excellent precision and
accuracy:  on repeat  analysis of 155  samples  the precision for  total non-
methane organic  compound concentrations  (NMQC)  was  0.49%  and on   fully
duplicate samples  (i.e.  two canisters were collected) the precision was
1.69%.  Two  different  laboratories  had  an  absolute agreement  of 8.9% and
the sum-of-species  from the gas chromatographic method was  2.4%  lower than
the principal laboratory total VOC from the PDFID method.  The mean  6-9 am
NMOC concentration  over 22  cities was 0.756 ppmC.

     These NMDC  ambient  data have  been used  in  a number  of EPA  studies.
One study computed the median  ambient urban NMOC/NOx  concentration  ratios
for several  US cities.   These  results are  shown in Table  3-9.   The median
NMOC  to  NOx  ratio was 13.9 ppmC/ppm.   Table 3-10  shows NmC/NOx  ratios
computed from the NAPAP 4.2 Emissions Inventory  for a number of  US cities.
The median  value was 3.9 ppmC/ppm.   It is  this type of  discrepancy that
strongly suggests that many NMOC  sources may be missing in the  current US
inventories.

      The gas chromatographic analysis of hydrocarbons  in  772  canisters has
been  used for  the purpose  of producing  chemical mechanism  speciation,
 especially for use in the  OZIPM/EKMA method21.  As part of this analysis,
 the 20 species with the highest concentration  in  each canister were analyzed
 for frequency of  appearance.   Table 3-11   lists the  100  most  frequently
occurring compounds.    Toluene  appeared  in  the   20  highest  concentration
 species  in every canister.   The 15th most prevalent species (1,2,4-trimethyl
benzene)  appeared in the 20 highest concentration species  in 75% of all the

-------
                                    12-A
                Table 3-9.   Median Ambient Urban* MOC-to-NOx
                            Concentration Ratios During 1984


 EPA Region                       Site                 Ratio (No.  of data)


    III                        Philadelphia                 19.6   (45)
                               Wilkes Barre                 14.3   (53)
                               Richmond                      10.5   (62)
                               Washington                    9.4   (54)

     IV                        Memphis                      13.9   (35)
                               Chattanooga                  16.8   (37)
                               Charlotte                     10.4   (55)
                               Birmingham                   11.7   (51)
                               Atlanta                      10.5   (52)
                               hiami                         13.3   (15)
                               W.  Palm Beach                 14.3   (60)

     V                        Akron                         12.8   (49)
                               Cincinnati                     9.1   (51)
                               Indianapolis                   8.3   (50)

    VI                        Beaumont                      25.3   (45)
                               Clute                         23.7   (52)
                               Dallas                        16.0   (69)
                               El  Paso                      15.3   (60)
                               Fort Worth                    11.6   (58)
                              W.  Orange                     50.0   (41)
                              Texas City                    37.7   (52)

   VII                        Kansas  City

       Median of Medians                                    13.9   (21)


          *In the Central Business District


Source:  Richter, H. G., F. F. McElroy,  V. L. Thompson, 1985:  Measurement
         of Ambient NMHC Concentrations in 22 Cities During 1984.   Paper
         85-22.7, Preprint Volume, 78th Annual Meeting Air Pollution
         Control Association, Detroit, Michigan, June 16-21.

-------
                         12-B
Table 3-10. . NMHC/NOx Emissions Ratios of Urban Counties



        (Based on NAPAP 4.2 Emissions Inventory)





    Urban Counties with Highest VOC Emissions Flux:





            County                     Ratio



    1.  New York, NY                    3.15



    2.  Queens, NY                      3.93



    3.  Baltimore City, MD              8.25



    4.  Philadelphia, PA                3.70



    5.  Richmond, NY                    4.97





                       Mean             4.80



                       Median      ,     3.93







    Urban Counties with Highest NOx 'Emissions Flux:



    1.  New York, NY         . -          3.15



    2.  Hudson, NJ                      1 .49



    3.  Queens, NY                      3.93



    4.  Union,  NJ                       2.91



    5.  Philadelphia,  PA                3.70





                       Mean       ,      3.04       .



                       Median .          3.15         .

-------
                                                   12-C
                   Table  3-11.
        The One-Hundred Most Frequently Observed
        Hydrocarbons  in  29  U.S.  Cities
                                            Total Number of Canisters = 773
                            Ave NMHC (ppbC)  = 761.0  Max NHHC = 2764.6  Min NMHC = 175.7
Rank Name
  1 TOLUENE
  2 n-PENTANE
  3 ISOPENTANE
  4 n-BUTANE
  5 m&p-XYLENE
  6 2-METHYLPENTANE
  7 ETHANE
  8 ETHYLENE
  9 BENZENE
 10 PROPANE
 11 3-METHYLPENTANE
 12 ISOBUTANE
Mean
6.0%
3.7%
7.4%
7.1%
3.3%
2.5%
4.4%
3.9%
2.2%
5.0%
1.8%
3.3%
 13 n-HEXANE,2-ETHYL-1-BUTENE2.0%
 14 ACETYLENE                2.6%
 15 1,2,4-TRIMETHYLBENZENE   2.0%
 16 o-XYLENE                 1.5%
 17 2,2,4-TRIMETHYLPENTANE   1.5%
 18 PROPENE                  2.1%
 19 2-METHYLHEXANE           1.5%
 20 p,m,o-METHYLSTYRENE      2.6%
 21 2-METHYLPROPENE.BUTENE-1 1.5%
 22 METHYLCYCLOPENTANE       1.4%
 23 ETHYLBENZENE             1.6%
 24 C10  AROMATIC             2.0%
 25 3-METHYLHEXANE           1.4%
 26 unknown                  2.2%
 27 C11  OLEFIN               2.0%
 28 n-HEPTANE                1.3%
 29 m-ETHYLTOLUENE           1.4%
 30 2,3-DIMETHYLPENTANE      1.7%
 31 1,2,3-TRIMETHYLBENZENE   4.1%
 32 n-DECANE                 1.7%
.33 a-PINENE                 4.9%
 34 METHYLCYCLOHEXANE        1.3%
 35 CYCLOHEXANE              3.2%
 36 C8 PARAFFIN              1.7%
 37 1-ME-4-ISOPROPYLBENZENE  2.3%
 38 C6 PARAFFIN              2.9%
 39 C9 OLEFIN                6.2%
 40 C10 AROMATIC             2.4%
 41  C11 AROMATIC             1.8%
 42 C11 PARAFFIN             2.7%
 43 2,2,3-TRIME-1-BUTENE     2.0%
 44  C11 AROMATIC             1.9%
 45  C10 PARAFFIN             2.8%
 46 ISOPRENE                 1.9%
 47 C-2-PENTENE              2.0%
 48  1,3-BUTADIENE            3.4%
 49  C9 PARAFFIN              2.2%
 50  1.2-DIKE-3-ETHYLBENZENE  1.8%
 ppbC  Max
 45.4 18.7%
 27.9 16.0%
 56.5 19.4%
 54.3 22.4%
 24.6 12.4%
 19.1  5.6%
 33.3 22.5%
 29.1 30.3%
 17.0  9.4%
 37.6 25.6%
 14.0  6.2%
 24.8 21.n
 15.8  8.5%
 19.3 12.3%
 14.8  7.4%
 11.0  4.2%
 12.1   2.4%
 17.2 20.2%
 11.3  3.4%
 16.3 15.8%
 11.2  9.3%
 12.8 14.2%
      13.7
       9.7
      11.8
      14.4
      10.7
      13.1
      10.3
      14.3
     18.1%
      5.4%
      4.2%
     15.0%
      7.6%
      3.3%
      2.5%
      3.6%
30.2 21.8%
13.6  3.5%
45.3 16.3%
12.2  7.2%
28.1 20.6%
12.9  4.5%
13.6  7.1%
14.4  9.3%
53.4 13.6%
25.0  4.8%
 8.8  5.6%
10.4 11.5%
14.7  8.3%
      6.5%
      5.1%
      6.0%
     10.3%
     22.1
     29.6
      8.8
     17.3
 Min Cans
 1.1% 773
 0.8% 769
 0.7% 768
 1.8% 766
 6.6% 758
 0.8% 753
 1.1% 752
 0.9% 746
 0.7% 745
 1.1% 739
 0.7% 712
 1.1% 707
 1.1% 678
 0.7% 665
 0.8% 647
 0.7% 485
 0.6% 420
 0.8% 414
 0.7% 379
 0.6% 306
 0.7% 221
 0.7% 202
 0.9% 146
 0.8% 128
 0.8% 127
 0.6% 123
 0.6% 113
 0.6% 102
 1.1% 99
 0.9%
 0.6%
 0.8%
 0.9%
 0.7%
 0.6%
 0.7%
 0.9%
 1.2%
 0.7%
 1.0%
0.9%
0.7%
0.6%
0.8%
0.9%
     22.7 10.4%
     17.8 12.6%
1.0%
0.9%
0.6%
1.2%
                                  12.2  3.8%  1.0%
76
73
71
59
52
43
42
42
41
39
37
33
29
26
25
25
25
19
18
18
18
Rank Name
  51 n-NONANE
  52 C10 PARAFFIN
  53 t-2-BUTENE
  54 C10 AROMATIC
  55 C9 PARAFFIN
  56, n-OCTANE
  57 C6 PARAFFIN'
  58 C10 PARAFFIN
  59 PARAFFIN
  60 UNKNOWN
  61 2,3-DIMETHYLBUTANE
  62 2-METHYL-2-BUTENE
  63 C3 PARAFFIN
  64 C7 PARAFFIN
  65 C5 OLEFIN
  66 2-METHYL-1-BUTENE
  67 t-2-PENTENE
  68 C10 PARAFFIN
  69 C7 PARAFFIN
  70 C6 OLEFIN
  71  C10 PARAFFIN
  72 C8 OLEFIN
  73 C6 OLEFIN
  74 ISOPROPYLBENZENE
  75  3,3-DIMETHYLPENTANE
  76 C10 PARAFFIN
  77 c-2-BUTENE
  78  C6  PARAFFIN
  79  C7  OLEFIN
  80  C6  OLEFIN
•  81  C10 PARAFFIN
  82  C3  PARAFFIN
  83  CYCLOPENTANE
  84 delta-3-CARENE
  85 C8 PARAFFIN
  86 C7 PARAFFIN
  87 C11 PARAFFIN   k
  88 2-METHYL-2-PENTENE
  89 C5 OLEFIN
 90 C12 AROMATIC
 91 C10 PARAFFIN
 92 C9 PARAFFIN
 93 C12 PARAFFIN
 94 C9 AROMATIC
 95 c or t-2-HEXENE
 96 C12 AROMATIC
 97 2,2,5-TRIMETHYLHEXANE
 98 2,4-DIMETHYLHEPTANE
 99 C5 OLEFIN
100 C4 OLEFIN
Mean
2.2%
2.2%
1.5%
1.7%
2.0%
3.4%
2.0%
1.8%
2.1%
9.8%
1.4%
2.3%
3.5%
2.4%
3.1%
1.2%
2.4%
1.7%
1.7%
1.7%
4.9%
1.5%
2.7%
3.1%
2.3%
2.7%
1.3%
1.8%
1.7%
1.9%
5.2%
1.8%
1.1%
4.4%
1.2%
1.5%
1.1%
2.4%
2.2%
1.7%
3.7%
1.6%
1.4%
1.5%
3.8%
1.3%
1.1%
1.6%
3.3%
1.4%
ppbC
17.9
25.1
15.3
19.8
10.3
18.8
13.2
16.9
9.3
121.9
21.4
22.3
21.6
11.6
31 .'9
9.3
20.7
9.2
20.8
12.8
31.7
7.7
26.6
12.8
10.7
12.0
17.4
11.7
5.4
16.0
31.9
21.4
15.1
51.0
13.0
5.5
3.6
20.0
8.2
5.8
32.9
11.6
9.0
12.5
22.2
6.3
6.8
3.6
59.9
15.7
Max
5.4%
0.1%
3.5%
3.3%
3.1%
0.4%
3.9%
4.2%
6.3%
1.7%
2.5%
1.8%
0.1%
4.0%
8.9%
2.0%
0.6%
2.1%
4.3%
2.8%
7.7%
1.9%
8.7%
6.6%
3.4%
6.2%
1.8%
3.4%
2.1%
2.4%
8.7%
2.4%
1.7%
7.4%
1.3%
2.4%
1.3%
3.0%
3.1%
2.0%
4.7%
2.2%
1.9%
1.7%
4.2%
T.5%
1.5%
1.7%
3.4%
1.5%
Min
1.0%
1.0%
0.9%
1.0%
1.2%
1.2%
1.2%
1.1%
0.9%
5.5%
0.8%
1.0%
1.2%
1.2%
1.3%
0.8%
1.0%
1.1%
1.1%
1.0%
2.5%
1.3%
1.0%
1.2%
0.7%
2.0%
1.0%
1.4%
1.3%
1.1%
2.1%
0.9%
0.8%
1.4%
1.0%
1.1%
0.8%
1.6%
1.4%
1.2%
1.4%
1.5%
1.1%
1.2%
3.2%
1.2%
1.0%
1.4%
3.1%
1.4%
Cans
17
17
15
15
14
13
12
12
12
11
10
9
9
8
8
7
7
7
6
6
6
6
6
6
5
5
5
5
5
4
4
4
4
4
4
4
4
3
3
3
3
3
3
3
2
2
2
2
2
2

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                                     13

canisters, the  25th most prevalent  species (3-methyl hexane)  appeared in
15% of  the canisters, and  the 50th most prevalent  species (1,2-dimethyl-
ethyl benzene) appeared in only 2% of the canisters.  The aromatics toluene,
ra-xylene, and p-xylene and the C4,  C5, and C6  alkanes dominate the top 10
species in the  canisters.   As will be discussed  in  a later section, these
are the species for which the chemical mechanisms are the most uncertain.

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                                       14

 4.0   CHEMICAL AND METEOROLOGICAL PROCESSES

 4.1   Chemical Processes.   Chemical Mechanisms  and Models.

       It has  been established through numerous laboratory and field  studies
 that  photochemical  ozone  and  other  oxidants  are products  of atmospheric
 reactions  involving  organic pollutants (VOC),  nitrogen oxides  (NOX)  and
 sunlight.  It is  also established that  the roles  of the VOC and NOV  precur-
 sors  in the  mechanism  of these reactions are so  involved that only  through
 complex kinetic mechanistic modeling  is  it possible to determine the magni-
 tudes, and  even  the^ direction  of the  effects  of  precursor  controls  on
 ozone.  Thus, photochemical  kinetics models are indispensable in develop-
 ment of  ozone  control  strategies.   Chemical  mechanism models  must  of
 necessity be  simpler than  the system  they  represent.  Further,  they can
 only include  what is present  knowledge of the  actual  chemical processes
 and they  well may  include distorted representations  of apparently known
 processes.  Increases in  computer resources have resulted  in increases  in
 the level of detail allowable  in chemical mechanisms and still have them be
 feasible to  solve; presumably  a  more  detailed  representation could lead to
 more accurate predictions.  In addition,  the continual increase in fundamen-
 tal ^kinetics knowledge (the detection of new reactions,  the measurement  of
 their_rate  constants,  and  the  elucidation  of  the reaction pathways  of
 organic compounds) leads to a  continual  improvement  in the  accuracy of the
 model s representation and therefore  to potentially  better  predictions  for
 untestable conditions.

      To prevent models  from being the mere opinion of their  developers all
 models that have  been  used in regulatory  applications in the US have had
 T^flSrf011 i?gainf-, ^P™ntal  dat*.  ^^lly  smog   chamber,  data.
 interestingly, all model  developers  claim to  have  "fit the  test  data"
 reasonably well.   For many of  these models, however, subsequent laboratory
 research has  revealed that many of the model's representations were incoi>
 rect  and that _ they fit  the test data because of various  compensating errors
 in the mechanism,  or because the  test data were too few, or  that critical
 input parameters  for the  test data were  poorly known, or  that  the test data
 were  simply too poor in quality to adequately exercise the weakest parts of
 w^h H?S1CS  r 6lS °r t0.be  US6ful  in distinguishing between two  models
 with different representations.  Thus,  in the presence  of such conditions,
 there  has _ been a  continual series of kinetics mechanisms "improvements"
 and, lagging  somewhat behind these theoretical developments, there has been
 the production of  experimental data  to test  and refine the mechanisms.
wirt,         ?f  th| difflcultief  in testing perhaps  imperfect mechanisms
?hi Ti??ST LTer5eCt^data' and 
-------
                                     15

evaluation have merits,  "evaluation against smog chamber data provides the
most unambiguous test of urban atmospheric photochemical mechanisms".  They
also agreed, however, that there are uncertainties associated with the smog
chamber data.   For  example,  there  are  uncertainties associated  with the
representation of chamber radical sources and of photolytic rates in outdoor
chambers, with smog  chamber measurement  errors, and with the representation
of as yet unknown reaction pathways.

     European investigators also  agreed  that it is important to ensure the
fullest possible  testing of the  chemical mechanisms against  smog chamber
data.  They also feel, however, that a further evaluation stage is required
which has been shown in Europe to be invaluable in providing policy guidance
for the ozone problem.  This involves evaluation against a benchmark chemi-
cal scheme  in  a quasi-realistic scenario application.  This evaluation has
been performed using complete and  condensed versions of schemes, to provide
benchmark secondary  pollutant  concentrations  and  chemical  reaction  flux
diagnostics.  These will have a vital role to play in  the subsequent evalua-
tion of  control  strategies  determined  from applications  of  the schemes
within large integrated modeling studies.

     Today's situation  is  that  mechanisms  suitable  for regulatory use
contain three types  of reactions:

     1)  The first class of reactions are those which are well characterized
         by the kinetics research community and appear in major reviews such
         as those  published by the NASA,  CODATA,  and  IUPAC  Groups.  At
         present these include  about 360 reactions which are mostly inorga-
         nic, but there  are data  sheets  on organic reactions for molecules
         up to three carbons.   All acceptable chemical kinetics mechanisms
         include the most important of  these  reactions  at their consensus
         rate constants.  The different  chemical mechanisms are essentially
         identical  for this portion.

     2)  The  second class of reactions  are those which are known to  occur
         and for which subsequent  reactions  of the products are fairly well
         characterized,  but  for which absolute rate  constants  are unknown.
         Thus, acceptable chemical kinetics mechanisms  will include  these
         reactions,  but  may have  different rate constants, resulting in the
         same products being  formed, but at different rates and magnitudes.
         "Model tuning"  to  experimental  data is often used to  select  these
         parameters. The C3+ olefin reactions and C6+ alkanes are in this
         class.

     3)  The  third class of reactions are those  which are known to occur,
         but for  which the subsequent reactions after the initial one are
         essentially unknown.   Thus,  chemical  kinetics  mechanisms  will
         include  the first  reaction at a consensus rate,  but subsequent
         reactions  and rates  are  based on the  beliefs  of  the mechanism
         author.  Therefore,  not  only are the parameters in the  reactions
         the  result of "model tuning", the whole reaction scheme is produced
         this way.   All of the reactions  of aromatic compounds are in this
         class.

-------
                                      16

      In addition to these classes of reactions,  to deal with the complexity
 of the hydrocarbon chemistry, two different methods  for generalizing their
 chemistries have  evolved:   the  "lumped  molecule"  or  surrogate  species
 approach,  and the  "lumped  structure"  or  carbon  bond  approach.   In  the
 former, the nearly explicit chemistry of a particular molecule is chosen to
 represent  the chemistry of an entire class of compounds, i.e.  propene  may
 represent  all terminal olefins.   Carbon number differences are ignored when
 molecules  are assigned to surrogates.   In  the latter, each molecule  to be
 represented is broken into different model species such that all the carbon
 is accounted for.  The model species are organized around carbon bond types.
 In this scheme,  propene would be assigned  to  two model molecules:   to OLE,
 which is a two-carbon double bond entity, and the terminal carbon on propene
 would be assigned to PAR, which is a single carbon entity.  Carbon concentra-
 tion is conserved in the latter.   In actual practice, each kinetics mechanism
 uses a combination of methods to  represent the complex  urban  hydrocarbon
 mix.

      Presently,  the mechanisms most comprehensively  evaluated against smog
 chamber data are the  latest versions of the Carter, Atkinson, Lurmann  (CAL)
 mechanism" and  the  Carbon Bond (CB4)  mechanism2^.  The  CAL mechanism is a
 132-reaction step  scheme  that uses  the  "lumped-molecule"  approach.   The
 CB4,  an 81-step  mechanism,  uses  a "lumped-structure"  approach.    Other
 pertinent  distinguishing characteristics of the two mechanism are summarized
 in Table 4-1.

      The CAL mechanism was evaluated by comparing mechanistic  predictions
 of ozone yields  with yields observed  in  smog  chamber  irradiations  of a
•variety of VOC,  NO^  mixtures.   The smog  chamber data  used were obtained
 from some  490 experiments  carried out in three indoor and. outdoor chambers
 of the Statewide Air Pollution Research  Center,  U.  California/Riverside,
 and one outdoor dual chamber  at  the  U.  North Carolina/Chapel  Hill.   A
 comparison of CAL-predicted  and CB4-predicted  maximum ozone concentrations
 with concentrations  observed in the smog  chamber is  shown  in Figure 4-1.
 Both mechanisms' predictions  agree with the smog  chamber data within 30%
 (with a few  exceptions),   a performance  which  at  first  glance  appears
 quite  satisfactory.   Such comparisons,  however, are  not of unquestionable
 validity.

     These evaluations  were  done  independently by  the  respective model
 developers, using somewhat different sets of smog chamber data and different
 evaluation procedures.   They  used different  assumptions regarding  light
 characterization, chamber effects, and in some cases different sets of rate
 constant values.  The mechanisms have different parameters  for the yields
 of  radicals  and  products  for propene  and differ  significantly  in their
 description of aromatics  oxidation  pathways.   In addition,  the mechanism
 tests  ignored  the  side-to-side  test conditions in  the UNC  dual chamber,
 i.e. performances were assessed  independently for each  side,  even though
 the data were paired.

-------
                                    16-A
    Table 4-1.   Characteristics of the CB4 and CAL Mechanisms  for Ozone
Characteristics
Mechanism Type
Number of Reactions
Inorganic Reactions
Organic Reactions
Photolytic Reactions
Number of Species
Inorganic Species
Primary Organicsb
or bonds representing
ambient VOC mix
Alkanes
Alkenes
Aromatics
Biogenic VOCs
Aldehydes
Non-Reactive VOCs
Organic Products
Organic Radicals
CB4
Lumped Structure
81
30
40
11
34
15
9


1
2
2
1
2
1
4
6
CAL
Lumped Molecule
132*
29
86
17
51
15
12


2
3
3
-
3
1
13
11
alncludes pseudo-first-order reaction to represent methane oxidation with
 a global methane concentration of 1.85 ppm

bOrganics or bonds for which either emissions or initial conditions should
 be specified

-------
                                      16-B
              -8
              4->
                                    • MO    AM
                                 Measured Ozone
                                                         1JD
          a
          a
          \*

          I
           c
          o
          •a
          I
O EC  7-Compon«nt
<*> ITC 4 OTC 0-Compon«nt
  UNO Multi-Component.
A ITC 4-Componont
  UNO 3-Compon«nt
  GAL Mechanism
                         T	1	1	1	1	1	1	T
                        03       0.4      0.6 '      0.8
                                   Maximum OZOM (pom)
Figure 4-1.  Scatter diagrams comparing model-predicted maximum ozone
             concentration versus measured values in several smog
             chambers

-------
                                     17

     Following the  developers tests,  a  comparison  and test  of  the  two
mechanisms using  selected  UNC  chamber  data  and  uniform  sets  of  input
parameters and conditions  was carried out at UNC25.  The first step was to
reconcile the different rate constants each mechanism  used for the inorganic
and carbonyl chemistries.  Then  a detailed characterization of the actinic
flux in  the outdoor  chamber  was used  to re-specify  the  photolytic rates
used in  both mechanisms.  Finally,  a comparison of  different  methods  for
representing the  chamber background reactivity was conducted.   The mecha-
nisms were  then  exercised over a  series  of "hierarchy  of species" tests.
Using exactly the same inputs to each mechanism, the results  for NCx,  03,
and the  principal HCs were that:

     a)  Both mechanisms were in excellent agreement with each other and
         with data for formaldehyde-NOx experiments;

     b)  Both mechanisms were in very good agreement with  ethene until the
         very end of the  experiment where the reactivity of CAL decreased
         slightly compared to the data and to  CB4;  this  decrease in CAL was
         due to different  radical termination  chemistry  than CB4;

     c)  CAL was  in better  agreement with  propene  experiments  than  CB4
         which was too reactive due to a higher radical yield in the ozone +
         propene  reactions;

     d)  Both did poorly for  1-butene experiments;

     e)  CAL was significantly better at  simulating  t-2-butene experiments
         than was CB4; this is because CAL has an explicit representation for
         t-2-butene  and  CB4  uses two ALDs  as a  surrogate representation
         which results in very slow initial chemistry in CB4;

     f)  CB4 was significantly  better at simulating toluene  experiments;
         CAL was significantly better for xylene;

     g)  Both  mechanisms  often  did better   at   simulating   mixtures  of
         hydrocarbons with all classes present than they did simulating the
         individual  components of the mixtures;

     h)  Both  mechanisms  simulated  a  16-component  synthetic automobile
         exhaust mixture  experiment  very well,  including  the effects of
         replacing 1/3 of the mixture carbon with methanol;

      i)  Both  mechanisms  were uniformly  too  reactive  for synthetic urban
         hydrocarbon mixture   (18-components)   experiments although  the
         ethene,  propene,  and toluene decays were well fitted;

     j)  Neither mechanism did well for  cool  conditions and neither mecha-
         nism predicted  formaldehyde as a product  very  well, being too low
          in the  olefin   systems  and  too  high  in  the  aromatic  systems.

-------
                                      18

      The conclusion  from  this  comparison  study  was  that  while  the two
 mechanisms sometimes differ in comparison with chamber data, in many cases,
 neither is  superior to  the  other.   Much  of the difference between the
 mechanisms arises  from the differences  in "model tuning"  against chamber
 data^ which was  used by  the developers  to estimate  the  parameters in the
 olefin and the mechanistic pathways and parameters in the aromatics chemis-
 try.  These choices become confounded  with the choices made for photolytic
 rates, that is,  the light characterization of the chambers, and  with the
 choice of wall  radical representations, that is,  with the quality of the
 chamber characterization  and  its  representation.   While  the  use  of  more
 uniform assumptions could narrow the difference between the two mechanisms,
 real advancement in mechanism quality awaits improved kinetics data on rate
 constants and pathways for secondary reactions.   Improvements in  the  data
 would result from a mechanistic  understanding of  chamber radical  sources.

      This issue of  proper evaluation of chemical  mechanisms was discussed
 exhaustively in  USEPA's   1987 Workshop  on  Mechanism  Documentation   and
 Evaluation^.   One key recommendation  arrived at  by  the participants—and
 endorsed in this  Workshop—was  that several  review groups be  established
 for the  purpose  of  periodically  assessing  the   state  of  knowledge  and
 establishing consensus  opinion  in  several domains,  namely:   accuracy  of
 kinetic data,  validity of mechanistic pathways,  quality  of  smog  chamber
 data, and mechanism evaluation (against smog chamber data) protocols.   With
 the exception  of  kinetic  data  accuracy,  no  such review activities  are
 currently in existence.  With respect to kinetic data evaluation,  two review
 panels have  been in existence for the past 12 years:   a NASA panel and  a
 CODATA Task Group.  The  NASA panel has produced  at  regular  intervals  a
 total of eight  reports  containing  evaluated data  on  approximately   200
 thermal and  photochemical  reactions.   The  CODATA  Task  Group,  recently
 replaced by an IUPAC sub-committee  has just completed  its  fourth  evaluation
 which now includes data sheets for 360 reactions of atmospheric interest
 including organic  molecules containing up  to  three carbon atoms.  Such an
 evaluation, which  involves detailed assessments  of the laboratory  studies
 along with  estimations  of error- limits  is clearly an excellent  starting
 point for considering a detailed mechanism  for the  formation of photochemi-
 cal oxidant in the  troposphere.

      It is doubtful, however,  in  terms  of the long time scale for  detailed
 kinetic data Devaluation,  if the present efforts of these panels  will ever
 reach the point  of including  a reasonably complete set of evaluated data
 for the enormous  range  of possible reactions  in  the polluted troposphere.
 It  is likely that future evaluations by  the  IUPAC sub-committee, in  particu-
 lar, will be expanded by including assessments of  only key reaction types
 for the more complex organic species.

     To fill the present  gap  between the individual reaction  approach of
 the evaluators and the detailed mechanistic requiranents of the atmospheric
modellers, it would  be  desirable  to set up an international panel with the
 task of preparing  a consensus mechanism for  tropospheric photo-oxidative
degradations or.organic species in  the NOx polluted troposphere.

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                                     19

4.2  Meteorological Processes.  Pollutant Transport and Dispersion/Transport
     Models

     The distribution  of chemical constituents emitted into the atmosphere
is critically  related  to  the  vertical  and  horizontal  transport.   The
mechanisms for  vertical  exchange  are  complex and  varied,  ranging  from
clear-air processes  over various terrain and  land use  conditions to moist
convection associated  with  non-precipitating  clouds  and cloud  systans.
Precipitating clouds redistribute pollutants vertically in the atmosphere,
with updrafts carrying surface-based pollutants into the upper layers, and
downdrafts bringing both rain and cloud and  interstitial  air  to the lower
levels of  the earth's   surface.   With regard to photochemical oxidants,
non-precipitating clouds  are  of particular interest, since they are preva-
lent in  the  warm  season  and are  effective  in  redistributing pollutants
between the mixed  layer and the  free troposphere.   The magnitude of their
impact is highly variable in time  and  space and will  depend  on the cloud
population, distribution and  their vertical extent.  Entrainment processes
within the  clouds play  a critical role  in  determining the net vertical
exchange in  the atmosphere.   The  horizontal  distribution  and population
density of  clouds  are  highly  variable  regionally   and  over  diurnal and
seasonal time  scales.    Long  range horizontal  transport  of ozone  and its
precursors are expected  to be strongly influenced by  cloud systems.  Experi-
mental evidence  of  cloud-induced vertical exchange  of ozone  between the
mixed layer and  free troposphere  has recently been documented^.

     Horizontal  transport of pollutants on  a regional  scale is controlled
by the height at which emissions are released, their chemical and physical
lifetimes and horizontal dispersion.  Consequently,  the horizontal distri-
bution of pollutants is  strongly impacted by such factors as the speed and
direction of  the transport winds,  vertical  mixing  in  and between layers,
presence of wind shear,  extent of  coupling between  the mixed layer and the
free troposphere,  surface pollutant fluxes  and  source distribution.   The
transport winds  are  expected to translate along isentropic surfaces, which
are not necessarily horizontal.  Wind shear will  cause pollutant sources to
undergo horizontal transport  and  dispersion  such  that the pollutants in the
upper air will be redistributed in  three dimensions and over a greater area
than would  be otherwise anticipated from surface  winds.   Significantly,
distorted horizontal patterns will develop  and  vary with respect  to the
vertical levels  of the atmosphere and the varying transport and dispersion
conditions.

     Simulation  of the atmospheric transport  in  photochemical  grid models
(e.g. the Systems  Applications,  Inc. Urban  Airshed  and Regional Transport
Models; the  EPA Regional Oxidant  Model)  requires  input  to the model  of
horizontal wind  vectors  defined  at each model grid point,  usually  on  an
hourly basis.  (The models themselves compute vertical  velocity via a form
of the mass continuity equation.)   Techniques  for wind  field generation can
be divided into  three general classes:

-------
                                     20

          objective analysis of observational data

          diagnostic wind modeling

          prognostic meteorological modeling

In general,  the  choice  of technique  depends  on  the spatial and temporal
representativeness of available observational data.

     Objective analysis involves  the mathematical combination  of observa-
tional data  to  produce a  wind vector  at a given grid  point.   Objective
analysis encompasses both interpolation and extrapolation, depending on the
location of the grid point with respect to the location of available obser-
vations.

     Use of  objective  analysis techniques to generate gridded wind fields
for a photochemical model implies an assumption that available observations
completely represent the airflow within the model domain.  This assumption
is frequently of doubtful validity,  especially  in regions of complex terrain
where the spatial separation between wind observations is much greater than
the relevant terrain scales.

     Diagnostic wind models provide  relatively  simple representations  of
certain complex terrain effects on airflow, including deflection of airflow
by terrain  obstacles  and  thermodynamically  generated  slope  flows.   The
diagnostic models  generally  combine  the  terrain-effect  treatments  with
objective analysis of available observations.  In one  approach, an objective
analysis of observations is carried  out;  the objectively analyzed field is
then adjusted for  terrain  effects.   In a second approach,  a "first guess"
wind field is generated  by adjustment of "mean" flow for terrain effects.
The "first-guess"  field  is  then incorporated along with available observa-
tional information into an objective analysis,  with the "first-guess" field
weighted heavily  in  subregions of  the domain  remote from observations.

     Diagnostic wind models are relatively inexpensive to run and in certain
areas may  require  fewer observations to  produce credible wind  fields.
However, diagnostic wind models are  incapable (in the  absence of representa-
tive observations)  of generating such  airflow features  as  sea  breezes,
low-level jets, and terrain-generated  mesoscale  eddies.   Representation of
such features  may  be  important  for  accurate  air  quality  simulation.

     Both objective analysis  and diagnostic wind  models rely  on observa-
tional data as critical inputs.  Observational data are irregularly distri-
buted in space, and in general, are not available in one-hourly intervals.
They have to be analyzed objectively on a regularly spaced three-dimensional
grid and interpolated  in time.   Standard methods are available to interpo-
late primary meteorological variables  as  wind  or temperature, but problems
arise in interpolating cloud  cover or  precipitation  rates.   The 12-hourly
precipitation rates from the  international  observational network  are not
sufficient for input  to  episodic models.  Also, cloud top heights are not
available from  the conventional synoptic  network.   These  gaps  could  be

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                                     21

filled partly by using satellite and radar data.  Unfortunately, these data
are not available in a  form to be used directly as input for a grid model.
Extensive data processing  and interpretation are  necessary  to extract the
desired information.  It is possible to derive variables such as the height
of cloud tops, cloud cover and cloud type from such data, but at this time
the methods needed are still under development and not applicable routinely.

     The third  category  of  wind  field  generation,  prognostic mesoscale
meteorological models, provides numerical solutions of the governing equa-
tions of  the atmosphere.   Unlike  objective  analysis  and diagnostic  wind
modeling, prognostic models do not require  significant mesoscale observa-
tional data  inputs.   Given (1)  a  representation of the  initial dynamic/
thermodynamic state of  the atmosphere  within the model domain,  and (2)  a
representation of  the  "forcing"   of  domain-scale  flow  by  larger-scale
processes not simulated by  the model, the prognostic  model simulates the
response of  the mesoscale airflow to differential surface heating (e.g.
sea breeze  circulations)  and  to  complex terrain (e.g. thermodynamically-
generated slope  flows,  blocking  and  deflection  of  airflow by   terrain
obstacles, mesoscale eddy development).

     The major advantage  of prognostic modeling over the other two methods
is the ability of prognostic models to simulate relevant physical processes
in the  absence  of  mesoscale  observational  data.  This may be especially
important in representing  the  spatial and temporal variability of upper-air
(i.e. above, say 100 m AGL) winds  for which representative observations are
frequently sparse or unavailable.

     In addition to simulating the wind  field,  prognostic models simulate
the temperature field.  Thus,  prognostic models may be  capable of providing
necessary mixing height  and  stability information  to  photochemical  grid
models.

     The major  disadvantage  of prognostic modeling is  its computational
expense relative to other methods of wind field  generation.  Additionally,
prognostic models  cannot  be expected to  reproduce all  available  individual
wind observations.  If, for example, the  location of frontal systems, cloud
and precipitation patterns, or the wind field are incorrectly  forecast, it
cannot be expected that the predicted pollution coincides with measurements.
Therefore,  if a dynamical model is used as a driver for  a. complex  dispersion
model, it  is necessary to  perform a comprehensive meteorological analysis
utilizing all available observations  in  order to estimate  the uncertainty
in the predicted meteorological variables.

     In the framework of the  PHOXA program  both methods have been  used to
prepare meteorological input for complex dispersion models.   The application
of an episodic photochemical model for the simulation of three photochemical
episodes  in north-western  Europe has  shown  that model  results  are quite
sensitive  to the  meteorological   input,  i.e. an accurate  description  of
meteorological  input  fields is a necessary premise for  good model perform-
ance.

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                                     22

     Major problem areas in the preparation of the meteorological input for
the RTM-III have been:

     ~  Wind fields over the sea.  In  Europe during the air pressure  con-
        figurations, usually associated  with oxidant formation,  pollutant
        transport occurs quite often over the sea,  e.g.  between the conti-
        nent and the UK, or  between  the UK and Scandinavia.   Lack of data
        makes it difficult to determine accurately the respective transport
        winds.

     -  Sea breeze circulations.   The  significant  temperature differences
        between land and water  establish land-sea-circulations which  lead
        to a cycling  of primary and secondary pollutants.  Available  data
        and the grid size used in  the  regional modeling make  it  difficult
        to consider such effects.

     -  Mixing  heights.   The height  of  the  boundary layer determines  the
        vertical extension of the first transport  layer of  the  RTM-III,  the
        mixed layer.  Mixing heights  for  RTM-III  are  constructed 'from
        observational data  in connection with  a boundary layer model.   In
        particular,  the  calculation of the vertical extension of the ground-
        based nighttime  inversion  is fairly  inaccurate.  There  are also
        problems in the  transition area between  land and  sea where internal
        boundary layers  can develop.

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                                     23

5.0  MODELING TECHNOLOGY AND APPLICATIONS

5.1  Physicochemical Air Quality Models

     Physicochemical air quality  simulation models (AQSM)  are now accepted
as being the most effective tools  for development  of ozone control strate-
gies.  Such  models have  been  in existence  in the US  for the  past two
decades, but  it is only recently  that AQSM's  have been put to routine use
in activities  pertaining  to assessment,  management  and  reduction  of ozone
risks.  The models most commonly used currently in the US are the Empirical
Kinetic Modeling Approach (EKMA) model2/,28, the Urban Airshed Model (UAM)zy
and  the Regional Ozone Model  (ROM) 3°.  The USEPA-developed EKMA model was
conceived  as  and intended  to  be  a  mathematical  expression of the causal
relationship between reactants and products in the 03-forming process, for
given sunlight intensity  and temperature conditions.  The model treats the
entire urban  atmosphere as  a reaction vessel, and is used in the form of 03-
isopleth plots depicting  dependence  of peak 03  concentration in the urban
area on  6-9-am  concentrations  of NMHC and NOx.   The  effect  of post-9-am
emissions  is  considered by  assuming  such  emissions  to disperse uniformly in
the  mixing layer above the  urban area.  Precursors  and  03  transported into
the  urban  area,  also,  can  be taken  into  account  using  some simplifying
assumptions.   The EKMA model is not  intended to predict absolute 03 concen-
trations;  rather,  it is intended to predict changes in peak 03 concentration
as a function of changes in the precursor  concentrations  and/or emissions.
This is  a conceptual  weakness of the model because it makes it extremely
difficult  to evaluate  the model's  accuracy  using real world data.  Relative
to UAM and ROM, EKMA is the simplest model and is appropriate for use only
' in the uncomplicated case of 03 arising at the end of the day from emissions
within an isolated urban  area.   For  complex cases,  such  as  when the 03
problem results from multi-day pollutant transport  or  from rural  emissions
or when the transported-in pollutants dominate the  03-forming process, the
EKMA model is inappropriate31.  Nevertheless,  because of its simplicity and
low application costs, the EKMA model found considerable use  in regulatory
activities in the US.

      The SAI-developed UAM model is a grid-type  model with four  vertical
layers and grid size  from  1 Km to 10 Km.   It can treat all major physical
and chemical processes underlying  the photochemical  ozone formation, namely,
advection, diffusion,  deposition and chemical transformations  of emissions.
Because of this the UAM is  capable of predicting absolute  03 concentations,
 an advantage over EKMA in that it allows for field evaluation of the model.
For the same reason,  the  UAM is inherently  more  valid  than EKMA but  is
 also much more complex.  It is also costly to use because of the  extremely
 detailed emissions and meteorological data required as input to the model.
 Like EKMA, UAM also is an urban scale model that predicts 03 concentrations
 resulting from a single day's reaction of the urban areas emissions.  It  is
 clearly the more appropriate model to use in urban areas with complex photo-
 chemical Oo problems-*'.  All  input information  required by both  EKMA and
 UAM is available  or can be measured except for  future boundary conditions
 (i.e. concentrations  of 03 and precursors  at  the  boundaries of the models'
 domains).  The  requisite data on this latter input can be estimated only
 through use of predictive regional scale models such as the ROM.

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                                      24

     The USEPA-developed ROM model is a grid-type model with 3 1 /2 vertical
 layers and 18 Km grid  size.   It was designed to  treat  all  processes  known
 to affect ozone  formation during several days  or ~1000 Kn of  pollutant
 transport, namely, advection, photochemistry, nighttime chemistry and trans-
 port,  pollutant "venting" through cumulus clouds,  mesoscale  vertical motion
 and eddy effects, terrain effects, subgrid scale  chemistry processes,  natu-
 ral emissions chemistry  and  transport,  and  wet  and  dry deposition.   The
 model  was developed  mainly for the purpose of perdicting  future impacts of
 upwind sources  on an urban area's air  quality.  Thus,  it  is ideally suited
 for implementing the  regional  approach  to  developing  urban  03  control
 strategies.   The complexity of the model and cost of  application,  however,
 limit  seriously the model's  utility.  To  illustrate  the  magnitude of  the
 modeling effort associated with applications,  a  three-day  simulation  re-
 quires six hours of  an  IBM 3090  computer as well as 25 mandays and 15  hours
 of a VAX  785  computer  for data preparation  and quality  assurance.   Also,
 the probabilistic nature of  the model predictions complicates  the use  of
 ROM for 03 strategy development.   Notwithstanding all  these  difficulties,
 however,  the  ROM is  already extensively used  in the US and promises greater
 use in the future.

 5.2 Applications of AQSM's

     Numerous AQSM  application  studies have been  conducted  in the US  by
 Federal,  State  or  local  government agencies,  research  institutions  and
 model  developers.  Most  common objective in those studies was to  study  the
 relative  roles of VOG and NOX in the  photochemical 03  problem  and determine
 and compare impacts  on 03 air quality of various unilateral  or combined VOC
 and NOx control strategies.  As a result of these studies, the USEPA has
 recently  rescinded  its   long  standing  policy that 03 must  be controlled
 through unilateral  control of VOC, and  is now receptive to 03 reduction
 strategies based on  NOx control.  The most significant  findings from  those
 studies are  listed   in  Table  5-1  in  the form  of  observations  arrived  at
 through use of the EKMA,  UAM and ROM models.

     Generally, the modeling studies to date appear to  suggest that relative
 to NOX control, VOC  control is  the more  effective approach to  urban  03
 reduction.  Existing models,  however,  still have  imperfections and, also,
 the  issue of whether or  to what degree biogenic emissions influence  the VOC-
 to-NOx ratio in urban areas generally, has not been resolved yet.

     A large  number  of photochemical model application studies have  been
 performed within Europe also,  on various aspects of the ozone problem.   A
 wide variety of  approaches  have  been adopted to account for dispersion and
 transport including  single layer  long  range transport  trajectory models,
 urban  scale trajectory  models and  large-scale  grid models.  The   chemical
 schemes vary from extensive schemes involving over 300 reactions through to
 the highly condensed acid-parameterized schemes associated with grid models.
 Common themes recur  in  all these applications;  hydrocarbon controls always
 reduce ozone whereas nitrogen oxides controls always increase ozone in some
places and decrease  ozone in  other places.  Also,  a framework of  emission
 control scenarios incorporating  Best Available  Control Technologies  have
been analyzed showing the importance  of controlling some source categories
and the rfcj.atively smaller impact of controlling others.

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                                    24-A
  Table 5-1.  Summary of Modeling Results Concerning Effectiveness of VOC,
                   and Combined Strategies for Reducing 03
Observation

 1 .  NOX decrease increases 03 near sources of NO

 2.  NQx control reduces peaks, but may move them
     closer to cities
 3.
 4.
 5.
 6 .
     With "high" NMOC/NOx ratios (e.g. >10:1)
     reductions in peak 03 accompanying initial
     control efforts may be more pronounced with
     NOX controls than for VOC controls

     Despite more rapid initial reduction in peak
     03, ultimate efforts needed to attain an air
     quality goal may sometimes be greater for
     NOX control than for VOC
     Greater benefit of 110^ control appears far
     downwind of urban areas (where 03 formation
     is presumably N0x-limited)

     Undesirable effects in #1 , 2 , 4 may be reduced
     or sometimes eliminated by controlling both
     VOC and
 8.
 9.
10.
11.
     Increases in 03 due to NO^ control occur in
     urban commercial districts where 03 is
     relatively low
     (Note:  ROM results show this result as well
     as showing 03 increases in the vicinity of
     high concentration areas near major urban
     source regions.  This could reflect ROM's
     coarser spatial resolution or UAM's limited
     ability to consider transport from upwind
     sources .)

     VOC controls work by delaying or slowing down
     03 accumulation

     VOC controls reduce peak 03 and move the
     reduced peaks further downwind

     Greatest reduction in 03 accompanying VOC
     controls occurs in 'major source areas, with
     reductions being somewhat less far downwind

     With "high" NMOC/NOx ratios (e.g. >10:1)
     effect of initial, increments of VOC control
     may be small
   Model(s)

EKMA, UAM, ROM

UAM


EKMA




EKMA




EKMA, UAM, ROM



EKMA.



UAM
EKMA


EKMA, UAM., ROM


EKMA, UAM, ROM



EKMA

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                                24-A (cont'd)
 Observation                                                   Model(s)
 12.   NOx or VOC + NOx control becomes                       EKMA
      preferable to controlling VOC
      alone  as

      a.   NMDC/NOx ratio  increases

      b.   severity of observed 03 levels decrease

      c.   reactivity of VOC emissions increases

      d.   atmospheric dilution increases

 13.   NOX controls  could  lower population exposed            UAM
      to  peak 03 levels but raise population
      exposed to moderate levels

 14.   The variation of VOC composition as described          EKMA
      in  Section 3.2.4 was found to have less than
      10% effect on VOC control requirements for
      both the CB4  and GAL mechanisms
Note:  UAM results reflect use of CB2 chemical mechanism.
       EKMA results reflect use of CB3 chemical mechanism.
       ROM results reflect use of CB4 chemical mechanism.
* EKMA: Empirical Kinetic Modeling Approach,  trajectory model on the
        urban scale, vertical resolution is mixed layer average

  UAM:  Urban Airshed Model,  three-dimensional grid model on the
        urban scale

  ROM:  Regional Oxidant Model,  three-dimensional grid model on the
        regional scale (1000  km)

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                                     25

6.0  SCIENTIFIC ISSUES ASSOCIATED WITH.03 CONTROL STRATEGIES

     Despite decades of research in several countries on all aspects of the
photochemical 03 problem, scientific  issues  still persist and, apparently,
hamper the  03  control effort  seriously.   Evidence  on  existing scientific
issues has been provided on an issue-by-issue basis by researchers and also
collectively by the  fact that apparent emission  changes  have not impacted
03 air quality in accordance with theoretical expectations.  The experience
in the US, for example, is that despite the substantial VOC controls effected
in past years the 03  air quality standard of 0.12 ppm for 1 hr/year continues
to be unattainable in most  urban areas.  The  USEPA viewpoint  on  this 03
non-attainment problem  is that  while unresolved scientific  issues  are a
part of the cause, most  of the problem is probably due to uncontrolled^and
unpredicted emissions growth that partly  or more than offset the emissions
reduction due  to controls.  Critics  of  the  OSEPA policies,  on the other
hand, allege that while  all  reasons for the non-attainment problem are not
clear, at  least  one  cause of the problem is that the US control policy is
based on  inadequate, if not wrong, understanding  of the photochemical 03
formation process and the factors affecting  it.

     As already discussed, well established scientific issues exist within
the chemical  mechanism  area,  namely:  the mechanisms  of  the  atmospheric
reactions of the aromatic  VOC's and the large molecular size VOC's are not
known accurately.   Also, uncertainties  exist  in the photolytic roles of
certain important  carbonyls  (e.g.  formaldehyde, glyoxals, ketones).  There
may be  other  inaccuracies  that escape detection because  the methods  for
evaluating  chemical  mechanisms  and kinetic parameters of  the  involved reac-
tion steps  have not been perfected  yet.  Thus,  evaluation  of mechanisms
through comparisons  with smog  chamber data is  still obscured by the  fact
that chamber  walls cause "extra reactivity" the  origins  of and  methods for
accounting for which have introduced uncertainties  in predictions.  Errors
are also  likely to be introduced by errors in the chemical  composition of
the ambient VOC mix—an important input  to  mechanistic models.  Errors of
this type are most  likely to  occur in the  measurements  of  oxygenated and
large molecular  size VOC's.

     In the EKMA modeling area,  the next  most important issue is the selec-
tion of  the  VOC-to-NOx ratio  value  to  be  used  as input  to  the model.
Measurements  of the 6-9-am ratio in center city areas give  highly  varying
 (with  time and  location)  results  and no bases  have  been  found  yet  for
justifying selection of e.g. the average or the median or any other single
value  for the ratio.

     In the emissions  disperison area, the most important issue probably is
 the one associated with the accuracy of the emission inventory data currently
available.  There is considerable evidence that the IE  emission inventories
 for VOC are  underestimated  in some  cases  because sources have  escaped
 inventorying and in other cases because emission rates  have been underesti-
mated.   Use of underestimated  VOC  emission inventory data would result in
artificially low VOC-to-NOx ratio conditions which, in turn,  would make the
models overpredict  the  effectiveness of VOC  control  or underpredict VOC
 control requirements.  A similar effect and error may be caused by  ignoring
 the biogenic VOC emissions in urban ozone control strategies.

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                                      26

     These as  yet unresolved issues have cast doubts on the reliability of
 the  current air quality models, not only for computing control requirements
 but  also for determining whether, relative  to NO* control, VOC control is
 the  more effective approach to  03 reduction.  With respect to the roles of
 these  scientific issues in the 03 non-attainment problem,  the US experiences
 have been used to support three distinct viewpoints.  The USEPA viewpoint
 adhering to the air quality management  approach to combating air pollution'
 favors continuing confidence in  current scientific  knowledge  and models'
 As its post 1987  ozone  policy,  USEPA continues to favor VOC control for Ch
 reduction but  is now receptive to strategies  that  include NOX control for
 achievement of the 03  standard.   An opposing  viewpoint,  expressed within
 the  industrial scientific community, holds  that current  understanding of
 the  ozone problem  is seriously lacking and that triggering  of the photo-
 chemical  ozone-forming  process  by  photochemically  aged pollutants  and by
 stratospheric  ozone are not  properly  considered  in the  theory  currently
 accepted  and used by  USEPA.  Finally,  the viewpoint held  by  some  State of
 California  air pollution analysts is that state-of-the-art models  are not
 reliable  enough to  be used  for  development of quantitative control strate-
 gies;  they  should be used  instead  only for making general  or qualitative
judgments about  effects of emission  controls  or of  other factors  on air
 quality.  Others,  such  as the South Coast Air Quality Management District
are making  comprehensive use of  three-day  simulations  with an  enhanced
version of  the Urban Airshed model.

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                                     27
7.0  CONCLUSIONS AND RECOMMENDATIONS

1 .  Photochemical 03  problem arises from atmospheric reactions  of VOC and
    NOx emissions  under  favorable  sunlight  intensity,  temperature  and
    dispersion conditions.   Such conditions occur  frequently both  in the
    US and Europe as  suggested by  the 03 monitoring  data available  for
    urban and rural areas in the two continents.  Such data indicate hourly
    03 concentrations as high as 0.3 ppm to occur in Europe and even higher
    in the US.

2.  The dual roles  of VOC and NC^,  being both precursors and scavengers of
    ozone, make  the  photochemical  03  formation process  so  complex that
    effective ozone control  strategies  cannot be developed based on common
    sense alone.  Accurate ozone air quality models are required, which, in
    turn, requires  that the processes of emission,  dispersion and chemical
    reaction of ozone precursors  in the atmosphere  be understood in detail
    and quantitatively.   These processes have  received in  the  past years
    considerable research attention  both in the US  and  Europe but signifi-
    cant gaps and scientific issues  are  still in  existence.  The seriousness
    and apparent  intractability of  the  photochemical  ozone problem make it
    imperative that research  continues  toward  resolution of the scientific
    issues and that the research efforts in .the European countries and the
    US be  coordinated to  the  extent possible  for maximum effectiveness.

3.  Precursor emission rates are the single most important factor to consider
    in development  and implementation  of ozone  control strategies.  Sub-
    stantial efforts  have been expended both  in  Europe and  the  US  for
    development of accurate VOC and NOx  emissions inventories.  Considerable
    uncertainties, however, continue to exist especially in the levels and
    composition of  VOC emissions.   Particularly disconcerting  are errors
    causing underestimation of VOC  emissions because such errors also lead
    to overestimation of the effectiveness of VOC controls for 03 reduction.
    Crucial uncertainties are associated also with the biogenic VOC's, both
    in regards to their emission levels  and also in regards to the importance
    of their role in the chemistry with  respect to destruction and formation
    processes of  tropospheric ozone.

4.  Atmospheric dispersion and transport processes  are  of particular inte-
    rest both because of their direct  connection to the magnitude of the
    ozone problem and also because of  the political implications of  inter-
    country or  inter-state  pollutant transport.   This emphasizes the need,
    both in Europe  and in the  US , for  regional  scale ozone models capable
    of determining  source  area-to-receptor  area  and  ozone-to-precursor
    emissions relationships in  a quantitative and reliable fashion.

 5.  Significant  advances have  been achieved  in the  recent years  in the
    atmospheric chemistry underlying the photochemical ozone problem.  Atmo-
    spheric reaction  pathways have  been established for most ambient VOC's
    and reaction  rate constant values  for a significant number  of atmo-
    spheric reaction  steps  are  of  undisputed  validity.   Gaps of strong
    consequence,  however,  still  exist, particularly in the  aromatic VOC

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                                      28

     chemistry area and perhaps in  other,  unsuspected areas  as  well.   With
     re!£e? u° Jhis, la^ter  P°ssibility,  it  is  crucially  important  that
     methods be developed  for reliably and  accurately evaluating  chemical
     mechanisms and identifying sources of error.  Given the importance  of
     the existing  gaps  and issues  and the  substantial relevant  expertise
     lying within  many countries  in the world,  it would be  extremely  pro-
     ductive to promote  international  collaboration  among  experts in the
     atmospheric reaction  mechanism, kinetics, and  chemical modeling areas.

6.   Ozone air quality models are now available and in routine use both  in
      u-US  f£5 Eur°Pe-   Modeling   studies  to  date  established  that the
     ambient VOC-to-NOx  ratio condition is extremely  important  in that  it
     determines whether  VOC control or NOx  control is  the more  effective
     approach  to ambient  03  reduction.  The models  indicate specifically
     that  low  VOC/NOx conditions favor VOC control whereas  under high VOC/
     NOx conditions NC^  control is  the  more  effective approach to  reducing
     peak  03  concentrations.   While  the quantitative  aspects of the ozone-
     precursor dependencies derived  by models  are uncertain reflecting the
     uncertainties in  the   model and model  inputs used,  the qualitative
     aspects and,  in  particular, the directional effects described above of
    precursor  controls on ozone for high  and for  low VOC/NOx conditions
    are almost certain to be accurate,  unaffected by current model imperfec-
    tions.  This  underscores  the importance  of  the  VOC/NOx  input to  the
    models and, hence, the need for reliable estimation of the VOC and NCv
    emission and ambient concentration factors.

7.  Based on the conclusions from the Workshop discussions and on impressions
    trom^ interactions among the Workshop participants,  the Workshop Steering
    Committee submitted the following specific  recommendations  for future
    actions:                                                          U.L.IU.C

    (a)   The results  of this Workshop should be reported to the Coordinators
         of  the US-German Environmental  Program, and that work on the photo-
         chemical  ozone problem  and  related  issues  be   recognized   and
         continued as a  Project activity  under  the  US/FRG  Environmental
        Agreement, with Dr. Basil Dimitriades, USEPA,  and Mr. Erich Weber
        FRG/BMJ,  as  the respective  US and  FRG Co-Chairmen.

    (b)  Support should be provided  by  the US and FRG Governments  for  the
        organization and  conduct of the  Second  US/FRG  Workshop on Ozone
        in  FY-90  (i.e. Spring 1990).

    (c)  A program  should be sponsored within  the  US/FRG  Environmental
        Agreement for  facilitating/supporting   exchange   of   scientists
        between US and FRG for  a three  to  six-month duration.

    (d)  International Work Groups   should be  formed  under  joint US/FRG
        sponsorship  to perform critical reviews  and assessments of:

        (i)    State-of-the-Science  chemical mechanisms for ozone

        (ii)   Existing smog chamber  data bases

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                            29

(iii) Existing reaction rate constants

(iv)  Development of advanced analytical techniques applicable for
      field as well as for smog chamber studies

(v)   Research needs in the area of ozone problems in general.

The Work  Groups should  convene  in conjunction  with  the  Second
US/FRG Workshop on Ozone.

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                                      30

 8.0  REFERENCES
   *  ISScnn/Q of S^  /cy CrLteria for Ozone and Other Photochemical Oxidants."
      &m-6UU/8-84-OZO  (5  volumes),  U.  S.  Environmental  Protection  Agency
      Environmental Criteria and  Assessment Office,  Research  Triangle Park  NC
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                                     31
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                                     32

25.  Jeffries, H. E.,  K.  G. Sexton, J. R,  Arnold,  and J. L. Li.  "Valida-
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                                     33

                            LIST OF PARTICIPANTS
Monika Baer
Institut fur Meteorologie
und KLimaforschung
Kernforschungszentrura
Karlsruhe/Universit'at Karlsruhe
Postfach 3640
7500 Karlsruhe/FRG
Tel. (7247)824770

Volker Bastian
Universitat Wuppertal
Phys. Chemie, Fachbereich 9
Gaupstr. 20
5600 Wuppertal/FRG
Tel. (202)439-2510

Karl H. Becker
Universitat Wuppertal
Phys. Chemie, Fachbereich 9
Gaupstr. 20
5600 Wuppertal/FRG
Tel. (202)439-2666

Frank Black
Atmospheric Sciences Research Laboratory
US Environmental Protection Agency
Research Triangle Park, NC  27711/USA
Tel. (919)541-3037

Thomas C. Curran
Office of Air Quality Planning and Standards
US Environmental Protection Agency
Research Triangle Park, NC  27711/USA
Tel. (919)541-5467

Kenneth L. Darnerjian
Atmospheric Sciences Research Centre
State University of New York
100 Fuller Road
Albany, NY  12205/USA
Tel. (518)442-3820

Richard G. Derwent
Harwell Laboratories
Didcot, Oxfordshire
0X11 ORA/UK
Tel. (235)24141 ext. 4403

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                                      34

 Basil Dimitriades
 Atmospheric Sciences Research Laboratory
 US Environmental Protection Agency
 Research Triangle Park,  NC 27711/USA
 Tel.  (919)541-2706

 Ralph Drauschke
 Amt fur Uraweltschutz
 Eifelwall 7
 5000  Koln/FRG
 Tel.  (221)2217617

 Adolf Ebel
 Universitat Koln
 Institut fur Geophysik
 und Meteorologie
 Albertus Magnus Platz
 5000  K61n 41/FRG
 Tel.  (221)212995

 Wolfgang Fricke
 Umweltbundesamt
 Pilotstation
 Frankfurterstr.  135
 6050  Offenbach/FRG
 Tel.  (69)888038

 Klaus D.  Hofken
 GSF Munchen/Proj ekttrager
 Umwelt -  und Klimaforschung
 Ingolstadter Landstr.  1
 8042  Neuherberg/FRG
 Tel.  (89)3187-3375

 Harvey E. Jeffries
 School  of Public Health
 University of North Carolina
 Chapel  Hill,  NC  27514/USA
 Tel.  (919)966-3848

 Dieter Jost
 Umweltbundesamt
 Bismarckplatz 1
 1000  Berlin  33/FRG
 Tel.  (30)8903294

 Michael Kaup
Amt fur Umweltschutz Koln
 Eifelwall 7
 5000 Koln/FRG
Tel.  (221)2217617

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                                     35

J. Alister Kerr
Department of Chemistry
University of Birmingham
Birmingham B15 2TT/UK
Tel. (21)414-4418

Robert C. Kessler
Systems Applications, Inc.
101 Lucas Valley Road
San Rafael, CA  94903/USA
Tel. (415)472-4011

Dieter KLey
Kernforschungsanlage Julich
Institut "Chemie der Atmosphare" ,
Postfach 1913
5170 Julich/FRG
Tel. (2461)613741

Barbara Lubkert
OECD, Environment Directorate
2, rue Andre Pascal
75775 Paris Cedex 16/F
Tel. (1) 45027612 (OECD)
     (43-2236)71521547 (IIASA/Austria)

Terry McGuire
Technical Support Division
California Air Resources Board
P.O. Box 2815
Sacramento, CA  95812/USA
Tel. (916)322-5350

Edwin L. Meyer
Office of Air Quality Planning Planning and Standards
US Environmental Protection Agency
Research Triangle Park, NC  27711/USA
Tel. (919)541-5594

Christa Morawa
Urnweltbundesamt
Bistnarckplatz 1
1000 Berlin 33/ERG
Tel. (30)8903-249

Katrin Nodop
NILU, Norsk Institutt for
Luftforskning
Postboks 64
2001 Lillestrom/N
Tel. (6)814170

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                                      36

 Andreas Obermeier
 Institut fur Kernenergetik
 Universitat Stuttgart/FRG
 Pfaffenwaldring 31
 7000 Stuttgart 80
 Tel. (711)685-2388

 Dieter Paffrath
 DRVLR, Institut fur
 Physik der Atmosphare"
 Munchener Str.
 8031  Oberpfaffenhofen/FRG
 Tel. (8153)28-511

 Jlirgen Pankrath
 Umweltbundesamt
 Bismarckplatz 1
 1000 Berlin 33/FRG
 Tel.  (30)8903-375

 Ulrich Platt
 Kernforschungsanlage Jlilich
 ICH 3
 Postfach 1913
 5170 Julich/FRG
 Tel.  (2461)613239

 S.  Trivikrama Rao
 Bureau of Air Research
 Division of Air Resources
 New York State Department of
 Environmental Conservation
 50 Wolf Road
Albany,  NY   12233/USA
 Tel.  (518)457-3200

 Kenneth L. Schere
Atmospheric Sciences Research Laboratory
US Environmental Protection Agency
Research Triangle Park, NC  27711/USA
Tel.  (919)541-3795

Ulrich Schurath
 Institut fur Phys. Chemie
der Universitat Bonn
Wegelerstr. 12
5300 Bonn/FRG
Tel.  (228)732507

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                                     37

Rainer Stern
Inst. f. Geophysikalische
Wissenschaften der
Freien Universitat Berlin
Thielallee 50
1000 Berlin 33/FRG
Tel. (30)838-3471

David Strother
Office of International Activities
US Environmental Protection Agency
Washington, DC  20460/USA
Tel. (202)382-4892

William Sylte
California Air Resources Board
P.O. Box 2815
Sacramento, CA  95812/USA
Tel. (916)362-9920

Neil B.A. Trivett
Air Quality and Inter-Environment
Research Branch
Atmospheric Environment Service
4905 Dufferin Street
Downsview
Ontario M3H 5T4/Canada
Tel. (416)739-4447

Chris Veldt
TNO
Division of Technology for Society
P.B. 342
NL - 7300 AH Apeldoorn/NL

Harry M. Walker
H.M. Walker and Associates, Inc.
3321 East Bayou Drive
Dickinson, TX  77539/USA
Tel. (713)337-1177

Erich Weber
Bundesministerium fur linwelt,
Naturschutz und Reaktorsicherheit
IG I 2
Postfach
5300 Bonn/FRG
Tel. (228)3052421

         •&US. GOVERNMENT PRINTING OFFICE: 1989 - 648-163/00305.

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