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CITYDELTA WORKSHOP MATERA FREE UNIVERSITY BERLIN CONTRIBUTION: LONG TERM MODELLING OF OXIDANTS AND A

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City-Delta Workshop Matera, October 2003. CITY-DELTA WORKSHOP MATERA ... Jennifer A. Logan. Harvard University, Cambridge, Massachusetts: ... – PowerPoint PPT presentation

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Title: CITYDELTA WORKSHOP MATERA FREE UNIVERSITY BERLIN CONTRIBUTION: LONG TERM MODELLING OF OXIDANTS AND A


1
CITY-DELTA WORKSHOP MATERA FREE UNIVERSITY
BERLIN CONTRIBUTION LONG TERM MODELLING OF
OXIDANTS AND AEROSOLS IN THE BERLIN-BRANDENBURG
AREA CD IIΒ PRELIMINARY RESULTS
  • R. Stern, A. Kerschbaumer
  • Free University Berlin
  • Institute of Meteorology
  • Carl-Heinrich-Becker-Weg 6-10, D-12165 Berlin,
    Germany

2
REM/CALGRID (RCG)COMBINED 3-D REGIONAL/URBAN
MODEL
  • TRANSPORT IN THE LOWER TROPOSPHERE
  • PHOTOCHEMICAL TRANSFORMATIONS (CB4-Mechanism)
  • Formation of O3 and other oxidants
  • INORGANIC AEROSOL FORMATION (ISORROPIA-Module)
  • Primary particles, fine and coarse mode PM2.5
    (EC, OC, Other) , PM10-PM2.5
  • Secondary inorganic aerosols SO4, NO3, NH4, Na,
    Cl
  • ORGANIC AEROSOL FORMATION (simplified
    SORGAM-Module of FORD)
  • SOA production caused by anthropogenic and
    biogenic VOC-precursors
  • DRY AND WET REMOVAL PROCESSES
  • EMISSIONS INTERFACE FOR LONG TERM APPLICATIONS
  • On the fly calculations of hourly anthropogenic
    and biogenic emissions, sea salt emissions, and
    wind blown dust (simple, very preliminary
    parametrization based on landuse and windspeed)

3
RCG-APPLICATION STATUS FOR CITY-DELTA II
  • 6 Runs EUROPEAN SCALE (EMEP-Emissions) Base Run
    1999, 5 scenario runs, (0.5 lon, 0.25 lat),
    Boundary conditions (BC)
  • 8 Runs URBAN SCALE BERLIN Base Run 1999, 7
    scenario runs (ca. 4x4 km2 )
  • SCENARIOS
  • Scenario 1 CLE 2010
    BC CLE
  • Scenario 2 CLE MFR1 (NOX ,SO2, PM) BCMFR1
  • Scenario 3 CLE MFR2 (VOC, CO, NH3) BC
    MFR2
  • Scenario 4 MFR 2010
    BC MFR 2010
  • Scenario 5 CLE MFR1 (NOX ,SO2, PM) BC CLE
  • Scenario 6 CLE MFR2 (VOC ,CO,NH3) BC CLE
  • Scenario 7 MFR 2010
    BC CLE

4
Large Scale RCG model area
  • RESOLUTION 0.25 LATIDUDE, 0.5 LONGITUDE

5
Urban scale modelling domain approx. 300x300 km2
long lat grid , ? long 0.06250, ? lat 0.03125(
approx. 4x4 km2)
6
RCG-Model Configuration
  • 5 vertical layers
  • a 20 m thick surface layer
  • two equal-thickness layers below the mixing
    height
  • 2 above the mixing height and extending to the
    domain top at 2500 m.
  • Results are for 10 m

7
LARGE AND URBAN SCALE DIAGNOSTIC METEOROLOGICAL
ANALYSIS SYSTEM
  • Optimum Interpolation of synoptic and radiosonde
    data
  • Vertical Resolution Isentropic surfaces 0 -10km
  • Time resolution 3 h
  • 3-D Wind, Temperature, Humidity, Density
  • 2-D Cloud cover, Mixing Height, Rain, u, MOL,
    surface wind, temperature

8
URBAN SCALE EMISSIONS BERLIN-BRANDENBURG CD II
  • Annual emission totals taken from the
    City-Delta II web page
  • Time profiles taken from the City-Delta II web
    page
  • VOC Profiles taken from the City-Delta II web
    page
  • No plume rise for point sources
  • Original data resolution ca. 2x2 km2,
    aggregated to model resolution of ca. 4x4 km2
  • Major differences to CD I Berlin emissions
  • factor of 2 more VOC emissions
  • factor of 10 less SO2 emissions
  • ca. 20 less PM emissions, ca. 10 less NOx
    emissions

9
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10
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11
BOUNDARY CONFIGURATION
  • Taken from RCG-large scale run (EMEP-Emissions)
  • Identical vertical configuration
  • 57 species
  • Hourly Update

12
REM/CALGRID TROPOSPHERIC O3 BACKGROUND USED FOR
URBAN AND REGIONAL APPLICATIONS
3-D monthly ozone climatology with resolution of
4 in latitude by 5 in longitude Jennifer A.
Logan Harvard University, Cambridge,
Massachusetts sonde data were used in
combination with surface and satellite data to
derive a gridded climatology for tropospheric
ozone
13
SOME EVALUATION RESULTSBASE CASE O3, NO2, PM10
  • 4x4 urban scale CD I versus CD II
  • CD II
  • New emissions, new time profiles, new VOC
    profiles
  • New meteorological data
  • Parameterization of wind blown dust as function
    of landuse and windspeed (very preliminary !!)
  • SOA added to the model
  • New parametrization of sulfate formation

14
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15
REM/CALGRID SIMULATION O3
16
No of days with max O3 8hmean gt 120Β΅g/m3
17
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18
REM/CALGRID SIMULATION NO2
19
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20
REM/CALGRID SIMULATION PM10
PM10 observed 0.8 TSP observed
21
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22
SUMMARY REM/CALGRID SIMULATION CD II
  • Compared to CD I
  • Higher O3 peak concentrations (higher
    background, higher VOC emissions in BB area)
  • Higher PM concentrations (less emissions than in
    CD I, but SOA added, wind blown dust added)
  • Slightly less NO2 concentrations (less emissions
    than in CD I)
  • Compared to Measurements (urban and rural, no
    street)
  • Overestimation of the observed O3 peak maxima
  • Underestimation of observed PM concentrations in
    summer
  • Underestimation of observed NO2 concentrations
  • NO check whether a station is representative for
    a 4x4 km2 grid !!!!
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