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Introduction to

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Fast screening tool for control strategies for PM ... Parameterized chemistry version uses algorithms from RTM-II (concluded) Presents:/s ... – PowerPoint PPT presentation

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Title: Introduction to


1
Introduction to The REMSAD Modeling System
Presented By Gerard Mansell ENVIRON
International Corporation
January 2002
2
What is REMSAD?
Regulatory Modeling System for Aerosols and
Deposition
  • Designed to be
  • Fast screening tool for control strategies for PM
  • Continental-scale tool for deposition of toxics
    and acidic precipitation

3
REMSAD as a PM Model
  • Applicable over regional scales
  • Includes both Primary and Secondary particulates
  • Responds to inventory-level control measures
  • Detailed representation of spatial and temporal
    distributions
  • Treats meteorological influences on transport and
    removal directly

4
Technical Overview
  • Based on UAM-V
  • Recast in sigma coordinate
  • Extended vertically to tropopause
  • Less detailed photochemistry (?CB-IV)
  • Processes Treated
  • Transport
  • Deposition (wet and dry)
  • Chemistry (gaseous, aqueous, aerosols)
  • Inputs
  • Emissions
  • Meteorology
  • Airquality
  • Chemical rates
  • Landuse

5
Technical Overview
(continued)
  • Outputs
  • Ammonium Sulfate Particulates
  • Acidic Sulfate Deposition Flux
  • Ammonium Nitrate Particulates
  • Nitric Acid Deposition Flux
  • Secondary Organic Aerosol
  • Primary Coarse Particulates
  • Primary Fine Particulates
  • Total Fine Particulates
  • Visibility Measures (Extinction, Deciview, Visual
    Range)

6
Advantages and Limitations
  • Existing databases
  • Simplified treatment allows cost effective
    solutions
  • Key features components consistent with
    state-of-the-science
  • Previous results peer review demonstrated
    capabilities of producing credible results

7
Advantages and Limitations
(continued)
  • Simplified O3 chemistry may not be adequate to
    simulate O3 concentrations or interactions of O3
    with other pollutants (PM)
  • No SOA treatment

8
Processes
  • Transport
  • Advection
  • Smolarkiewicz on Arakawa-C grid
  • Other schemes -- Petrov-Galerkin,
    Taylor-Galerkin, Van Leer
  • Turbulent Diffusion
  • K-Theory or First-order Closure
  • Kx, Ky, Kz - Eddy Diffusivity Coefficients
  • Horizontal -- Deformation of Horiz. Wwinds
    (Smagorinsky)
  • Vertical -- Diagnosed form wind temp (McNider
    Pielke) or interpolated from MM5

9
Processes
(continued)
  • Transport
  • Cloud Dynamics
  • Diagnosed as in MM5 (Anthes et al., 1987)
  • Deep Convective Clouds
  • Vertical redistribution due to deep convection
  • Calculated only if rainfall
  • Within Cloud -- tendency for species proportional
    to cloud cover and vertical gradients within and
    below
  • Mass Conservation/Continuity -- tendencies within
    cloud balanced with subcloud layer, vertical
    exchange between cloud layer and subcloud layers

10
Processes
(continued)
  • Stratiform Clouds
  • Vertical redistribution performed if maximum
    cloud coverage gt 10 and
  • Cloud depth gt 0.1s and
  • Bottom of cloud layer lt 3000 m AGL
  • Explicit K-theory (Lin et al., 1994)
  • Shallow Cumulus Clouds (not considered)

11
Processes
(continued)
  • Deposition (dry)
  • Dry Deposition based on RADM Algorithm
    (Wesley,1989)
  • Flux to ground F - C Vd
  • Deposition velocity (gases)
  • Ra Aerodynamic resistance (PBL similarity model
    Louis, 1979)
  • Rb Boundary (quasi-laminar) layer resistance
  • Rs Surface resistance (dependent on leaf
    stomata and cuticles, lower canopy resistance,
    soil litter, and water)
  • Deposition velocity (particles)

12
Processes
(continued)
  • Gaseous Deposition (wet)
  • Parameterized based on
  • Henry Laws solubility coefficients, rainfall
    rates, cloud depth and temperature
  • Hales Sutter (1979) original work and developed
    ionization constants for SO2
  • ATDM extended to (NO, NO2, SO2, NH3, VOC, HNO3)
    and 7 toxic species
  • New solubility constants taken from literature,
    now temperature dependent
  • Drop size and velocity parameterized based on
    rainfall rate - Scott (1978)
  • Each model layer successively adjusted for
    deposition
  • Typical cloud pH of 4.5 has been used for
    solubility calculations

13
Processes
(continued)
  • Particle Deposition (wet)
  • Based on relationships developed by Scott (1978)
  • Rainfall rate and cloud type related to fraction
    of sulfate within rainwater reaching ground
  • Extended to treat any aerosol -- function of
    sulfate rate
  • Key assumptions
  • Aerosols lt 1 ?m in dia - Nucleation of cloud
    droplets around aerosols
  • Aerosols gt 1 ?m in dia - removed only through
    impaction with falling drops
  • Within-Cloud washout rate
  • Time in which active hydrometeor growth occurs
  • cloud depth, temperature, rainfall rate, and
    cloud type
  • Below cloud base to ground washout rate (liquid
    only)
  • function of rainfall rate

14
Processes
(continued)
  • Gas Phase Chemistry
  • Parameterized
  • Uses OH lookup tables OHf(O3,NOx,sunlight)
  • O3 input
  • Treats NOx, SO2, NH3, VOC, HNO3

15
Processes
(continued)
  • Gas Phase Chemistry
  • ?CB-IV
  • Reduced organic speciation
  • Inorganics and radicals same as CB-IV
  • 3 organics species VOC, ISOP, CARB
  • Responds to NOx and VOC controls
  • Approximates full CB-IV
  • Predicts precursors to secondary particulates

16
Processes
(concluded)
  • Aqueous Phase Chemistry
  • In-cloud sulfate formation
  • Reactions of SO2 w/ H2O2, O2 and O3
  • Uses representation of Martin (1994) to estimate
    rate of sulfate formation
  • Assumed pH of 4.5
  • Parameterized chemistry version uses algorithms
    from RTM-II

17
Processes
(concluded)
  • Aerosol Chemistry
  • Nitrate from equilibrium between nitrate,
    sulfate, and ammonia
  • MARS-A equilibrium routines from CMAQ
  • Earlier versions use parameterized chemistry to
    estimate equilibrium

18
REMSAD System
19
Flow of Major ATDM Processes
20
Nesting GridExamples
21
Vertical Grid Structurein Typical
REMSADApplication
?

?????????
0.0
pt
0.1
0.3
0.5
0.7
0.78
0.84
0.93
0.98
1.00
22
Examples ofVertical Nesting
23
Model Inputs
  • Airquality (Initial Boundary concentrations)
  • ppm for gases µg/m3 for particulates)
  • CAMx or UAM preprocessor
  • Winds (u v components m/s2)
  • supplied for coarse grid optionally for nested
    grids
  • w component calculated internally
  • Temperature ( K )
  • three dimensional temps at cell centers
  • Surface air temperature
  • supplied for coarse grid only

24
Model Inputs
(continued)
  • Humidity (water vapor mixing ratio kg/kg)
  • supplied for coarse grid only
  • used for cloud diagnosis sulfate chemistry
    deposition
  • Cloud Liquid Water (mixing ratio kg/kg)
  • supplied for coarse grid only
  • used to compute reaction rates for aqueous-phase
    chemistry wet deposition rates
  • Rain Liquid Water (mixing ratio kg/kg)
  • supplied for coarse grid only
  • used to compute reaction rates for aqueous-phase
    chemistry

25
Model Inputs
(continued)
  • Surface pressure (mbar)
  • supplied for coarse grid optionally for nested
    grids
  • defines vertical heights and 3D pressure
  • used to calculate reaction rates, photolysis
    rates, deposition, plumerise
  • Vertical Turbulent Exchange Coefficients (m2/s)
  • supplied for coarse grid optionally for nested
    grids
  • determines rate of vertical diffusion
  • non-zero minima (0.1-1 m2/s)
  • Precipitation (rainfall rate in/hr)
  • supplied for coarse grid only
  • used in cloud diagnosis, wet deposition

26
Model Inputs
(continued)
  • Surface characteristics
  • supplied for coarse grid optionally for nested
    grids
  • defines landuse fraction for each of 11 land use
    categories
  • used to calculate deposition rates
  • Terrain (m above sea level)
  • supplied for coarse grid only
  • surface elevation
  • Not needed (use dummy values of zero)
  • CHEMPARAM
  • Defines species to be simulated and lower bounds
  • particle size and mass distributions
  • varies by model version

27
Model Inputs
(concluded)
  • Photolysis Rates
  • tabulated rates for five key reactions
  • photolysis of NO2, HCHO, O3 and ALD2
  • function of height zenith angle under constant
    albedo (0.08), ozone column (0.318) and haze
    (0.2)
  • Emission inventory
  • Gridded low-level area sources
  • supplied for coarse grid and all nested grids
  • Elevated point sources
  • NO, NO2, POA, PEC, GSO4, PNO3, VOC, SOA, SO2, CO,
    NH3, CARB, ISOP, PMFINE, PMCOARS
  • EPS2 or SMOKE processor

28
Model Outputs
  • Average files
  • average layer 1 concentrations
  • µg/m3 for all species
  • user specified species
  • Instant files
  • three dimensional instantaneous concentrations
  • ppm for all species
  • includes all species
  • Deposition files
  • wet and dry surface depositon
  • g/m3 for all species
  • user specified species
  • Diagnostic outputs

29
REMSAD PostprocessingSystem Flowchart
30
Visibility Measures
bext (?) bscat (?) babs (?)
bscat babs (usually)
  • Extinction
  • Deciview
  • Visual Range

DV 10 ln (bext/10), where Bext is in
Mm-1
- ln (0.02) bext
3.912 bext
vr

31
WRAP REMSAD Modeling Domain
32
Computer Resource Requirements
  • WRAP modeling domain (120 x 84 x 12)
  • Disk storage (per simulation day)
  • Inputs
  • Emissions 45 Mb
  • Meteorology 88 Mb
  • Outputs
  • Average 26 Mb
  • Deposition 52 Mb
  • Instant 315 Mb
  • CPU (per simulation day)
  • 50 min. on Linux box w/ 1.2 GHz AMD Athelon 1
    Gb memory

33
Computer Resource Requirements
(Continued)
34
Computer Resource Requirements
(Concluded)
35
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