meteorological and photochemical modelling at the csir · 2014. 3. 17. · •new group, seasoned...

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© CSIR 2010 Slide 1 www.csir.co.za Meteorological and Photochemical Modelling at the CSIR Mogesh Naidoo Climate Studies, Modelling and Environmental Health Natural Resources and the Environment CSIR Dialogue on Integrated Local and Regional Scale Air Quality Modelling using the GAINS Model 14 th February 2014 Knowledge Commons, CSIR, Pretoria.

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  • © CSIR 2010 Slide 1 www.csir.co.za

    Meteorological and Photochemical Modelling at the CSIR

    Mogesh Naidoo Climate Studies, Modelling and Environmental Health

    Natural Resources and the Environment

    CSIR

    Dialogue on Integrated Local and Regional Scale Air Quality Modelling

    using the GAINS Model 14th February 2014

    Knowledge Commons, CSIR, Pretoria.

  • © CSIR 2010 Slide 2

    • New group, seasoned scientists (atmospheric, environmental, health)

    • Modelling = Atmospheric (Climate and Air Quality)

    • Climate modelling output (present day + projections) • Hydrological studies

    • Agriculture impact

    • Land-surface processes

    • Seasonal forecasting

    • Adaptation planning

    • Vulnerability studies

    • Air quality modelling output (present day + projections) • Environmental health

    • Regional tropospheric chemistry research

    • Industrial and municipal impact studies

    Research at CSM&EH

  • © CSIR 2010 Slide 3

    • NWP and RCM based on the Conformal Cubic Atmospheric Model

    (CCAM). Developed at CSIRO

    • CCAM is a cube-based global model; semi-Lagrangian semi-implicit

    solution of the hydrostatic primitive equations

    Climate modelling

  • © CSIR 2010 Slide 4

    • Can run in quasi-uniform (previous slide) or stretched grid mode

    Climate modelling

    CCAM applied in stretched-grid mode Modest stretching provides a resolution

    of about 0.5 degrees over tropical and

    southern Africa; decreases to about 4

    degrees in the far-field. Options for

    spectral nudging, gridpoint nudging or

    no nudging from the host model

    (atmospheric fields)

  • © CSIR 2010 Slide 5

    Climate modelling

    CGCMs: A2 SRES and RCP4.5 & 8.5 Simulation period: 1961 - 2100

    Global simulations,

    quasi-uniform C192

    resolution (~ 50 km)

    Very high-resolution

    simulations over

    areas of interest (~ 8

    km).

    Bias corrected SST and SIC

    SST, sea ice, atmospheric

    nudging

    User applications Regrid to

    lat/lon

  • © CSIR 2010 Slide 6

    • Model verification

    Climate modelling

    Intra-annual cycle in rainfall and circulation

    (Engelbrecht et al., 2009; IJC)

    Closed-low tracks and extreme rainfall

    events (Engelbrecht et al., 2012; IJC)

    Inter-annual variability in AMIP-style runs

    (Landman et al., 2010; WRC Report)

    Accuracy and skill in short-range weather

    forecasting (Potgieter 2006; Engelbrecht et

    al., 2011; Water SA)

  • © CSIR 2010 Slide 7

    • Results used previously

    Climate modelling

    CCAM ensemble: projected change in annual average

    temperature for 2071-2100 vs 1961-1990

    Under the A2 emission scenario, temperature increases of more

    than 4oC are projected for the region, ~x2 the global rate.

    This occurs in response to the strengthening of high-pressure

    systems in the mid-troposphere over South Africa

  • © CSIR 2010 Slide 8

    • Results used previously

    Climate modelling

    CCAM ensemble: projected change in the number of very hot

    days (annual totals) for 2071-2100 vs 1961-1990

    Under the A2 emission scenario, it is plausible that drastic

    increases in the annual number of very hot days will occur over

    the region – the number of such days is projected to increase by

    90 to 120 over north-eastern South Africa

  • © CSIR 2010 Slide 9

    • Results used previously

    Climate modelling

    CCAM ensemble: projected change in the number of extreme

    rainfall events for 2071-2100 vs 1961-1990

    A general increase in the frequency of occurrence of extreme

    rainfall events (20 mm of rain falling within 24 hours over an area

    of 50 km x 50 km) is projected for South Africa

  • © CSIR 2010 Slide 10

    • Results currently generated, e.g 8km Limpopo basin run

    Climate modelling

  • © CSIR 2010 Slide 11 www.csir.co.za

    Air Quality modelling

    © CSIR 2013

    • A changing climate effect on air quality?

    • Rainfall, temperature, cloud cover, inversions, advection

    • CCAM climate model forcing CAMx photochemical air quality model

    • CAMx = ozone (NOx, VOC species, PM species)

    • Model period 1989 – 2009 (20 years)

    • Inter-annual variability

    • 20 years not enough (Large ENSO cycles)

    • Earliest is 1989 due to input required (TOMS)

  • © CSIR 2010 Slide 12 www.csir.co.za

    Air Quality modelling – CCAM-CAMx

    © CSIR 2013

    CAMx

    Surface and 3D concentrations

    Source apportionment

    Process analysis

    Deposition (wet and dry)

    CCAM Meteorology NCEP

    Reanalysis (FNL)

    EPS Emissions Emissions data

    (Spatial, temporal, speciated)

    Initial / Boundary ICBC

    Cape GAW data

    Photolysis rates NCAR TUV

    TOMS / OMI Total column

    ozone

  • © CSIR 2010 Slide 13 www.csir.co.za

    Air Quality modelling – Current domains

    © CSIR 2013

  • © CSIR 2010 Slide 14 www.csir.co.za

    Air Quality modelling – Emissions inventory

    © CSIR 2013

    • Previous research emission inventory (ozone formation over the Highveld)

    o National at 12km resolution

    o NOx, VOC, PM, SO2, CO and NH3

    • Large industry (Sasol + Eskom + Coastal refineries)

    • Small industry (Scheduled processes)

    • Transport sector (SANRAL ADT + Arrive Alive)

    • Residential fuel combustion (Census 2001)

    • Biogenic emissions (GLOBEIS)

  • © CSIR 2010 Slide 15 www.csir.co.za

    Air Quality modelling – Ancillary data

    © CSIR 2013

    • Photolysis rates

    o NCAR TUV radiative transfer model (results for CB4)

    o TOMS/OMI total column ozone

    • No total column ozone measurements for 1995/96

    • Lateral boundary and initial conditions

    o Cape Point GAW data

    o Model initialize beginning of every month

  • © CSIR 2010 Slide 16 www.csir.co.za

    Air Quality modelling – Camden monitoring station

    © CSIR 2013

  • © CSIR 2010 Slide 17 www.csir.co.za

    Results – Camden comparison 2006 (Annual average diurnal)

    © CSIR 2013

    0

    10

    20

    30

    40

    50

    60

    1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24

    Ave

    rag

    e s

    urf

    ac

    e o

    zo

    ne

    (p

    pb

    )

    Hour of day

    OBS

    CAMx

  • © CSIR 2010 Slide 18 www.csir.co.za

    Results – Camden comparison 2006 (Seasonal diurnal average)

    © CSIR 2013

    0

    10

    20

    30

    40

    50

    60

    1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24

    Ave

    rage

    su

    rfac

    e o

    zon

    e (p

    pb

    )

    Hour of day

    OBS

    CAMx

    0

    10

    20

    30

    40

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    1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24

    Ave

    rage

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    rfac

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    e (p

    pb

    )

    Hour of day

    OBS

    CAMx

    0

    10

    20

    30

    40

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    60

    1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24

    Ave

    rage

    su

    rfac

    e o

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    e (p

    pb

    )

    Hour of day

    OBS

    CAMx

    0

    10

    20

    30

    40

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    1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24

    Ave

    rage

    su

    rfac

    e o

    zon

    e (p

    pb

    )

    Hour of day

    OBS

    CAMx

    SPRING WINTER

    SUMMER AUTUMN

  • © CSIR 2010 Slide 19 www.csir.co.za

    Results – Annual average surface ozone (1989-2009)

    © CSIR 2013

  • © CSIR 2010 Slide 20 www.csir.co.za

    Results – Seasonal average surface ozone (1989-2009)

    © CSIR 2013

    SPRING

    SPRING SUMMER

    AUTUMN WINTER

  • © CSIR 2010 Slide 21 www.csir.co.za

    Results – Annualar slope of linear regression (1989-2009)

    © CSIR 2013

    aka “trend”

  • © CSIR 2010 Slide 22 www.csir.co.za

    Results – Seasonal slope of linear regression (1989-2009)

    © CSIR 2013

    SPRING

    SPRING SUMMER

    AUTUMN WINTER

  • © CSIR 2010 Slide 23

    To be completed…

    • Complete selected 2010-2100 runs

    • Correlate ozone trends to climate trends (establish mechanisms)

    • Cloud cover (UV)

    • Rainfall (Deposition/Chemistry)

    • Temperature inversions (Transport)

    • CAMx input optical depth

    • ENSO (???) - AMT

  • © CSIR 2010 Slide 24

    Thank you for your time