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Untangling the influence of air-mass
origin in interpreting composition trends
Zoë FlemingPaul Monks, Roland Leigh (Leicester University)
Brian Bandy, Stuart Penkett (UEA)
Lucy Carpenter, James Lee, Sarah Moller, Katie Read (York University)
Alistair Manning (Met office)
7th July 2010
The measurement stations
The NAME model
• Originally NAME stood for Nuclear Accident ModEl
• Lagrangian transport/dispersion model
Numerical
Atmospheric Dispersion
Modelling
Environment
• Uses Unified model met data and can run with
chemistry or for neutral inert particle releases
Run conditions
• 3 hourly release of particles backwards ten
days in time (1 or 5 days for London)
• Run at 2 or 3 height ranges (most interested in
low level to show interaction with surface
emissions)
Monthly footprints
Weybourne Cape Verde BT tower
Yearly averaged
Campaigns: SOS, Cape Verde and
TORCH2, Weybourne
Individual days
Campaign averaged
Weybourne air mass sectors
Weybourne regional distribution
100
80
60
40
20
0
% d
istr
ibu
tion
of se
cto
rs
01
/10
/20
06
01
/01
/20
07
01
/04
/20
07
01
/07
/20
07
01
/10
/20
07
01
/01
/20
08
01
/04
/20
08
01
/07
/20
08
01
/10
/20
08
01
/01
/20
09
01
/04
/20
09
01
/07
/20
09
01
/10
/20
09
America Europe Atlantic Scandinavia Greenland and Iceland UK North Sea Arctic
Weybourne regional variations
100
80
60
40
20
0
% d
istr
ibu
tio
n o
f se
cto
rs
13
/10
/20
07
00
:00
14
/10
/20
07
00
:00
15
/10
/20
07
00
:00
16
/10
/20
07
00
:00
17
/10
/20
07
00
:00
18
/10
/20
07
00
:00
19
/10
/20
07
00
:00
20
/10
/20
07
00
:00
21
/10
/20
07
00
:00
22
/10
/20
07
00
:00
23
/10
/20
07
00
:00
24
/10
/20
07
00
:00
25
/10
/20
07
00
:00
26
/10
/20
07
00
:00
27
/10
/20
07
00
:00
28
/10
/20
07
00
:00
29
/10
/20
07
00
:00
30
/10
/20
07
00
:00
31
/10
/20
07
00
:00
01
/11
/20
07
00
:00
0.8
0.6
0.4
0.2
0.0
America Europe Atlantic Scandinavia Greenland_and_Iceland UK North_Sea Arctic pure_Arctic
100
80
60
40
20
0
% d
istr
ibu
tio
n o
f se
cto
rs
10
/02
/20
07
02
/03
/20
07
22
/03
/20
07
11
/04
/20
07
01
/05
/20
07
21
/05
/20
07
10
/06
/20
07
30
/06
/20
07
America Europe Atlantic Scandinavia Greenland and Iceland UK North Sea Arctic
From Regional division to trajectory type
• Derive threshold for each region to decide
whether significant influence or proportion of
total particle journey
• Combination of which regions covered in
transport decides which trajectory type
4x10-3
3
2
1
0
part
icle
concentr
ation/ g s
/ m
3
01/01/2007 01/07/2007 01/01/2008 01/07/2008 01/01/2009 01/07/2009
Dust 'thresh0.0005' th_Af
NO2: 2006-2008 sectors
0
2
4
6
8
10
12N
O2
/ p
pb
v
2006
2007
2008
CN and SO2
0
20000
40000
60000
80000
100000
120000
140000
CN
2006
2007
0
0.2
0.4
0.6
0.8
1
1.2
1.4
1.6
SO2
/ p
pb
v
2008
2009
Arctic air masses
• Arctic and Scandinavian ozone
highest
• Run on global model domain to
track back 20 days to Asia up to
5000 m elevation
0
5
10
15
20
25
30
35
40
45
50
O3
O3
/ p
pb
v2006-2009 average
Arctic
Arctic + Europe
Atlantic
Europe
local
scand,greenland
America
Cape Verde air mass division
Cape Verde
100
80
60
40
20
0
% c
ontr
ibutio
n o
f e
ach
sect
or
01/1
1/2
006
01/0
1/2
007
01/0
3/2
007
01/0
5/2
007
01/0
7/2
007
01/0
9/2
007
01/1
1/2
007
01/0
1/2
008
01/0
3/2
008
01/0
5/2
008
01/0
7/2
008
01/0
9/2
008
01/1
1/2
008
01/0
1/2
009
01/0
3/2
009
01/0
5/2
009
01/0
7/2
009
01/0
9/2
009
Coastal African
Polluted marine (Europe)
Saharan Africa (Dust)
Atlantic continental (North America)
Atlantic marine
Cape Verde air mass division
African European
Coastal African
American
Classification into 7 major trajectory types
Atlantic and African coast
American, Atlantic and African coast
Saharan and no Europe
Saharan and Europe
Polluted and marine
Atlantic MarineAmerican Continental and Atlantic
Local air (flag for contamination or
slow transport)100
80
60
40
20
0
% o
f tim
e s
pen
t in
each
are
a
01/1
1/2
00
6
01/0
1/2
00
7
01/0
3/2
00
7
01/0
5/2
00
7
01/0
7/2
00
7
01/0
9/2
00
7
01/1
1/2
00
7
01/0
1/2
00
8
01/0
3/2
00
8
01/0
5/2
00
8
01/0
7/2
00
8
01/0
9/2
00
8
01/1
1/2
00
8
01/0
1/2
00
9
01/0
3/2
00
9
01/0
5/2
00
9
01/0
7/2
00
9
01/0
9/2
00
9
CoastalAfrican
Polluted_marine
Dust
Atlantic_cont
Atlantic_marine
site_ne
site_nw
site_sw
site_se
Relating to back to chemistry
(harmonised timeseries of 56
parameters)
01/1
1/2
006
01/0
1/2
007
01/0
3/2
007
01/0
5/2
007
01/0
7/2
007
01/0
9/2
007
01/1
1/2
007
01/0
1/2
008
01/0
3/2
008
01/0
5/2
008
01/0
7/2
008
01/0
9/2
008
01/1
1/2
008
01/0
1/2
009
01/0
3/2
00
9
01/0
5/2
009
01/0
7/2
009
01/0
9/2
009
01/1
1/2
009
01/0
1/2
010
01/0
3/2
010
2000
1500
1000
500
0
NO
xy a
nd V
OC
/ pptv
50
40
30
20
10
0
O3/p
pbv
220
200
180
160
140
120
100
80
60
CO
/ ppbv
3000
2500
2000
1500
1000
500
aero
sol n
um
ber
NO2
O3
CO ethane benzene isoprene ethene Aerosol number Temperature
Averaging/binning by trajectory type
-10
-5
0
5
10
15
20
Atlantic and
African coast
Atlantic
Marine only
American
and Atlantic
American,
Atlantic and African coast
European Africa (no
European)
Africa and
Europe
iso
pre
ne
/ p
ptv
isoprene 3 year averages
0
20
40
60
80
100
120
140
Atlantic and African coast
Atlantic Marine only
American and Atlantic
American, Atlantic and
African coast
European Africa (no European)
Africa and Europe
CO
/ p
pb
v
CO 3 year averages
0
0.2
0.4
0.6
0.8
1
1.2
1.4
Atlantic and African coast
Atlantic Marine only
American and Atlantic
American, Atlantic and African coast
European Africa (no European)
Africa and Europe
CH
Br3
/ p
ptv
CHBr3 3 year averages
0
100
200
300
400
500
600
700
800
Atlantic and African coast
Atlantic Marine only
American and Atlantic
American, Atlantic and
African coast
European Africa (no European)
Africa and Europe
NO
y/
pp
tv
NOy filtered 3 year averages
VOCs
0
5
10
15
20
25
30
35
Atlantic and African
coast
Atlantic Marine
only
American and
Atlantic
American, Atlantic
and African coast
European Africa (no European)
Africa and Europe
VO
C/
pp
tv
isobutane
isopentane
DMS
ethene
Ozone monthly averaging and
de-seasonalisation60
50
40
30
20
10
ozon
e/ p
pbv
350300250200150100500
3 year time series divided in 360 degrees
Sin wave equation y0 =31.491 ± 0.073 A =-8.1982 ± 0.101 f =0.05431 ± 0.000123 phi =1.8367 ± 0.0244
O3
polynomial to power 10 O3 sine function mean ozone ozone deseaonalised (from difference) ozone deseas ratio
0
5
10
15
20
25
30
35
40
45
Atlantic and African coast
Atlantic Marine only
American and Atlantic
American, Atlantic and African coast
European Africa (no European)
Africa and Europe
O3
/ p
pb
v
O3 deseasonalised 3 year averages
0
5
10
15
20
25
30
35
40
45
50
Atlantic and African coast
Atlantic Marine only
American and Atlantic
American, Atlantic and African coast
European Africa (no European)
Africa and Europe
O3
/ p
pb
v
O3 3 year averages
Aerosol monthly averages
0
100
200
300
400
500
600
700
800
900
Atlantic and African coast
Atlantic Marine only
American and Atlantic
American, Atlantic and
African coast
European Africa (no European)
Africa and Europe
aero
sol n
um
be
r
aerosol number 3 year averages
• Saharan and European have highest aerosol loading
Ratio analysis between trajectory types
• O-VOC ratios different
between marine and
terrestrial sources
5000
4000
3000
2000
1000
aceto
ne
/p
ptv
70006000500040003000200010000
methanol/ pptv
Atlantic and African coast Atlantic marine only American and Atlantic American, Atlantic and African coast Polluted and marine African and no Europe African and Europe
y = 0.4093x - 10.098 (R² = 0.4578)y = 0.4241x - 10.736 (R² = 0.5334)y = 0.3251x - 0.6948 (R² = 0.4688)y = 0.3685x - 3.6453 (R² = 0.6019)y = 0.4266x - 10.109 (R² = 0.5943)y = 0.3231x - 0.5268 (R² = 0.4171)y = 0.4635x + 289.71 (R² = 0.0998)
50
40
30
20
10
O3/
pp
bv
14012010080
CO/ ppbv
African and Europe
African and no Europe
American and Atlantic
American, Atlantic and African coast
Polluted and marine
Atlantic and African coast
Atlantic marine only
y = 0.4093x - 10.098 (R² = 0.4578)y = 0.4241x - 10.736 (R² = 0.5334)y = 0.3251x - 0.6948 (R² = 0.4688)y = 0.3685x - 3.6453 (R² = 0.6019)y = 0.4266x - 10.109 (R² = 0.5943)y = 0.3231x - 0.5268 (R² = 0.4171)y = 0.313x + 0.0773 (R² = 0.5026)
• O3 : CO ratios show a large
spread but higher gradients
for European and African
Mace Head, Harwell and Marylebone
road and Eltham 1 day backwards
• Marylebone rd• Eltham
• Harwell• Mace Head
BT tower 1 day back runs
• 5 day backwards split into sectors
• 1 day backwards split the UK and North
Sea, northern France/ Benelux into 10
regions
100
80
60
40
20
0
% c
ontr
ibution o
f geogra
phic
al secto
rs to a
ir a
rriv
ing a
t B
T tow
er
01/02/2006 01/03/2006 01/04/2006 01/05/2006 01/06/2006 01/07/2006
Arctic
Scandinavia
Europe
Atlantic
Greenland_and_Iceland
America
UK
North_Sea
Running forwards from London
• Forward run combined with NAEI emission
inventory to track chemistry emissions from
London affecting the surrounding areas
• Run forwards from surrounding areas towards
BT tower
Conclusions
• Have built up a library of successive 3 hourly back
trajectories from NAME for 3 sites
• Analysis of regional distribution of transport shows
how quickly and when air mass direction changes
• Combination of regional influences can define
trajectory types
• Can provide footprints or detailed 3 hourly influence
regional distribution for campaigns or one off events
• Can look at long term changes / seasonal changes or
variations in chemistry between trajectory types
• Future project to run NAME forwards with chemistry
and combining with emission inventories