Local Air Pollution Modeling Local Air Pollution Modeling AIM/Air AIM/Air
Takeshi Fujiwara and Yuzuru Matsuoka Takeshi Fujiwara and Yuzuru Matsuoka 2003/03/13 2003/03/13 The 8 The 8th
th AIM International Workshop
Local Air Pollution Modeling Local Air Pollution Modeling AIM/Air - - PowerPoint PPT Presentation
Local Air Pollution Modeling Local Air Pollution Modeling AIM/Air AIM/Air Takeshi Fujiwara and Yuzuru Matsuoka Takeshi Fujiwara and Yuzuru Matsuoka 2003/03/13 2003/03/13 th AIM International Workshop The 8 th AIM International Workshop The
th AIM International Workshop
Source recepter matrix
Receptor models
Human health impacts Soils acidification /eutrophication Forests acidification /eutrophication Water bodies acidification /eutrophication In door receptor model
Source models AIM/Local and Inventory
Residential Transport Commercial Industry Energy
Air Model Long range transport (LRT) model LPS model Area Source model
LPS (plume and puff) model AS(Euler) model Long range transportation model
Height 1 Height 2 Height 3
3 Layered Euler model 1 Layered AS model (Euler) 10km 50km
Vertical Relation between AS model and LRT model
1st layer (~1000m) 2nd layer (~3000m) 3rd layer (~5000m) 50km LPS model (plume and puff)
50km LRT cell Relation among LPS grid, AS grid and LRT grid 30km 30km 10km 50km 10km AS cell LPS cell
MASCON Wind velocity is interpolated based on air mass balance ECMWF Meteorology data
AS model A diffusion model in the lower mixing layer for pollutants emitted from area sources LRT model A model for Long-Range Transportation of air pollutants. LPS model Plume and Puff model for pollutants emitted from large point sources GIS Geographic Information System LPS data Large point sources data AS data Area sources data
prep.d wind.lrt wind.as u.d v.d w.d geo.d sg.d rad.d cloud.d temp.d emit.lps emit.as
diffusionLRT diffusionAS diffusionLPS
ECMWF GRIBEX
interpAS interpLRT balanceAS balanceLRT ReadGRIB wind.lps interpLPS stabLPS
prep.d u.d v.d w.d geo.d sg.d rad.d cloud.d temp.d
ECMWF GRIBEX
ReadGRIB
Wind velocity(u,v,w) Geo potential Surface Geo potential Precipitation Total cloud cover Solar radiation Temperature
u.d v.d w.d geo.d sg.d rad.d cloud.d temp.d emit.lps
diffusionLPS
wind.lps interpLPS stabLPS
LPS location Stack height Emission intensity Gas flow rate Interpolation of wind velocity at LPS site and stack height Calculation of atmospheric stability
wind.as u.d v.d w.d geo.d sg.d emit.as
diffusionAS
interpAS balanceAS
Emission intensity at each cell Primary interpolation of wind velocity Secondary interpolation of wind velocity using mass balance equation (MASCON)
prep.d wind.lrt u.d v.d w.d geo.d sg.d emit.lps emit.as
diffusionLRT
interpLRT balanceLRT
Primary interpolation of wind velocity Secondary interpolation of wind velocity using mass balance equation (MASCON)
3000m 1000m αhPa βhPa γhPa P r e s s u r e l e v e l 3000m 1000m αhPa βhPa
Surface Geopotential
γhPa P r e s s u r e l e v e l P r e s s u r e l e v e l
Interpolation Geopotential
( ) ( ) ( ) ( ) ( )
2 2 2 1 1
1 , , , , , z z y y x x z y x u z y x u
i i i i N i i N i i i i i
− + − + − = =
∑ ∑
= =
λ λ λ
( )
( ) ( ) { }
hPa a G hPa G hPa hPa G a G hPa G hPa G
u E E u E E E E a u
α β β α α β
× − + × − × − =
, , , , , ,
1
( ) ( ) ( )
+ − + − − − =
2 2 2 2 2 2
2 2 exp 2 exp 2 , ,
z e z e y z y P
H z H z y u Q z y x C σ σ σ σ πσ
Plume model x: downstream coordinate, y: horizontally transverse coordinate, z: vertical coordinate (representative height=1.5m, σy,σz: diffusion coefficients and calculated with the next equations, Qp: emission from LPS, u: wind velocity, He: effective height of stacks γy,γz,αy,αz: parameters given with Pasquill-Gifford diagram. He is given by the next CONCAWE equation. QH is a heat emission (cal/s), and uh is a wind velocity at the outlet
z y
x x
z z y y α α
γ σ γ σ ⋅ = ⋅ = , ( )
4 3 2 1
175 . T T q C Q u Q H H H H
g g p H h H e
− = = ∆ ∆ + =
−
ρ
Puff model in case of no wind/weak wind where α and γ is given with Pasquill stability classification. In this case, He is given by Briggs equation.
( ) ( ) ( ) ( ) ( )
∫
∞ − + − + − + + − − − −
= + + + = − + + = − ⋅ + + − ⋅ + − =
W t e e P
dt e W H z y x H z y x ux x u ux ux x u ux u Q z y x C
2
1 erfc 2 erfc 2 exp 2 1 1 2 erfc 2 exp 2 1 1 2 exp 2 , ,
2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 2 3
π γ α η γ α η αη η α αη π η αη η α αη π η α γ π
8 3 4 1
4 . 1
−
= ∆ dz d Q H
H
θ
(K/m) gradient re temperatu potential is dz dθ
i i i v i h i h i i i i
Q R z c k z y c k y x c k x z wc y vc x uc t c + + ∂ ∂ ∂ ∂ + ∂ ∂ ∂ ∂ + ∂ ∂ ∂ ∂ + ∂ ∂ − ∂ ∂ − ∂ ∂ − = ∂ ∂ ) ( ) ( ) (
P
C ⋅
S
x ∆
S
v
N
v
N
x ∆
E
C ⋅
W
C ⋅
N
C ⋅
S
C ⋅
W
y ∆
E
y ∆
W
u
E
u
Input and output through a cell
i
c
h
k
v
k
i
R
i
Q
Concentration Diffusion parameters Reaction terms
2 2 2 2 2
, , , , SO SO P SO
SO in SO P
R Q E E z y x t C + + − = ∆ ⋅ ∆ ⋅ ∆ ⋅ ∆ ∆
4 4 4 4 4
, , , , SO SO P SO
SO in SO P
R Q E E z y x t C + + − = ∆ ⋅ ∆ ⋅ ∆ ⋅ ∆ ∆
k: reaction rate of SO2→SO42 –
W: dry deposition ratio
PR: wet deposition rate
( ) { }
z y x kC z y x C PR z W R
SO P SO P SO P SO P SO P
∆ ⋅ ∆ ⋅ ∆ ⋅ − ∆ ⋅ ∆ ⋅ ∆ ⋅ ⋅ − ∆ − =
2 2 2 2 2
, , , , ,
( ) { }
z y x C PR z W z y x C k R
SO P SO P SO P SO P SO P
∆ ⋅ ∆ ⋅ ∆ ⋅ ⋅ − ∆ − + ∆ ⋅ ∆ ⋅ ∆ ⋅ ⋅ =
4 4 4 2 2
, , , , ,
Dry deposition Wet deposition Oxidation Emission SO2 SO4
2-